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  • 2020-2024  (9,438)
  • 2024  (9,438)
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  • 1
    Publication Date: 2024-06-22
    Description: Selected multicorer cores of R/V Sonne cruise SO268-1 and were scanned by a Toshiba Aquilion 64 computer tomograph (CT) at the hospital Klinikum Bremen-Mitte with an x-ray source voltage of 120 kV and a current of 600 mA. The CT image stacks have a resolution of 0.35 mm in x/y-direction and 0.5 mm resolution in z-direction (0.3 mm reconstruction unit). Images were reconstructed using Toshiba's patented helical cone beam reconstruction technique (TCOT) and are provided in DICOM-format. The data were processed with the ZIB edition of the Amira software (version 2021.03; Stalling et al., 2005; http://amira.zib.de). Within Amira, the core liners, including about 2 mm of the core rims, were deleted from the data set. Mangan nodules with diameters 〉1 mm, open bioturbation traces, an unidentified organism (only present in core SO268-2-200-1 MC18), the natural bioturbated and surficial homogenised sediment were segmented by a marker-based watershed segmentation and visualized in 3D. Subsequently, the sediment components were quantified (MaterialStatistics module; volume per slice) and the mean and standard deviation of the sediment x-ray attenuation (MaterialStatistics module; statistics per slice per label; to avoid marginal averaging effects the sediment label was reduced by three voxels) were determined.
    Keywords: Binary Object; Bioturbation; Bioturbation, volume; Center for Marine Environmental Sciences; Clarion-Clipperton Fraction Zone, North East Pacific Ocean; Computed Tomography; Computer tomography (CT) Toshiba Aquilion 64; Cracks, relative volume; Cracks, volume; DEPTH, sediment/rock; File content; JPI Oceans - Ecological Aspects of Deep-Sea Mining; JPIO-MiningImpact; Manganese nodules, relative volume; Manganese nodules, volume; MARUM; Mining impact; MUC; MUC-02; MultiCorer; Number of slice; Number of voxels, matrix sediment; Sediment, bioturbated lower layer, relative volume; Sediment, bioturbated lower layer, volume; Sediment, homogenized upper layer, relative volume; Sediment, homogenized upper layer, volume; Sediment characterisation; SO268/1; SO268/1_6-1; Sonne_2; X-ray attenuation, matrix sediment, mean; X-ray attenuation, matrix sediment, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 12997 data points
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  • 2
    Publication Date: 2024-06-22
    Description: Oxygen isotopes in biogenic silica (δ18O BSi) from lake sediments allow for quantitative reconstruction of past hydroclimate and proxy–model comparison in terrestrial environments. The signals of individual records have been attributed to different factors, such as air temperature (T air ), atmospheric circulation patterns, hydrological changes and lake evaporation. Here, we provide 55 composite down–core records published to date and complemented with additional lake basin parameters (e.g. lake water residence time and catchment size) to best characterize the signal properties. Records feature widely different temporal coverage and resolution ranging from decadal–scale records covering the last 150 years to records with multi–millennial scale resolution spanning glacial–interglacial cycles. Best coverage in number of records (N=37) and datapoints (N=2112) is available for northern hemispheric (NH) extra–tropic regions throughout the Holocene (corresponding to Marine Isotope Stage 1; MIS 1).
    Keywords: Compilation; delta O-18; Diatom; Lake sediment core; paleoclimate proxy
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 3
    Publication Date: 2024-06-22
    Description: Selected multicorer cores of R/V Sonne cruise SO268-1 and were scanned by a Toshiba Aquilion 64 computer tomograph (CT) at the hospital Klinikum Bremen-Mitte with an x-ray source voltage of 120 kV and a current of 600 mA. The CT image stacks have a resolution of 0.35 mm in x/y-direction and 0.5 mm resolution in z-direction (0.3 mm reconstruction unit). Images were reconstructed using Toshiba's patented helical cone beam reconstruction technique (TCOT) and are provided in DICOM-format. The data were processed with the ZIB edition of the Amira software (version 2021.03; Stalling et al., 2005; http://amira.zib.de). Within Amira, the core liners, including about 2 mm of the core rims, were deleted from the data set. Mangan nodules with diameters 〉1 mm, open bioturbation traces, an unidentified organism (only present in core SO268-2-200-1 MC18), the natural bioturbated and surficial homogenised sediment were segmented by a marker-based watershed segmentation and visualized in 3D. Subsequently, the sediment components were quantified (MaterialStatistics module; volume per slice) and the mean and standard deviation of the sediment x-ray attenuation (MaterialStatistics module; statistics per slice per label; to avoid marginal averaging effects the sediment label was reduced by three voxels) were determined.
    Keywords: Binary Object; Bioturbation; Bioturbation, volume; Center for Marine Environmental Sciences; Clarion-Clipperton Fraction Zone, North East Pacific Ocean; Computed Tomography; Computer tomography (CT) Toshiba Aquilion 64; DEPTH, sediment/rock; File content; JPI Oceans - Ecological Aspects of Deep-Sea Mining; JPIO-MiningImpact; Manganese nodules, relative volume; Manganese nodules, volume; MARUM; Mining impact; MUC; MUC-03; MultiCorer; Number of slice; Number of voxels, matrix sediment; Sediment, bioturbated lower layer, relative volume; Sediment, bioturbated lower layer, volume; Sediment, homogenized upper layer, relative volume; Sediment, homogenized upper layer, volume; Sediment characterisation; SO268/1; SO268/1_7-1; Sonne_2; X-ray attenuation, matrix sediment, mean; X-ray attenuation, matrix sediment, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 10754 data points
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  • 4
    Publication Date: 2024-06-22
    Description: Selected multicorer cores of R/V Sonne cruise SO268-1 and were scanned by a Toshiba Aquilion 64 computer tomograph (CT) at the hospital Klinikum Bremen-Mitte with an x-ray source voltage of 120 kV and a current of 600 mA. The CT image stacks have a resolution of 0.35 mm in x/y-direction and 0.5 mm resolution in z-direction (0.3 mm reconstruction unit). Images were reconstructed using Toshiba's patented helical cone beam reconstruction technique (TCOT) and are provided in DICOM-format. The data were processed with the ZIB edition of the Amira software (version 2021.03; Stalling et al., 2005; http://amira.zib.de). Within Amira, the core liners, including about 2 mm of the core rims, were deleted from the data set. Mangan nodules with diameters 〉1 mm, open bioturbation traces, an unidentified organism (only present in core SO268-2-200-1 MC18), the natural bioturbated and surficial homogenised sediment were segmented by a marker-based watershed segmentation and visualized in 3D. Subsequently, the sediment components were quantified (MaterialStatistics module; volume per slice) and the mean and standard deviation of the sediment x-ray attenuation (MaterialStatistics module; statistics per slice per label; to avoid marginal averaging effects the sediment label was reduced by three voxels) were determined.
    Keywords: Binary Object; Bioturbation; Bioturbation, volume; Center for Marine Environmental Sciences; Clarion-Clipperton Fraction Zone, North East Pacific Ocean; Computed Tomography; Computer tomography (CT) Toshiba Aquilion 64; DEPTH, sediment/rock; File content; JPI Oceans - Ecological Aspects of Deep-Sea Mining; JPIO-MiningImpact; Manganese nodules, relative volume; Manganese nodules, volume; MARUM; Mining impact; MUC; MUC-08; MultiCorer; Number of slice; Number of voxels, matrix sediment; Sediment, bioturbated lower layer, relative volume; Sediment, bioturbated lower layer, volume; Sediment, homogenized upper layer, relative volume; Sediment, homogenized upper layer, volume; Sediment characterisation; SO268/1; SO268/1_39-1; Sonne_2; X-ray attenuation, matrix sediment, mean; X-ray attenuation, matrix sediment, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 9688 data points
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  • 5
    Publication Date: 2024-06-22
    Description: Selected multicorer cores of R/V Sonne cruise SO268-1 and were scanned by a Toshiba Aquilion 64 computer tomograph (CT) at the hospital Klinikum Bremen-Mitte with an x-ray source voltage of 120 kV and a current of 600 mA. The CT image stacks have a resolution of 0.35 mm in x/y-direction and 0.5 mm resolution in z-direction (0.3 mm reconstruction unit). Images were reconstructed using Toshiba's patented helical cone beam reconstruction technique (TCOT) and are provided in DICOM-format. The data were processed with the ZIB edition of the Amira software (version 2021.03; Stalling et al., 2005; http://amira.zib.de). Within Amira, the core liners, including about 2 mm of the core rims, were deleted from the data set. Mangan nodules with diameters 〉1 mm, open bioturbation traces, an unidentified organism (only present in core SO268-2-200-1 MC18), the natural bioturbated and surficial homogenised sediment were segmented by a marker-based watershed segmentation and visualized in 3D. Subsequently, the sediment components were quantified (MaterialStatistics module; volume per slice) and the mean and standard deviation of the sediment x-ray attenuation (MaterialStatistics module; statistics per slice per label; to avoid marginal averaging effects the sediment label was reduced by three voxels) were determined.
    Keywords: Binary Object; Bioturbation; Bioturbation, volume; Center for Marine Environmental Sciences; Clarion-Clipperton Fraction Zone, North East Pacific Ocean; Computed Tomography; Computer tomography (CT) Toshiba Aquilion 64; DEPTH, sediment/rock; File content; JPI Oceans - Ecological Aspects of Deep-Sea Mining; JPIO-MiningImpact; Manganese nodules, relative volume; Manganese nodules, volume; MARUM; Mining impact; MUC; MUC-06; MultiCorer; Number of slice; Number of voxels, matrix sediment; Sediment, bioturbated lower layer, relative volume; Sediment, bioturbated lower layer, volume; Sediment, homogenized upper layer, relative volume; Sediment, homogenized upper layer, volume; Sediment characterisation; SO268/1; SO268/1_26-1; Sonne_2; X-ray attenuation, matrix sediment, mean; X-ray attenuation, matrix sediment, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 10672 data points
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  • 6
    Publication Date: 2024-06-22
    Description: Selected multicorer cores of R/V Sonne cruise SO268-1 and were scanned by a Toshiba Aquilion 64 computer tomograph (CT) at the hospital Klinikum Bremen-Mitte with an x-ray source voltage of 120 kV and a current of 600 mA. The CT image stacks have a resolution of 0.35 mm in x/y-direction and 0.5 mm resolution in z-direction (0.3 mm reconstruction unit). Images were reconstructed using Toshiba's patented helical cone beam reconstruction technique (TCOT) and are provided in DICOM-format. The data were processed with the ZIB edition of the Amira software (version 2021.03; Stalling et al., 2005; http://amira.zib.de). Within Amira, the core liners, including about 2 mm of the core rims, were deleted from the data set. Mangan nodules with diameters 〉1 mm, open bioturbation traces, an unidentified organism (only present in core SO268-2-200-1 MC18), the natural bioturbated and surficial homogenised sediment were segmented by a marker-based watershed segmentation and visualized in 3D. Subsequently, the sediment components were quantified (MaterialStatistics module; volume per slice) and the mean and standard deviation of the sediment x-ray attenuation (MaterialStatistics module; statistics per slice per label; to avoid marginal averaging effects the sediment label was reduced by three voxels) were determined.
    Keywords: Binary Object; Bioturbation; Bioturbation, volume; Center for Marine Environmental Sciences; Clarion-Clipperton Fraction Zone, North East Pacific Ocean; Computed Tomography; Computer tomography (CT) Toshiba Aquilion 64; DEPTH, sediment/rock; File content; JPI Oceans - Ecological Aspects of Deep-Sea Mining; JPIO-MiningImpact; Manganese nodules, relative volume; Manganese nodules, volume; MARUM; Mining impact; MUC; MUC-08; MultiCorer; Number of slice; Number of voxels, matrix sediment; Sediment, bioturbated lower layer, relative volume; Sediment, bioturbated lower layer, volume; Sediment, homogenized upper layer, relative volume; Sediment, homogenized upper layer, volume; Sediment characterisation; SO268/1; SO268/1_39-1; Sonne_2; X-ray attenuation, matrix sediment, mean; X-ray attenuation, matrix sediment, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 9352 data points
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  • 7
    Publication Date: 2024-06-22
    Description: Selected multicorer cores of R/V Sonne cruise SO268-1 and were scanned by a Toshiba Aquilion 64 computer tomograph (CT) at the hospital Klinikum Bremen-Mitte with an x-ray source voltage of 120 kV and a current of 600 mA. The CT image stacks have a resolution of 0.35 mm in x/y-direction and 0.5 mm resolution in z-direction (0.3 mm reconstruction unit). Images were reconstructed using Toshiba's patented helical cone beam reconstruction technique (TCOT) and are provided in DICOM-format. The data were processed with the ZIB edition of the Amira software (version 2021.03; Stalling et al., 2005; http://amira.zib.de). Within Amira, the core liners, including about 2 mm of the core rims, were deleted from the data set. Mangan nodules with diameters 〉1 mm, open bioturbation traces, an unidentified organism (only present in core SO268-2-200-1 MC18), the natural bioturbated and surficial homogenised sediment were segmented by a marker-based watershed segmentation and visualized in 3D. Subsequently, the sediment components were quantified (MaterialStatistics module; volume per slice) and the mean and standard deviation of the sediment x-ray attenuation (MaterialStatistics module; statistics per slice per label; to avoid marginal averaging effects the sediment label was reduced by three voxels) were determined.
    Keywords: Binary Object; Bioturbation; Bioturbation, volume; Center for Marine Environmental Sciences; Clarion-Clipperton Fraction Zone, North East Pacific Ocean; Computed Tomography; Computer tomography (CT) Toshiba Aquilion 64; DEPTH, sediment/rock; File content; JPI Oceans - Ecological Aspects of Deep-Sea Mining; JPIO-MiningImpact; Manganese nodules, relative volume; Manganese nodules, volume; MARUM; Mining impact; MUC; MUC-10; MultiCorer; Number of slice; Number of voxels, matrix sediment; Sediment, bioturbated lower layer, relative volume; Sediment, bioturbated lower layer, volume; Sediment, homogenized upper layer, relative volume; Sediment, homogenized upper layer, volume; Sediment characterisation; SO268/1; SO268/1_43-1; Sonne_2; X-ray attenuation, matrix sediment, mean; X-ray attenuation, matrix sediment, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 11110 data points
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  • 8
    Publication Date: 2024-06-22
    Description: Selected multicorer cores of R/V Sonne cruise SO268-1 and were scanned by a Toshiba Aquilion 64 computer tomograph (CT) at the hospital Klinikum Bremen-Mitte with an x-ray source voltage of 120 kV and a current of 600 mA. The CT image stacks have a resolution of 0.35 mm in x/y-direction and 0.5 mm resolution in z-direction (0.3 mm reconstruction unit). Images were reconstructed using Toshiba's patented helical cone beam reconstruction technique (TCOT) and are provided in DICOM-format. The data were processed with the ZIB edition of the Amira software (version 2021.03; Stalling et al., 2005; http://amira.zib.de). Within Amira, the core liners, including about 2 mm of the core rims, were deleted from the data set. Mangan nodules with diameters 〉1 mm, open bioturbation traces, an unidentified organism (only present in core SO268-2-200-1 MC18), the natural bioturbated and surficial homogenised sediment were segmented by a marker-based watershed segmentation and visualized in 3D. Subsequently, the sediment components were quantified (MaterialStatistics module; volume per slice) and the mean and standard deviation of the sediment x-ray attenuation (MaterialStatistics module; statistics per slice per label; to avoid marginal averaging effects the sediment label was reduced by three voxels) were determined.
    Keywords: Binary Object; Bioturbation; Bioturbation, volume; Center for Marine Environmental Sciences; Clarion-Clipperton Fraction Zone, North East Pacific Ocean; Computed Tomography; Computer tomography (CT) Toshiba Aquilion 64; DEPTH, sediment/rock; File content; JPI Oceans - Ecological Aspects of Deep-Sea Mining; JPIO-MiningImpact; Manganese nodules, relative volume; Manganese nodules, volume; MARUM; Mining impact; MUC; MUC-18; MultiCorer; Number of slice; Number of voxels, matrix sediment; Sediment, bioturbated lower layer, relative volume; Sediment, bioturbated lower layer, volume; Sediment, homogenized upper layer, relative volume; Sediment, homogenized upper layer, volume; Sediment characterisation; SO268/1; SO268/1_75-1; Sonne_2; X-ray attenuation, matrix sediment, mean; X-ray attenuation, matrix sediment, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 10034 data points
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  • 9
    Publication Date: 2024-06-22
    Description: Selected multicorer cores of R/V Sonne cruise SO268-1 and were scanned by a Toshiba Aquilion 64 computer tomograph (CT) at the hospital Klinikum Bremen-Mitte with an x-ray source voltage of 120 kV and a current of 600 mA. The CT image stacks have a resolution of 0.35 mm in x/y-direction and 0.5 mm resolution in z-direction (0.3 mm reconstruction unit). Images were reconstructed using Toshiba's patented helical cone beam reconstruction technique (TCOT) and are provided in DICOM-format. The data were processed with the ZIB edition of the Amira software (version 2021.03; Stalling et al., 2005; http://amira.zib.de). Within Amira, the core liners, including about 2 mm of the core rims, were deleted from the data set. Mangan nodules with diameters 〉1 mm, open bioturbation traces, an unidentified organism (only present in core SO268-2-200-1 MC18), the natural bioturbated and surficial homogenised sediment were segmented by a marker-based watershed segmentation and visualized in 3D. Subsequently, the sediment components were quantified (MaterialStatistics module; volume per slice) and the mean and standard deviation of the sediment x-ray attenuation (MaterialStatistics module; statistics per slice per label; to avoid marginal averaging effects the sediment label was reduced by three voxels) were determined.
    Keywords: Binary Object; Bioturbation; Bioturbation, volume; Center for Marine Environmental Sciences; Clarion-Clipperton Fraction Zone, North East Pacific Ocean; Computed Tomography; Computer tomography (CT) Toshiba Aquilion 64; DEPTH, sediment/rock; File content; JPI Oceans - Ecological Aspects of Deep-Sea Mining; JPIO-MiningImpact; Manganese nodules, relative volume; Manganese nodules, volume; MARUM; Mining impact; MUC; MUC-20; MultiCorer; Number of slice; Number of voxels, matrix sediment; Sediment, bioturbated lower layer, relative volume; Sediment, bioturbated lower layer, volume; Sediment, homogenized upper layer, relative volume; Sediment, homogenized upper layer, volume; Sediment characterisation; SO268/1; SO268/1_80-1; Sonne_2; X-ray attenuation, matrix sediment, mean; X-ray attenuation, matrix sediment, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 9526 data points
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  • 10
    Publication Date: 2024-06-22
    Description: Selected multicorer cores of R/V Sonne cruise SO268-1 and were scanned by a Toshiba Aquilion 64 computer tomograph (CT) at the hospital Klinikum Bremen-Mitte with an x-ray source voltage of 120 kV and a current of 600 mA. The CT image stacks have a resolution of 0.35 mm in x/y-direction and 0.5 mm resolution in z-direction (0.3 mm reconstruction unit). Images were reconstructed using Toshiba's patented helical cone beam reconstruction technique (TCOT) and are provided in DICOM-format. The data were processed with the ZIB edition of the Amira software (version 2021.03; Stalling et al., 2005; http://amira.zib.de). Within Amira, the core liners, including about 2 mm of the core rims, were deleted from the data set. Mangan nodules with diameters 〉1 mm, open bioturbation traces, an unidentified organism (only present in core SO268-2-200-1 MC18), the natural bioturbated and surficial homogenised sediment were segmented by a marker-based watershed segmentation and visualized in 3D. Subsequently, the sediment components were quantified (MaterialStatistics module; volume per slice) and the mean and standard deviation of the sediment x-ray attenuation (MaterialStatistics module; statistics per slice per label; to avoid marginal averaging effects the sediment label was reduced by three voxels) were determined.
    Keywords: Binary Object; Bioturbation; Bioturbation, volume; Center for Marine Environmental Sciences; Clarion-Clipperton Fraction Zone, North East Pacific Ocean; Computed Tomography; Computer tomography (CT) Toshiba Aquilion 64; Cracks, relative volume; Cracks, volume; DEPTH, sediment/rock; File content; JPI Oceans - Ecological Aspects of Deep-Sea Mining; JPIO-MiningImpact; Manganese nodules, relative volume; Manganese nodules, volume; MARUM; Mining impact; MUC; MUC-15; MultiCorer; Number of slice; Number of voxels, matrix sediment; Sediment, bioturbated lower layer, relative volume; Sediment, bioturbated lower layer, volume; Sediment characterisation; SO268/1; SO268/1_66-1; Sonne_2; X-ray attenuation, matrix sediment, mean; X-ray attenuation, matrix sediment, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 10598 data points
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  • 11
    Publication Date: 2024-06-22
    Description: Selected multicorer cores of R/V Sonne cruise SO268-1 and were scanned by a Toshiba Aquilion 64 computer tomograph (CT) at the hospital Klinikum Bremen-Mitte with an x-ray source voltage of 120 kV and a current of 600 mA. The CT image stacks have a resolution of 0.35 mm in x/y-direction and 0.5 mm resolution in z-direction (0.3 mm reconstruction unit). Images were reconstructed using Toshiba's patented helical cone beam reconstruction technique (TCOT) and are provided in DICOM-format. The data were processed with the ZIB edition of the Amira software (version 2021.03; Stalling et al., 2005; http://amira.zib.de). Within Amira, the core liners, including about 2 mm of the core rims, were deleted from the data set. Mangan nodules with diameters 〉1 mm, open bioturbation traces, an unidentified organism (only present in core SO268-2-200-1 MC18), the natural bioturbated and surficial homogenised sediment were segmented by a marker-based watershed segmentation and visualized in 3D. Subsequently, the sediment components were quantified (MaterialStatistics module; volume per slice) and the mean and standard deviation of the sediment x-ray attenuation (MaterialStatistics module; statistics per slice per label; to avoid marginal averaging effects the sediment label was reduced by three voxels) were determined.
    Keywords: Binary Object; Bioturbation; Bioturbation, volume; Center for Marine Environmental Sciences; Clarion-Clipperton Fraction Zone, North East Pacific Ocean; Computed Tomography; Computer tomography (CT) Toshiba Aquilion 64; DEPTH, sediment/rock; File content; JPI Oceans - Ecological Aspects of Deep-Sea Mining; JPIO-MiningImpact; Manganese nodules, relative volume; Manganese nodules, volume; MARUM; Mining impact; MUC; MUC-21; MultiCorer; Number of slice; Number of voxels, matrix sediment; Sediment, bioturbated lower layer, relative volume; Sediment, bioturbated lower layer, volume; Sediment, homogenized upper layer, relative volume; Sediment, homogenized upper layer, volume; Sediment characterisation; SO268/1; SO268/1_85-1; Sonne_2; X-ray attenuation, matrix sediment, mean; X-ray attenuation, matrix sediment, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 10840 data points
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  • 12
    Publication Date: 2024-06-22
    Description: Selected multicorer cores of R/V Sonne cruise SO268-1 were scanned by a Toshiba Aquilion 64 computer tomograph (CT) at the hospital Klinikum Bremen-Mitte with an x-ray source voltage of 120 kV and a current of 600 mA. The CT image stacks have a resolution of 0.35 mm in x/y-direction and 0.5 mm resolution in z-direction (0.3 mm reconstruction unit). Images were reconstructed using Toshiba's patented helical cone beam reconstruction technique (TCOT) and are provided in DICOM-format. The data were processed with the ZIB edition of the Amira software (version 2021.03; Stalling et al., 2005; http://amira.zib.de). Within Amira, the core liners, including about 2 mm of the core rims, were deleted from the data set. Mangan nodules with diameters 〉1 mm, open bioturbation traces, an unidentified organism (only present in core SO268-2-200-1 MC18), the natural bioturbated and surficial homogenised sediment were segmented by a marker-based watershed segmentation and visualized in 3D. Subsequently, the sediment components were quantified (MaterialStatistics module; volume per slice) and the mean and standard deviation of the sediment x-ray attenuation (MaterialStatistics module; statistics per slice per label; to avoid marginal averaging effects the sediment label was reduced by three voxels) were determined.
    Keywords: Binary Object; Bioturbation; Bioturbation, volume; Center for Marine Environmental Sciences; Clarion-Clipperton Fraction Zone, North East Pacific Ocean; Computed Tomography; Computer tomography (CT) Toshiba Aquilion 64; DEPTH, sediment/rock; File content; JPI Oceans - Ecological Aspects of Deep-Sea Mining; JPIO-MiningImpact; Manganese nodules, relative volume; Manganese nodules, volume; MARUM; Mining impact; MUC-24; Multicorer with television; Number of slice; Number of voxels, matrix sediment; Sediment, bioturbated lower layer, relative volume; Sediment, bioturbated lower layer, volume; Sediment, homogenized upper layer, relative volume; Sediment, homogenized upper layer, volume; Sediment characterisation; SO268/2; SO268/2_122-1; Sonne_2; TVMUC; X-ray attenuation, matrix sediment, mean; X-ray attenuation, matrix sediment, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 10226 data points
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  • 13
    Publication Date: 2024-06-22
    Description: Selected multicorer cores of R/V Sonne cruise SO268-1 were scanned by a Toshiba Aquilion 64 computer tomograph (CT) at the hospital Klinikum Bremen-Mitte with an x-ray source voltage of 120 kV and a current of 600 mA. The CT image stacks have a resolution of 0.35 mm in x/y-direction and 0.5 mm resolution in z-direction (0.3 mm reconstruction unit). Images were reconstructed using Toshiba's patented helical cone beam reconstruction technique (TCOT) and are provided in DICOM-format. The data were processed with the ZIB edition of the Amira software (version 2021.03; Stalling et al., 2005; http://amira.zib.de). Within Amira, the core liners, including about 2 mm of the core rims, were deleted from the data set. Mangan nodules with diameters 〉1 mm, open bioturbation traces, an unidentified organism (only present in core SO268-2-200-1 MC18), the natural bioturbated and surficial homogenised sediment were segmented by a marker-based watershed segmentation and visualized in 3D. Subsequently, the sediment components were quantified (MaterialStatistics module; volume per slice) and the mean and standard deviation of the sediment x-ray attenuation (MaterialStatistics module; statistics per slice per label; to avoid marginal averaging effects the sediment label was reduced by three voxels) were determined.
    Keywords: Binary Object; Bioturbation; Bioturbation, volume; Center for Marine Environmental Sciences; Clarion-Clipperton Fraction Zone, North East Pacific Ocean; Computed Tomography; Computer tomography (CT) Toshiba Aquilion 64; DEPTH, sediment/rock; File content; JPI Oceans - Ecological Aspects of Deep-Sea Mining; JPIO-MiningImpact; Manganese nodules, relative volume; Manganese nodules, volume; MARUM; Mining impact; MUC-24; Multicorer with television; Number of slice; Number of voxels, matrix sediment; Sediment, bioturbated lower layer, relative volume; Sediment, bioturbated lower layer, volume; Sediment, homogenized upper layer, relative volume; Sediment, homogenized upper layer, volume; Sediment characterisation; SO268/2; SO268/2_122-1; Sonne_2; TVMUC; X-ray attenuation, matrix sediment, mean; X-ray attenuation, matrix sediment, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 13274 data points
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  • 14
    Publication Date: 2024-06-22
    Description: Selected multicorer cores of R/V Sonne cruise SO268-1 and were scanned by a Toshiba Aquilion 64 computer tomograph (CT) at the hospital Klinikum Bremen-Mitte with an x-ray source voltage of 120 kV and a current of 600 mA. The CT image stacks have a resolution of 0.35 mm in x/y-direction and 0.5 mm resolution in z-direction (0.3 mm reconstruction unit). Images were reconstructed using Toshiba's patented helical cone beam reconstruction technique (TCOT) and are provided in DICOM-format. The data were processed with the ZIB edition of the Amira software (version 2021.03; Stalling et al., 2005; http://amira.zib.de). Within Amira, the core liners, including about 2 mm of the core rims, were deleted from the data set. Mangan nodules with diameters 〉1 mm, open bioturbation traces, an unidentified organism (only present in core SO268-2-200-1 MC18), the natural bioturbated and surficial homogenised sediment were segmented by a marker-based watershed segmentation and visualized in 3D. Subsequently, the sediment components were quantified (MaterialStatistics module; volume per slice) and the mean and standard deviation of the sediment x-ray attenuation (MaterialStatistics module; statistics per slice per label; to avoid marginal averaging effects the sediment label was reduced by three voxels) were determined.
    Keywords: Binary Object; Bioturbation; Bioturbation, volume; Center for Marine Environmental Sciences; Clarion-Clipperton Fraction Zone, North East Pacific Ocean; Computed Tomography; Computer tomography (CT) Toshiba Aquilion 64; DEPTH, sediment/rock; File content; JPI Oceans - Ecological Aspects of Deep-Sea Mining; JPIO-MiningImpact; Manganese nodules, relative volume; Manganese nodules, volume; MARUM; Mining impact; MUC; MUC-12; MultiCorer; Number of slice; Number of voxels, matrix sediment; Sediment, bioturbated lower layer, relative volume; Sediment, bioturbated lower layer, volume; Sediment, homogenized upper layer, relative volume; Sediment, homogenized upper layer, volume; Sediment characterisation; SO268/1; SO268/1_50-2; Sonne_2; X-ray attenuation, matrix sediment, mean; X-ray attenuation, matrix sediment, standard deviation
    Type: Dataset
    Format: text/tab-separated-values, 10056 data points
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  • 15
    Publication Date: 2024-06-22
    Description: Oxygen isotopes in biogenic silica (δ18O BSi) from lake sediments allow for quantitative reconstruction of past hydroclimate and proxy–model comparison in terrestrial environments. The signals of individual records have been attributed to different factors, such as air temperature (T air ), atmospheric circulation patterns, hydrological changes and lake evaporation. Here, we provide 55 composite down–core records published to date and complemented with additional lake basin parameters (e.g. lake water residence time and catchment size) to best characterize the signal properties. Records feature widely different temporal coverage and resolution ranging from decadal–scale records covering the last 150 years to records with multi–millennial scale resolution spanning glacial–interglacial cycles. Best coverage in number of records (N=37) and datapoints (N=2112) is available for northern hemispheric (NH) extra–tropic regions throughout the Holocene (corresponding to Marine Isotope Stage 1; MIS 1).
    Keywords: 03-2K, 05-4P; AGE; Alps; Aluminium oxide; AWI Arctic Land Expedition; BAIK13; Baikal; BALGGU171; Baringo-Bogoria Basin; Baunt Lake; BD_4; BDP1996; BDP96-2; BNT14_1-8; BUCKET; Bucket water sampling; Co1309; Co1321; Co1412; COMPCORE; Compilation; Composite Core; CON01-6; CON01-603-2; CON01-605-3; Core; CORE; Core III; Corrected for contamination; D110; D160; delta O-18; Depth, composite bottom; Depth, composite mean; Depth, composite top; Depth, relative; Dethlingen; Diatom; Diatoms, δ18O; Diatoms, δ18O, standard deviation; DRILL; Drilling/drill rig; EC1; Elgygytgyn2003; Elgygytgyn crater lake, Sibiria, Russia; Event label; EWK; G7/02; Garba Guracha; GC; GL1; Grandfather Lake; Gravity corer; Hausberg Tarn; Heart Lake; HL-1; HT1; Identification; Kamchatka2007; KL_Mg; KOL; KTK2; KULC; KULLENBERG corer; L850; Laboratory code/label; Ladoga Lake, Russia; Lago Chungara; Laguna Verda Baja; Laguna Verde Alta; Laguna Zacapu; Lake 850; Lake Baikal, Russia; Lake Baikal/Academician Ridge; Lake Bolshoye Shchuchye, Polar Urals, Russia; Lake Brazi; Lake Challa; Lake Chuna; Lake Emanda; Lake Gosciaz; Lake Kotokel; Lake Malawi; Lake Petit; Lake Pinarbasi; Lake Pupuke; Lake Rutundu; Lake sediment core; Lake Spaime; Lake Stuor Goussasjavri; LB03-01; LB04-02; LC-1; LCHA-1; Les Echets; LG-1; Linsley Pond; Livingstone piston corer; LP1; LPC; LR-1; LS-1; LSG-1; LVA-1; LVB-1; Lz1024; Lz1029; M98-2P; MACC; Mackereth corer; Makgadikgadi; MBG-1; MC-2; Mica Lake; NAR0110; Nar Golu; Nettilling Lake; Ni-2B; northeastern Siberia; NW-Spain; OUTCROP; Outcrop sample; P2; P210; P260; paleoclimate proxy; PCOR; PCUWI; Percussion corer; PET09P2; PG1857-2; Piston corer, UWITEC; Piston corer (Kiel type); Piston corer Meischner large; PN94C; PTAU1; Raw data; RM1; RU-Land_2003_Elgygytgyn; RU-Land_2007_Kamchatka; RUSC; Russian corer; Sample code/label; Sampling/drilling in lake; Schrader Pond; SCP16-2A; Section; SEDCO; Sediment corer; SHT1; Silicon dioxide; SIL-MC; Simba Tarn; Small Hall Tarn; SQRL; Square-rod Livingston piston sampler; ST1; Sunken Island Lake; Tauca; TDB-1; TL1; Tonsberg Lake; Two-Yurts Lake; VAY1; Vereshchagin; Vuolep Allakasjaure; Yellowstone Lake; YL16-2C; ZAC/3; ZK2; δ13C, diatom-bound organic matter
    Type: Dataset
    Format: text/tab-separated-values, 19805 data points
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  • 16
    Publication Date: 2024-06-22
    Description: Oxygen isotopes in biogenic silica (δ18O BSi) from lake sediments allow for quantitative reconstruction of past hydroclimate and proxy–model comparison in terrestrial environments. The signals of individual records have been attributed to different factors, such as air temperature (T air ), atmospheric circulation patterns, hydrological changes and lake evaporation. Here, we provide 55 composite down–core records published to date and complemented with additional lake basin parameters (e.g. lake water residence time and catchment size) to best characterize the signal properties. Records feature widely different temporal coverage and resolution ranging from decadal–scale records covering the last 150 years to records with multi–millennial scale resolution spanning glacial–interglacial cycles. Best coverage in number of records (N=37) and datapoints (N=2112) is available for northern hemispheric (NH) extra–tropic regions throughout the Holocene (corresponding to Marine Isotope Stage 1; MIS 1).
    Keywords: 03-2K, 05-4P; Age, interval; Alps; Americium-241 (yes/no); Argon-40/Argon-39 chronology (yes/no); AWI Arctic Land Expedition; BAIK13; Baikal; BALGGU171; Baringo-Bogoria Basin; Baunt Lake; BD_4; BDP1996; BDP96-2; BNT14_1-8; BUCKET; Bucket water sampling; Caesium-137 (yes/no); Calendar age, maximum/old; Calendar age, minimum/young; Carbon-14, number of samples used for chronology; Carbon-14 chronology (yes/no); Catchment area; Chronology; Co1309; Co1321; Co1412; Comment; COMPCORE; Compilation; Composite Core; CON01-6; CON01-603-2; CON01-605-3; Continent; Core; CORE; Core III; Core length; Country; D110; D160; Dating; delta O-18; Depth, description; Depth, sampling; Dethlingen; Diatom; Diatoms, δ18O (yes/no); Discharge, average per year; DRILL; Drilling/drill rig; EC1; ELEVATION; Elgygytgyn2003; Elgygytgyn crater lake, Sibiria, Russia; Event label; EWK; From the HydroLakes database; From the original publication; G7/02; Garba Guracha; GC; Gear; GL1; Grandfather Lake; Gravity corer; Hausberg Tarn; Heart Lake; HL-1; HT1; Identification; Isotope notation; Isotopes, precipitation (yes/no); Isotopes, water (yes/no); Kamchatka2007; KL_Mg; KOL; KTK2; KULC; KULLENBERG corer; L850; Ladoga Lake, Russia; Lago Chungara; Laguna Verda Baja; Laguna Verde Alta; Laguna Zacapu; Lake; Lake, water depth, maximum; Lake, water depth, mean; Lake 850; Lake Baikal, Russia; Lake Baikal/Academician Ridge; Lake Bolshoye Shchuchye, Polar Urals, Russia; Lake Brazi; Lake Challa; Lake Chuna; Lake Emanda; Lake Gosciaz; Lake Kotokel; Lake Malawi; Lake Petit; Lake Pinarbasi; Lake Pupuke; Lake Rutundu; Lake sediment core; Lake Spaime; Lake Stuor Goussasjavri; Lake surface area; Lake Tilo; Lake type; Lake water volume; LATITUDE; LB03-01; LB04-02; LC-1; LCHA-1; Lead-210 (yes/no); Lead-214 (yes/no); Les Echets; LG-1; Linsley Pond; Livingstone piston corer; Location type; LONGITUDE; LP1; LPC; LR-1; LS-1; LSG-1; LT1; LVA-1; LVB-1; Lz1024; Lz1029; M98-2P; MACC; Mackereth corer; Magnetic susceptibility (yes/no); Makgadikgadi; MBG-1; MC-2; Mica Lake; NAR0110; Nar Golu; Nettilling Lake; Ni-2B; northeastern Siberia; Number of points; NW-Spain; Optically stimulated luminescence chronology (yes/no); OUTCROP; Outcrop sample; P2; P210; P260; paleoclimate proxy; Paleomagnetics (yes/no); PCOR; PCUWI; Percussion corer; Persistent Identifier; PET09P2; PG1857-2; Piston corer, UWITEC; Piston corer (Kiel type); Piston corer Meischner large; PN94C; Profile ID; PTAU1; Radium-226 (yes/no); Reference/source; Residence time; RM1; RU-Land_2003_Elgygytgyn; RU-Land_2007_Kamchatka; RUSC; Russian corer; Sampling/drilling in lake; Schrader Pond; SCP16-2A; SEDCO; Sediment corer; SHT1; SIL-MC; Simba Tarn; Small Hall Tarn; SQRL; Square-rod Livingston piston sampler; ST1; Sunken Island Lake; Tauca; TDB-1; Tephra/volcanic ash; Time resolution; TL1; Tonsberg Lake; Two-Yurts Lake; Type; Uranium-thorium chronology (yes/no); Used in paper for synthesis and analysis; Varve chronology (yes/no); VAY1; Vereshchagin; Vuolep Allakasjaure; Year of publication; Year of sampling; Yellowstone Lake; YL16-2C; ZAC/3; ZK2
    Type: Dataset
    Format: text/tab-separated-values, 2978 data points
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  • 17
    Publication Date: 2024-06-21
    Description: Stromboli (Italy) is an open-vent volcano with persistent explosive activity producing up to five hundred mild explosions per day. Fluctuations in explosion intensity, varying even by orders of magnitude in terms of emitted volume and their subsequent impact on the surrounding regions, sometimes occur abruptly. Consequently, identifying precursors of larger eruptive activities, particularly for more intense (paroxysmal) explosions, is challenging. In order to search for anomalies in the pre-paroxysm activity related to the summer 2019 eruption, we applied a hybrid method to the automatic analysis of geophysical and geochemical time series. This approach is based on the combination of two methods: 1. the Empirical Mode Decomposition (EMD) and 2. the Support Vector Regression (SVR). The aggregation of these two methods allowed us to identify anomalies in the patterns of the geophysical and geochemical parameters measured on Stromboli in a ten-month period including the July–August 2019 eruption. The results of this study are encouraging for an improvement of the monitoring systems and for volcano early warning applications.
    Description: This work has been supported by the INGV project Pianeta Dinamico 2023-2025 - ObseRvation, Measurement and modelling of Eruptive processes (ORME), and partially supported by the Progetto Strategico Dipartimentale INGV 2019 “Forecasting eruptive activity at Stromboli volcano: timing, eruptive style, size, intensity and duration” (FIRST, Delibera n. 144/2020; Scientific Responsibility: S.C.). Furthermore, this research has benefited from the support of Convenzione B2 DPC-INGV 2022-2024, Stromboli, Task 1.3 “Development of a unique activity index and estimation of the probability of the transition between ‘ordinary’ and ‘extraordinary’ eruptive activity”, and of the INGV project “Reti Multiparametriche”, Task A2 “Development of methods for the identification of precursors of Stromboli's paroxysms and major explosions based on multiparametric data analysis and study of possible early warning techniques”.
    Description: In press
    Description: 108131
    Description: OSV1: Verso la previsione dei fenomeni vulcanici pericolosi
    Description: JCR Journal
    Keywords: Stromboli volcano ; Volcanic monitoring ; Data analysis ; Multiparametric geophysics ; Paroxysmal explosions ; 04.08. Volcanology
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 18
    Publication Date: 2024-06-21
    Description: The Qinghai-Tibet Plateau (QTP) is characterized by a vast number of frozen and unfrozen freshwater reservoirs, which is why it is also called “the third pole” of the Earth or “Asian Water Tower”. We analyzed testate amoeba (TA) biodiversity and corresponding protozoic biosilicification in lake sediments of the QTP in relation to environmental properties (freshwater conditions, elevation, and climate). As TA are known as excellent bio-indicators, our results allowed us to derive conclusions about the influence of climate warming on TA communities and microbial biogeochemical silicon (Si) cycling. We found a total of 113 TA taxa including some rare and one unknown species in the analyzed lake sediments of the QTP highlighting the potential of this remote region for TA biodiversity. 〉1/3 of the identified TA taxa were relatively small (〈30 μm) reflecting the relatively harsh environmental conditions in the examined lakes. TA communities were strongly affected by physico-chemical properties of the lakes, especially water temperature and pH, but also elevation and climate conditions (temperature, precipitation). Our study reveals climate-related changes in TA biodiversity with consequences for protozoic biosilicification. As the warming trend in the QTP is two to three times faster compared to the global average, our results provide not only deeper insights into the relations between TA biodiversity and environmental properties, but also predictions of future developments in other regions of the world. Moreover, our results provide fundamental data for paleolimnological reconstructions. Thus, examining the QTP is helpful to understand microbial biogeochemical Si cycling in the past, present, and future.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
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  • 19
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    Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung
    In:  EPIC3Berichte zur Polar- und Meeresforschung = Reports on polar and marine research, Bremerhaven, Alfred-Wegener-Institut Helmholtz-Zentrum für Polar- und Meeresforschung, 786, 65 p., pp. 1-65, ISSN: 1866-3192
    Publication Date: 2024-06-21
    Repository Name: EPIC Alfred Wegener Institut
    Type: "Berichte zur Polar- und Meeresforschung" , notRev
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  • 20
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    American Meteorological Society
    In:  EPIC3Journal of Climate, American Meteorological Society, 37(8), pp. 2505-2518, ISSN: 0894-8755
    Publication Date: 2024-06-21
    Description: A fundamental statistic of climate variability is its spatiotemporal correlation function. Its complex structure can be concisely summarized by a frequency-dependent measure of the effective spatial degrees of freedom (ESDOF). Here we present, for the first time, frequency-dependent ESDOF estimates of global natural surface temperature variability from purely instrumental measurements, using the HadCRUT4 dataset (1850-2014). The approach is based on a newly developed method for estimating the frequency-dependent spatial correlation function from gappy data fields. Results reveal a multicomponent structure of the spatial correlation function, including a large-amplitude short-distance component (with weak time scale dependence) and a small-amplitude long-distance component (with increasing relative amplitude toward the longer time scales). Two frequency-dependent ESDOF measures are applied, each responding mainly to either of the two components. Both measures exhibit a significant ESDOF reduction from monthly to multidecadal time scales, implying an increase of the effective spatial scale of natural surface temperature fluctuations. Moreover, it is found that a good approximation to the global number of equally spaced samples needed to estimate the variance of global mean temperature is given, at any frequency, by the greater one of the two ESDOF measures, decreasing from ;130 at monthly to ;30 at multidecadal time scales. Finally, the multicomponent structure of the correlation function together with the detected ESDOF scaling properties indicate that the ESDOF reduction toward the longer time scales cannot be explained simply by diffusion acting on stochastically driven anomalies, as it might be suggested f rom simple stochastic-diffusive energy balance models.
    Repository Name: EPIC Alfred Wegener Institut
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  • 21
    Publication Date: 2024-06-21
    Description: Background: Wildfires are recognized as an important ecological component of larch-dominated boreal forests in eastern Siberia. However, long-term fire-vegetation dynamics in this unique environment are poorly understood. Recent paleoecological research suggests that intensifying fire regimes may induce millennial-scale shifts in forest structure and composition. This may, in turn, result in positive feedback on intensifying wildfires and permafrost degradation, apart from threatening human livelihoods. Most common fire-vegetation models do not explicitly include detailed individual-based tree population dynamics, but a focus on patterns of forest structure emerging from interactions among individual trees may provide a beneficial perspective on the impacts of changing fire regimes in eastern Siberia. To simulate these impacts on forest structure at millennial timescales, we apply the individual-based, spatially explicit vegetation model LAVESI-FIRE, expanded with a new fire module. Satellite-based fire observations along with fieldwork data were used to inform the implementation of wildfire occurrence and adjust model parameters. Results: Simulations of annual forest development and wildfire activity at a study site in the Republic of Sakha (Yakutia) since the Last Glacial Maximum (c. 20,000 years BP) highlight the variable impacts of fire regimes on forest structure throughout time. Modeled annual fire probability and subsequent burned area in the Holocene compare well with a local reconstruction of charcoal influx in lake sediments. Wildfires can be followed by different forest regeneration pathways, depending on fire frequency and intensity and the pre-fire forest conditions. We find that medium-intensity wildfires at fire return intervals of 50 years or more benefit the dominance of fire-resisting Dahurian larch (Larix gmelinii (Rupr.) Rupr.), while stand-replacing fires tend to enable the establishment of evergreen conifers. Apart from post-fire mortality, wildfires modulate forest development mainly through competition effects and a reduction of the model’s litter layer. Conclusion: With its fine-scale population dynamics, LAVESI-FIRE can serve as a highly localized, spatially explicit tool to understand the long-term impacts of boreal wildfires on forest structure and to better constrain interpretations of paleoecological reconstructions of fire activity.
    Repository Name: EPIC Alfred Wegener Institut
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  • 22
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    Academy of Sciences of the Republic of Sakha (Yakutia)
    In:  EPIC3ARCTIC AND SUBARCTIC NATURAL RESOURCES, Academy of Sciences of the Republic of Sakha (Yakutia), 28(4), pp. 584-594, ISSN: 2618-9712
    Publication Date: 2024-06-21
    Description: 〈jats:p〉This study presents the results of research on the climatic signal of radial growth of Siberian larch (〈jats:italic〉Larix cajanderi Mayr〈/jats:italic〉.) in the Omoloy River Basin, (north-eastYakutia). Tree-ring width chronologies were obtained from three sites  located in the valley complexes of subarctic tundra and forest-tundra ecotone, with chronologies spanning up to 498 years. Comparative analysis of radial growth dynamics and its statistical parameters indicated similar variability patterns within the study region. Dendroclimatic analysis revealed that the primary limiting factor determining the magnitude of radial growth in Siberianlarch is the air temperature during the first half of the growing season. Increasing temperatures have led to an increased role of precipitation and changes in the strength of growth-temperature correlations, especially in northern sites.This study highlights the potential for dendroclimatic and dendroecological researchin northern Yakutia.〈/jats:p〉
    Repository Name: EPIC Alfred Wegener Institut
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  • 23
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    Springer Nature
    In:  EPIC3International Journal of Biometeorology, Springer Nature, 68(4), pp. 1-17, ISSN: 0020-7128
    Publication Date: 2024-06-21
    Description: The Great Lakes region of North America has warmed by 1–2 °C on average since pre-industrial times, with the most pronounced changes observable during winter and spring. Interannual variability in temperatures remains high, however, due to the influence of ocean-atmosphere circulation patterns that modulate the warming trend across years. Variations in spring temperatures determine growing season length and plant phenology, with implications for whole ecosystem function. Studying how both internal climate variability and the “secular” warming trend interact to produce trends in temperature is necessary to estimate potential ecological responses to future warming scenarios. This study examines how external anthropogenic forcing and decadal-scale variability influence spring temperatures across the western Great Lakes region and estimates the sensitivity of regional forests to temperature using long-term growth records from tree-rings and satellite data. Using a modeling approach designed to test for regime shifts in dynamic time series, this work shows that mid-continent spring climatology was strongly influenced by the 1976/1977 phase change in North Pacific atmospheric circulation, and that regional forests show a strengthening response to spring temperatures during the last half-century.
    Repository Name: EPIC Alfred Wegener Institut
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  • 24
    Publication Date: 2024-06-21
    Description: Invasive alien species (IAS) threaten biodiversity and human well-being. These threats may increase in the future, necessitating accurate projections of potential locations and the extent of invasions. The main aim of the IAS prototype Digital Twin (IAS pDT) is to dynamically project the level of plant invasion at habitat level across Europe under current and future climates using joint species distribution models. The pDT detects updates in data sources and versions of the datasets and model outputs, implementing the FAIR principles. The pDT’s outputs will be available via an interactive dashboard. All input and output data will be freely accessible.
    Keywords: Invasive alien species ; Digital Twin ; climate change ; joint species distribution models ; Dynamic Data-Driven Application Systems ; workflows
    Repository Name: National Museum of Natural History, Netherlands
    Type: info:eu-repo/semantics/article
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  • 25
    Publication Date: 2024-06-21
    Description: Gut microbial communities are critical in determining the evolutive success of fruit fly phytophagous pests (Diptera, Tephritidae), facilitating their adaptation to suboptimal environmental conditions and to plant allelochemical defences. An important source of variation for the microbial diversity of fruit flies is represented by the crop on which larvae are feeding. However, a “crop effect” is not always the main driver of microbial patterns, and it is often observed in combination with other and less obvious processes. In this work, we aim at verifying if environmental stress and, by extension, changing environmental conditions, can promote microbial diversity in Zeugodacus cucurbitae (Coquillett), a cosmopolitan pest of cucurbit crops. With this objective, 16S rRNA metabarcoding was used to test differences in the microbial profiles of wild fly populations in a large experimental setup in Eastern Central Tanzania. The analysis of 2,973 unique ASV, which were assigned to 22 bacterial phyla, 221 families and 590 putative genera, show that microbial α diversity (as estimated by Abundance Coverage Estimator, Faith’s Phylogenetic Diversity, Shannon-Weiner and the Inverse Simpson indexes) as well as β microbial diversity (as estimated by Compositional Data analysis of ASVs and of aggregated genera) significantly change as the species gets closer to its altitudinal limits, in farms where pesticides and agrochemicals are used. Most importantly, the multivariate dispersion of microbial patterns is significantly higher in these stressful environmental conditions thus indicating that Anna Karenina effects contribute to the microbial diversity of Z. cucurbitae. The crop effect was comparably weaker and detected as non-consistent changes across the experimental sites. We speculate that the impressive adaptive potential of polyphagous fruit flies is, at least in part, related to the Anna Karenina principle, which promotes stochastic changes in the microbial diversity of fly populations exposed to suboptimal environmental conditions.
    Keywords: Crops ; Larvae ; Agriculture ; Crop management ; Insects ; Bacteria ; Fruits ; Pesticides
    Repository Name: National Museum of Natural History, Netherlands
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  • 26
    Publication Date: 2024-06-21
    Description: The emergence of alternative stable states in forest systems has significant implications for the functioning and structure of the terrestrial biosphere, yet empirical evidence remains scarce. Here, we combine global forest biodiversity observations and simulations to test for alternative stable states in the presence of evergreen and deciduous forest types. We reveal a bimodal distribution of forest leaf types across temperate regions of the Northern Hemisphere that cannot be explained by the environment alone, suggesting signatures of alternative forest states. Moreover, we empirically demonstrate the existence of positive feedbacks in tree growth, recruitment and mortality, with trees having 4–43% higher growth rates, 14–17% higher survival rates and 4–7 times higher recruitment rates when they are surrounded by trees of their own leaf type. Simulations show that the observed positive feedbacks are necessary and sufficient to generate alternative forest states, which also lead to dependency on history (hysteresis) during ecosystem transition from evergreen to deciduous forests and vice versa. We identify hotspots of bistable forest types in evergreen-deciduous ecotones, which are likely driven by soil-related positive feedbacks. These findings are integral to predicting the distribution of forest biomes, and aid to our understanding of biodiversity, carbon turnover, and terrestrial climate feedbacks.
    Repository Name: National Museum of Natural History, Netherlands
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  • 27
    Publication Date: 2024-06-21
    Description: As the largest instrumentally recorded earthquake in the fold‐and‐thrust belt of the northwestern Zagros mountain so far, the fault structure of the 2017 7.3 Sarpol‐e Zahab earthquake and its contribution to regional crustal shortening remain controversial. Here, we utilize the integration of Interferometric Synthetic Aperture Radar observations and 2D finite element models incorporating various fault geometries such as planar faults, ramp‐flat faults, and the combined models of ramp‐flat and splay faults to explore frictional afterslip process due to coseismic stress changes following the mainshock. Our findings suggest that a ramp‐flat frictional afterslip model, characterized by the maximum afterslip of ∼1.0 m and frictional variations (⁠ ⁠) of ∼0.001 and ∼0.0002 for the up‐dip and down‐dip portions, respectively, better explains the long‐wavelength postseismic deformation than planar fault models. However, an integration model of a ramp‐flat and a splay fault further improves the model fit, although the splay fault’s frictional slip is limited to 〈0.2 m, which is much smaller than that on the ramp‐flat part (∼0.9 m). Considering the relocated aftershocks and structural cross‐sections, the combined model could be best attributed to fault slip on the blind Mountain Front fault. Our findings thus suggest the complexity of the fault interactions between the basement and sedimentary cover in the Zagros, and that this largest basement‐involved event in the region contributes to both thick‐ and thin‐skinned shortening via seismic and aseismic behaviors, respectively.
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  • 28
    Publication Date: 2024-06-21
    Description: The earthquake, which occurred in Yogyakarta, Indonesia, on May 26, 2006, at 22:53:58 UTC with Mw ∼6.4, was one of the most destructive earthquakes in Indonesia. The earthquake caused thousands of fatalities, tens of thousands of injuries, and hundreds of thousands of house damages in the Yogyakarta area and its surroundings at a loss of billions of dollars. Previous studies from seismic tomography and satellite radar imaging hypothesized that the earthquake was caused by activating a so far unknown fault east of the Opak Fault. Although, in the beginning, the Opak fault was suspected to be the source of the Yogyakarta earthquake in 2006. This assumption was made because the damage was maximum in the Bantul area west of the Opak Fault. This study demonstrates that our seismic tomography achieved a higher resolution than the previous study and could resolve a failed complex fault system. We utilized more aftershocks (2170 events) and smaller grid sizes for seismic tomography inversion. Four focal mechanisms from aftershocks for Mw ≥ 4.5 were also conducted to support structure interpretation in the study area. Our results successfully delineate the Opak Fault and the second fault, namely the Ngalang Fault, parallel to the eastern part of the fault at a depth of 9 km. Two faults could be indicated by the velocity contrast of Vp, Vp/Vs ratio, and Vs from a horizontal section tomogram. Our focal mechanisms also support seismic tomography, revealing two fault planes in our study area. The results show that the two faults are connected by the Oyo Fault, which is ruptured in the opposite direction compared to the two faults.
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  • 29
    Publication Date: 2024-06-21
    Description: Large igneous provinces (LIP) are vast (0.2 to 〉1 Mkm3) outpourings of basaltic lava and voluminous intrusions of magmas that have had important environmental consequences, in many cases leading to immense greenhouse gas release and mass extinctions. Magmatic oxygen fugacity (fO2) influences the chemistry of volcanic gases and is an important parameter for examining the links between LIP eruptions and environmental change. To constrain the fO2 of LIP magmas, we report olivine elemental chemistry of 399 crystals from a set of fifteen olivine-rich LIP samples, spanning in age from the Proterozoic (∼1270 Ma) to the Miocene (∼17 Ma). Concentrations of V in olivine are used to show that mafic LIP lavas erupted at +1.20 ± 0.95 ΔFMQ, on average more oxidized than mid ocean ridge basalts (MORB) at −0.28 ± 0.28 ΔFMQ. Mafic LIP magmas show a much larger range than MORB, however. Additionally, fO2 shows a negative correlation with parental magma MgO content, with high MgO lavas approaching the MORB range. This correlation is likely due to sampling of a heterogeneous mixture of oxidized and reduced lithologies, as also sampled by ocean island basalts (OIB). Correlation between fO2 and isotopic ratios such as 143Nd/144Nd demonstrates that the oxidized endmember is geochemically enriched, and may result from subduction recycling of oxidized surficial materials. The high fO2 of primitive LIP magmas demonstrate that they largely emitted oxidized gases during eruption, and furthermore, that LIP magmas associated with mass extinctions have similar magmatic fO2 to those that are not. Global plate tectonic position, magnitude and duration of LIP volcanic eruptions and magmatic degassing, as well as interaction with sedimentary basins in the crust - but not mantle source fO2 - are likely to be the critical factors for whether a LIP was associated with a mass extinction.
    Language: English
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  • 30
    Publication Date: 2024-06-21
    Type: info:eu-repo/semantics/workingPaper
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  • 31
    Publication Date: 2024-06-21
    Description: The mean sea surface in different regions is non-equipotential, rendering Vietnam’s traditional approach, which relies on the Hon-Dau tide gauge station as a reference, not yet scientifically invalid. To overcome this, our study utilized the Vietnam national mean dynamic topography model (MDTVN22) for depth observations, particularly in the Gulf of Tonkin. Covering 3430 monitoring sites in Hai Phong and 813 sites in Quang Ninh, our experiments highlighted a 5 to 6 mm difference between the mean sea surface and MDTVN22 references. • Our research establishes a resilient methodology, integrating shore tide gauge station data and the MDTVN22 model, aimed at enhancing precision in depth observations. • Validation experiments in Hai Phong demonstrate a minimal discrepancy of ±0.006 m be- tween measurements obtained from the traditional mean sea surface and the MDTVN22 model. • These findings underscore the significance of adopting the MDTVN22 model for improved accuracy in assessing Vietnam’s seabed topography.
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  • 32
    Publication Date: 2024-06-21
    Description: Reported fault slip rates, a key quantity for earthquake hazard and risk analyses, have been inconsistent for the northern Dead Sea fault (DSF). Studies of offset geological and archeological structures suggest a slip rate of 4 to 6 millimeters per year, consistent with the southern DSF, whereas geodetic slip-rate estimates are only 2 to 3 millimeters per year. To resolve this inconsistency and overcome limited access to the northern DSF in Syria, we here use burst-overlap interferometric time-series analysis of satellite radar images to provide an independent slip-rate estimate of ~2.8 millimeters per year. We also show that the high geologic slip rate could, by chance, be inflated by earthquake clustering and suggest that the slip-rate decrease from the southern to northern DSF can be explained by splay faults and diffuse offshore deformation. These results suggest a microplate west of the northern DSF and a lower earthquake hazard for that part of the fault.
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  • 33
    Publication Date: 2024-06-21
    Description: Eruptions of volcanoes and geysers share many fundamental similarities: for example, they are manifestations of Earth’s geothermal energy, involving the pressure-driven expulsion of fluids from the Earth’s interior. However, while volcanoes can produce spectacular lava bubbles that burst, water bubbles are rarely observed on the surface of geysers. It is still unclear why some of these low-viscosity geyser systems produce none, while others produce them regularly. There is no quantification of the size, speed, and height of these bubbles at geysers, which is the gap we fill here. Strokkur creates a water bulge in its surface pool (bulge stage). When the bulge bursts, water is ejected into the air (jet stage). The steam then continues to rise buoyantly and drift away (drift stage). Here we study the evolution of the three stages using records from video camera campaigns and a local seismic network. We find that larger bulges are associated with larger ascent velocities and cause larger jet heights. As energy is channeled into a high jet, small seismic ground motions are recorded. The bulge formation itself is barely visible seismically. Our work suggests that the 0.74±0.27 s-long bulge stage can be used as a first-order proxy for predicting eruption height. This study might also be relevant for understanding fluid dynamics in volcanic systems.
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  • 34
    Publication Date: 2024-06-21
    Description: Ab Weihnachten 2023 kam es zu einer Hochwassersituation vor allem im Bereich der Flüsse Ems, Weser und Elbe, welche bis in den Januar 2024 hinein zu einer angespannten Lage vor allem in weiten Teilen Nordwestdeutschlands führte. Dieses Winterhochwasser wurde ausgelöst durch großräumige Dauerniederschläge vor allem in Norddeutschland über Weihnachten 2023 (19.-25.12.2023) und verstärkt durch nachfolgende, wenn auch schwächere Niederschlagsereignisse bis Anfang Januar 2024, welche darüber hinaus auf bereits gesättigte Böden trafen. Die Ungewöhnlichkeit des Weihnachtsniederschlagsereignisses bestand in seiner großen räumlichen Ausdehnung und langen zeitlichen Andauer von sieben Tagen. Es hing zusammen mit einer Wetterlage (charakterisiert durch ein ausgedehntes Tiefdrucksystem mit Zentrum über Südskandinavien), welche an sich nicht außergewöhnlich war, jedoch extrem lange andauerte. Das spezifische räumliche Muster dieses einwöchigen Niederschlagsereignisses war auch in der Vergangenheit sowohl mit ergiebigen Dauerniederschlägen als auch mit der zuvor erwähnten Wetterlage assoziiert. Die nachfolgenden Niederschlagsereignisse Ende Dezember und Anfang Januar waren für sich betrachtet wesentlich schwächer. Deren zeitliches Zusammenspiel mit dem vorherigen Weihnachtsereignis führte jedoch dazu, dass gebietsweise über lange Zeiträume von bis zu zweieinhalb Wochen extreme mittlere Niederschlagsintensitäten auftraten. Das Hochwasser als Auswirkung der Niederschläge war ebenfalls im Wesentlichen durch seine große räumliche Ausdehnung charakterisiert, nur vereinzelt wurden extreme Flusspegelstände gemessen. Unter allen Hochwassern in Deutschland seit 1955 (für welche die Abflüsse über zwei Wochen eine Wiederkehrzeit von mindestens 10 Jahren aufwiesen) rangiert die räumliche Ausdehnung des Weihnachtshochwassers 2023 mit gut 100.000 km² auf Platz 9. Die räumliche Ausdehnung ist hierbei nicht die Überflutungsfläche, sondern die Fläche, in der die Hochwasserabflüsse einen bestimmten Schwellenwert überschreiten. Die Überflutungsfläche selbst erreichte eine Ausdehnung von ca. 1000 km² und betraf mehr als 40 Landkreise, vor allem in Niedersachsen und Bremen, aber auch in Teilen Hessens und Nordrhein-Westfalens. Betroffen waren dabei, je nach Abschätzung, 18.000 bis 30.000 Personen, rund 2000 Gebäude, 4,6 km² bebaute Fläche und 470 km Straßen. Die im Dezember 2023 gemessene Monatsniederschlagssumme von 164 mm (über einem besonders von den Niederschlägen betroffenen Gebiet in Niedersachsen: 51,5°N - 53,5°N, 8,0°O - 11,0°O) tritt in den Wintermonaten im heutigen Klima durchschnittlich nur ca. alle 120 Jahre auf. Eine Attributionsstudie des Deutschen Wetterdienstes (DWD) zeigt, dass sich die Wahrscheinlichkeit für ein Ereignis dieser Intensität aufgrund der bisherigen Klimaerwärmung von 1,2°C (seit etwa 1900) um den Faktor 1,8 (Ergebnisspanne: 0,1 bis 140) erhöht hat, und dass sich diese Wahrscheinlichkeit im Falle eines 2°C wärmeren Klimas, d.h. einer zusätzlichen Erwärmung um weitere 0,8°C, nochmals erhöhen wird. Die Studie zeigt jedoch auch, dass diese Abschätzungen mit großen Unsicherheiten verbunden sind. Dennoch sind diese Abschätzungen konsistent mit den Ergebnissen verschiedener Studien, welche sowohl eine Zunahme des mittleren Winterniederschlags zeigen als auch eine Intensivierung extremer Niederschlagsereignisse im nördlichen Mitteleuropa.
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  • 35
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    In:  Hydrology and Earth System Sciences
    Publication Date: 2024-06-21
    Description: Extremely large floods that far exceed previously observed records are often considered virtually “impossible”, yet they are an ever-present threat similar to the sword suspended over the head of Damocles in the classical Greek anecdote. Neglecting such floods may lead to emergency situations where society is unprepared and to disastrous consequences. Four reasons why extremely large floods are often considered next to impossible are explored here, including physical (e.g. climate change), psychological, socio-economic and combined reasons. It is argued that the risk associated with an “impossible” flood may often be larger than expected and that a bottom-up approach should be adopted that starts from the people affected and explores possibilities of risk management, giving high priority to social in addition to economic risks. Suggestions are given for managing this risk of a flood considered impossible by addressing the diverse causes of the presumed impossibility.
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  • 36
    Publication Date: 2024-06-21
    Description: Double seismic zones (DSZs) are a feature of some subducting slabs, where intermediate-depth earthquakes (~70–300 km) align along two separate planes. The upper seismic plane is generally attributed to dehydration embrittlement, whereas mechanisms forming the lower seismic plane are still debated. Thermal conductivity of slab minerals is expected to control the temperature evolution of subducting slabs, and therefore their seismicity. However, effects of the potential anisotropic thermal conductivity of layered serpentine minerals with crystal preferred orientation on slab’s thermal evolution remain poorly understood. Here we measure the lattice thermal conductivity of antigorite, a hydrous serpentine mineral, along its crystallographic b- and c-axis at relevant high pressure-temperature conditions of subduction. We find that antigorite’s thermal conductivity along the c-axis is ~3–4 folds smaller than the b-axis.Our numericalmodels further reveal thatwhen the lowthermal-conductivity c-axis is aligned normal to the slab dip, antigorite’s strongly anisotropic thermal conductivity enables heating at the top portion of the slab, facilitating dehydration embrittlement that causes the seismicity in the upper plane of DSZs. Potentially, the antigorite’s thermal insulating effect also hinders the dissipation of frictional heat inside shear zones, promoting thermal runaway along serpentinized faults that could trigger intermediatedepth earthquakes.
    Language: English
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  • 37
    Publication Date: 2024-06-21
    Description: Dust deposited on the surface of snow and glaciers can significantly reduce the snow and ice albedo and accelerate melting. Manual observations of the dust mass concentration (DMC) on snow and glacier surfaces are routinely performed at many locations worldwide. However, snow and ice surface DMC monitoring methods based on remote sensing data still face challenges. This study presents a new retrieval scheme for estimating dust load on snow-covered surfaces from MODIS and VIIRS in Northeast and Northwest China that utilizes a classical snow radiative transfer model. Our results indicate that the coefficient of variation (CV) of DMC retrieved from in situ measurements of snow spectral reflectance is 4%, which is within a +4% difference compared to DMC observed in snow and ice samples. Estimating atmospheric dust pollutants content deposited on snow surfaces based on satellite remote sensing observations is feasible. In Northwest China, the root mean square error (RMSE) of the DMC values retrieved from VNP09GA data is 9.78 ppm, while that of the DMC values retrieved from MOD09GA data is 13.74 ppm. In Northeast China, the RMSE of the DMC values retrieved from VNP09GA data is 73.98 ppm, while that of the DMC values retrieved from MOD09GA data is 184.32 ppm. The research results can realize continuous monitoring of the atmospheric dust pollutants deposited on snow surfaces, which is of great practical significance to understanding and studying the pollution process of atmospheric dust on snow.
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  • 38
    Publication Date: 2024-06-21
    Description: Previous studies have shown that it is difficult to determine whether the 2015 Pishan earthquake occurred on a uniform fault or a ramp-flat fault with variable dip angles due to the similar goodness of data fit to coseismic and afterslip models on these two fault models. Here, we first present the InSAR deformation obtained from both ascending and descending orbits, covering the coseismic period and cumulative 5-yr period after the 2015 Pishan earthquake. We then determine the preferred fault geometry by the spatial distributions between the positive Coulomb failure stress change triggered by main shock and the afterslip. Based on the preferred fault model, we finally use a combined model to determine the contributions of elastic and viscoelastic deformation in the post-seismic deformation. We find that the Pishan earthquake prefers to occur on a ramp-flat fault, and the coseismic slip is mainly distributed at a depth of 9–13 km, with a maximum slip of about 1.3 m. The post-seismic deformation is primarily governed by afterslip, as the poroelastic rebound-induced deformation fails to account for the observed post-seismic deformation and the contributions from the viscoelastic relaxation mechanism can be considered negligible in the combined model. Moreover, the modelled stress-driven afterslip and observed kinematic afterslip have good consistency, and the difference between the root mean square error of the two afterslip models is only 4.3 mm. The results from the afterslip model indicate that both of the updip and downdip directions distribute the afterslip, and slip in the updip direction is greater than that of the downdip direction. Meanwhile, the maximum cumulative afterslip after 5 yr is approximately 0.26 m which is equivalent to a released seismic moment of a Mw 6.47.
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  • 39
    Publication Date: 2024-06-21
    Description: Common environmental adsorbents (clay minerals, metal-oxides, metal-oxyhydroxides and organic matter) can significantly impact the chemistry of aqueous fluids via adsorption–desorption reactions. The dissolved chemistry of rivers have routinely been used to quantify silicate mineral dissolution rates, which is a key process for removing carbon dioxide (Image 1) from the atmosphere over geological timescales. The sensitivity of silicate weathering rates to climate is disproportionately weighted towards regions with high erosion rates. This study quantifies the impact of adsorption-desorption reactions on the chemistry of three large Himalayan rivers over a period of two years, utilising both the adsorbed and dissolved phases. The concentration of riverine adsorbed cations are found to vary principally as a function of the concentration and cation exchange capacity (CEC) of the suspended sediment. Over the study period, the adsorbed phase is responsible for transporting ∼70% of the mobile (adsorbed and dissolved) barium and ∼10% of the mobile calcium and strontium. The relative partitioning of cations between the adsorbed and dissolved phases follows a systematic order in both the monsoon and the dry-season (preferentially adsorbed: Ba 〉 Sr & Ca 〉 Mg & K 〉 Na). Excess mobile sodium (Image 2=Na-Cl) to silicon (Si) riverine ratios are found to vary systematically during an annual hydrological cycle due to the mixing of low temperature and geothermal waters. The desorption of sodium from uplifted marine sediments is one key process that may increase the Na*/Si ratios. Accounting for the desorption of sodium reduces silicate weathering rate estimates by up to 83% in the catchments. This study highlights that surficial weathering processes alone are unable to explain the chemistry of the rivers studied due to the influence of hydrothermal reactions, which may play an important role in limiting the efficiency of silicate weathering and hence modulating atmospheric Image 1 concentrations over geological time.
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  • 40
    Publication Date: 2024-06-21
    Description: Tourmaline is common in rare element pegmatites of the Nb-Y-F (NYF) type in the south-central part of the Proterozoic Sveconorwegian orogen in southern Norway. In the global context, however, tourmaline appears rare in this type of pegmatite. This study aims to explain the unusual tourmaline abundance in these pegmatites and the origin of boron (B) in the respective melts, and to raise awareness of tourmaline in NYF pegmatites generally. Tourmalines from six pegmatites in three Sveconorwegian lithotectonic units: Bamble, Kongsberg and Idefjorden, were investigated in terms of their mineral chemistry and δ11B values, in addition to bulk rock analyses of pegmatites and host rocks. Tourmalines in pegmatites from Bamble and Kongsberg record B isotopic compositions (δ11B = -1.0 to + 9.9 ‰) that are heavy relative to continental crust and mantle sources. In contrast, tourmaline in pegmatites and host rocks from Idefjorden have light B isotopic ratios (δ11B = -14.8 to −12.5 ‰) that are typical crustal values. We suggest that the latter melts were sourced from orthogneisses at depth. We relate the heavy B isotopic composition of Bamble and Kongsberg pegmatites to regional Na-metasomatism by fluids sourced from Mesoproterozoic shallow marine sediments. This is supported by previously published δ11B ratios from metasomatized Bamble host rocks. The spatial association of pegmatites with Na-metasomatism in the basement rocks suggests that metasomatism enhanced the fertility and B-concentration in the affected lithologies, favouring partial melting and the formation of tourmaline-bearing pegmatites. These findings contribute to understanding the petrogenesis of Sveconorwegian pegmatites but they also imply that B can play a greater role in the formation of NYF pegmatites than previously thought and that tourmaline has value as a petrogenetic tool in this type of pegmatites as well as in the Li-Cs-Ta (LCT) type to which is it is more commonly applied.
    Language: English
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  • 41
    Publication Date: 2024-06-21
    Keywords: 40Ar/39Ar geochronology; Age, mineral; Age, standard deviation; Analysis; argon; biotite; Calculated, 2 sigma; ELEVATION; Geological sample; GEOS; Himalaya; hornblende; LATITUDE; LONGITUDE; Marsyangdi_Valley; Mineral age, Biotite; muscovite; Sample ID; thermochronology
    Type: Dataset
    Format: text/tab-separated-values, 36 data points
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  • 42
    Publication Date: 2024-06-21
    Keywords: 40Ar/39Ar geochronology; Age, mineral; Age, standard deviation; Analysis; argon; biotite; Calculated, 2 sigma; ELEVATION; Geological sample; GEOS; Himalaya; hornblende; LATITUDE; LONGITUDE; Marsyangdi_Valley; Mineral age, Biotite; muscovite; Sample ID; thermochronology
    Type: Dataset
    Format: text/tab-separated-values, 80 data points
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  • 43
    Publication Date: 2024-06-21
    Description: Liquid water content and total water content from the Nevzorov probe, collected during the HALO-AC³ campaign out of Longyearbyen, Svalbard in April 2022. The dataset contains measurements from the three collector sensors of the Nevzorov probe. These are the cylindrical LWC sensor, the 8 mm TWC cone and the 12 mm TWC cone (for a description of the probe see doi:10.1175/1520-0426(1998)015〈1495:TNAHWL〉2.0.CO;2, doi:10.5194/egusphere-2022-647 ). Furthermore, corrected LWC and TWC values are contained in the dataset. These values are best estimates of LWC and TWC. They are computed by solving a system of equations and they consider collection efficiencies, the different latent heats of water and ice and the sensitivity of the LWC sensor to ice particles. For a description of the computation see Lucke et al. (2023) (doi:10.4271/2023-01-1485). However, for this data, the 12 mm cone was not included in the computation, as its data were deemed to be too unreliable in conditions where droplet diameters are low. NaNs are represented as 9999.999 in the dataset. The dataset only contains research flight 8 - 13. For the previous flights a problem with the probe existed and no data was recorded.
    Keywords: AC; Aircraft; Arctic; Arctic Amplification; Date/Time of event; Event label; HALO - (AC)3; HALO-(AC)³; HALO-AC3_20220401_P6_RF08; HALO-AC3_20220404_P6_RF09; HALO-AC3_20220405_P6_RF10; HALO-AC3_20220408_P6_RF11; HALO-AC3_20220409_P6_RF12; HALO-AC3_20220410_P6_RF13; ice water content; IWC; liquid water content; LWC; mixed-phase clouds; netCDF file; netCDF file (File Size); NEVZ; Nevzorov probe; P6_231_HALO_2022_2204011101; P6_231_HALO_2022_2204041201; P6_231_HALO_2022_2204051301; P6_231_HALO_2022_2204081401; P6_231_HALO_2022_2204091501; P6_231_HALO_2022_2204101601; P6-231_HALO_2022; Polar 6; POLAR 6; Polarimetric Radar Observations meet Atmospheric Modelling (PROM) - Fusion of Radar Polarimetry and Numerical Atmospheric Modelling Towards an Improved Understanding of Cloud and Precipitation Processes; SPP2115_PROM; Svalbard; total water content; TWC
    Type: Dataset
    Format: text/tab-separated-values, 6 data points
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  • 44
    Publication Date: 2024-06-21
    Description: During the HALO-(AC)³ aircraft campaign in 2022, onboard of Polar 6 aircraft, refractory black carbon (BC) mass and number concentration was measured by a single particle soot photometer (SP2) in the mass equivalent diameter range of 70-675 nm. The instrument was installed behind the counter-flow virtual impactor (CVI) inlet, and therefore measured the BC properties of cloud residuals when the aircraft flew through clouds and the counter flow was switched on. During out-of cloud measurements, the counter flow of the CVI was switched off and the instrument measured the total aerosol's BC properties. In the data files, the column CVI_flag indicates if total aerosol was sampled (value of 0), cloud residuals were sampled (value of 1). A CVI_flag value of 2 indicates that the inlet counter flow was currently switched on or off and therefore the measurement is not valid. The provided time resolution is 3 seconds.
    Keywords: AC3; aerosol; Arctic Amplification; black carbon; CVI; HALO-(AC)³; Polar 6; SP2
    Type: Dataset
    Format: application/zip, 10 datasets
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  • 45
    Publication Date: 2024-06-21
    Keywords: 40Ar/39Ar geochronology; Age, mineral; Age, standard deviation; Analysis; argon; biotite; Calculated, 2 sigma; ELEVATION; Geological sample; GEOS; Himalaya; hornblende; LATITUDE; LONGITUDE; Marsyangdi_Valley; Mineral age, Biotite; muscovite; Sample ID; thermochronology
    Type: Dataset
    Format: text/tab-separated-values, 160 data points
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  • 46
    Publication Date: 2024-06-21
    Description: Vegetated coastal ecosystems have been increasingly recognized for their capacity to sequester organic carbon in their soils and sediments under the term blue carbon. The vegetation of these habitats shows specific adaptations to severe abiotic soil conditions, particularly, waterlogging and salinity, and supports therefore ecosystem functioning and services. Wadden Sea salt marshes in Schleswig-Holstein (Germany) have been utilized for high density sheep grazing over centuries. At the beginning of the 1990s, in many parts of salt marshes livestock densities were reduced and the maintenance of the anthropogenic drainage system was ceased. In 2012, 17 years after the change of land utilization, the contents, densities, and accumulation rates of surface soil carbon were investigated at 50 sampling positions with different elevations along eight transects in Wadden Sea mainland salt marshes at Hamburger Hallig, Schleswig-Holstein, Germany, under different livestock grazing regimes (ungrazed, moderately grazed, intensively grazed). Surface soil was collected in 150 permanent plots (2 m * 2 m) at 50 sampling positions, covering a salt marsh area of 1050 ha. The carbon contents, pH, and bulk density were determined from dried soil. The elevations of the 150 permanent plots were measured and annual vertical accretion rates were calculated from 17 years sedimentation monitoring. This study was supported by the BASSIA project (Biodiversity, management, and ecosystem functions of salt marshes in the Wadden Sea National Park of Schleswig-Holstein), funded by the Bauer-Hollmann Foundation and Universität Hamburg.
    Keywords: Agrostis stolonifera, cover; Armeria maritima, cover; Artemisia maritima, cover; Aster tripolium, cover; Atriplex littoralis, cover; Atriplex portulacoides, cover; Atriplex prostrata, cover; blue carbon; Calculated; Climate change; DATE/TIME; Density, dry bulk; Depth, soil, maximum; Distance; ELEVATION; Elymus athericus, cover; Elymus repens, cover; Festuca rubra, cover; Glaux maritima, cover; inorganic and organic carbon stock; Inorganic carbon, soil; Juncus gerardii, cover; Limonium vulgare, cover; Livestock density; Multi parameter analyser, Eijkelkamp, 18.28; Optical levelling instrument; Organic carbon, soil; pH; Plantago coronopus, cover; Plantago maritima, cover; Plot of land; Potentilla anserina, cover; Puccinellia maritima, cover; Salicornia europaea, cover; Sample position; Sea level rise; Soil corer; Sonchus asper, cover; Sonchus sp., cover; Spartina anglica, cover; Spergularia maritima, cover; SSC_2012_HH-SH-G; Suaeda maritima, cover; tidal wetland; TMAP Wadden Sea Vegetation Database (Stock 2012); Total organic carbon (TOC) analyzer, Elementar, Liqui-TOC; coupled with extension module, Elementar, soliTIC; Triglochin maritima, cover; Vegetation, cover; Vegetation type; Vertical accretion rate, annual mean; Wadden Sea, Germany
    Type: Dataset
    Format: text/tab-separated-values, 5300 data points
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  • 47
    Publication Date: 2024-06-21
    Description: One of the main goals of the HALO-(AC)3 Arctic airborne campaign conducted in spring 2022 was a quasi-Lagrangian sampling of air masses. This means that the same air masses were to be sampled twice. Such a measurement strategy allows for concrete observations of air mass transformations, which can for example be used to benchmark weather models. After finishing the campaign, trajectory calculations were conducted for all flights of the HALO aircraft to check whether the flight strategy was a success. For this, the trajectory calculation tool Lagranto was used in conjunction with wind fields from the ERA5 reanalysis. Latter has an output resolution of around 30 km and one hour. The hourly data was bi-linearly interpolated to one minute resolution. Air masses were initialized temporally every one minute along the flight track of HALO, and vertically every 5 hPa between 250 hPa and 10 hPa above the ground level. Horizontally, air masses were started within a 30 km radius circle centered around the location of HALO. In each circle, 30 air masses were initialized evenly spaced approximately every 10 km, allowing for a better statistical analysis. Trajectories were then calculated in one-minute steps up to 10 hours forward in time. At typical HALO flight times of up to 10 hours, around 2.7 million trajectories were calculated per research flight. A quasi-Lagrangian match is registered if the same air mass is seen again below HALO at a later time of the same day and within the same 30 km radius. In order to allow air masses to evolve, a minimum temporal threshold of one hour was applied between matches.
    Keywords: AC; AC3; Aircraft; Arctic; Arctic Amplification; Date/Time of event; Event label; HALO; HALO_220312a; HALO_220313a; HALO_220314a; HALO_220315a; HALO_220316a; HALO_220320a; HALO_220321a; HALO_220328a; HALO_220329a; HALO_220330a; HALO_220401a; HALO_220404a; HALO_220407a; HALO_220408a; HALO_220410a; HALO_220411a; HALO_220412a; HALO_AC3; HALO-(AC)³; Image; Lagrangian data; Optional event label; RF02; RF03; RF04; RF05; RF06; RF07; RF08; RF09; RF10; RF11; RF12; RF13; RF14; RF15; RF16; RF17; RF18; Text file; trajectories
    Type: Dataset
    Format: text/tab-separated-values, 34 data points
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  • 48
    Publication Date: 2024-06-21
    Description: One of the main goals of the HALO-(AC)3 Arctic airborne campaign conducted in spring 2022 was a quasi-Lagrangian sampling of air masses. This means that the same air masses were to be sampled twice. Such a measurement strategy allows for concrete observations of air mass transformations, which can for example be used to benchmark weather models. After finishing the campaign, trajectory calculations were conducted for all flights of the HALO aircraft to check whether the flight strategy was a success. For this, the trajectory calculation tool Lagranto was used in conjunction with wind fields from the ERA5 reanalysis. Latter has an output resolution of around 30 km and one hour. The hourly data was bi-linearly interpolated to one minute resolution. Air masses were initialized temporally every one minute along the flight track of HALO, and vertically every 5 hPa between 250 hPa and 10 hPa above the ground level. Horizontally, air masses were started within a 30 km radius circle centered around the location of HALO. In each circle, 30 air masses were initialized evenly spaced approximately every 10 km, allowing for a better statistical analysis. Trajectories were then calculated in one-minute steps up to 32 hours forward in time. At typical HALO flight times of up to 10 hours, around 2.7 million trajectories were calculated per research flight. A quasi-Lagrangian match is registered if the same air mass is seen again below HALO on the subsequent day and within the same 30 km radius.
    Keywords: AC; AC3; Aircraft; Arctic; Arctic Amplification; Date/Time of event; Event label; HALO; HALO_220312a; HALO_220313a; HALO_220314a; HALO_220315a; HALO_220320a; HALO_220328a; HALO_220329a; HALO_220407a; HALO_220410a; HALO_220411a; HALO_AC3; HALO-(AC)³; Image; Lagrangian data; Optional event label; RF02; RF03; RF04; RF05; RF07; RF09; RF10; RF14; RF16; RF17; Text file; trajectories
    Type: Dataset
    Format: text/tab-separated-values, 30 data points
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  • 49
    Publication Date: 2024-06-21
    Description: This data set is composed of in-situ measurement of arctic cloud microphysical properties (particle size distribution and volumic cloud particle scattering properties) observed during the HALO-AC3 campaign, which occurred between March 20th and April 10th 2022. These measurements were made using the 2D stereoscopic (2D-S, SPEC Inc.) and Polar Nephelometer (Gayet et al., 1997) probes from the airborne measurement platform of the Laboratoire de Météorologie Physique (CNRS/UCA, Aubière, France). There is one file per flight. All files are in NetCDF format, with a complete description of the parameters inside. A detailed list of the parameters present in the data set is added in a separate document (see "Further details" link).
    Keywords: 2D-S Stereo Probe, SPEC Inc., and Polar Nephelometer according to Gayet et al. (1997); AC; AC3; Aircraft; Arctic; Arctic Amplification; Atmospheric and Earth System Research with HALO – High Altitude and Long Range Research Aircraft; Cloud Microphysics; Date/Time of event; Event label; HALO - (AC)3; HALO-(AC)³; HALO-AC3_20220320_P6_RF01; HALO-AC3_20220322_P6_RF02; HALO-AC3_20220326_P6_RF04; HALO-AC3_20220328_P6_RF05; HALO-AC3_20220329_P6_RF06; HALO-AC3_20220330_P6_RF07; HALO-AC3_20220401_P6_RF08; HALO-AC3_20220404_P6_RF09; HALO-AC3_20220405_P6_RF10; HALO-AC3_20220408_P6_RF11; HALO-AC3_20220409_P6_RF12; HALO-AC3_20220410_P6_RF13; In-Situ Measurements; netCDF file; netCDF file (File Size); P6_231_HALO_2022_2203200401; P6_231_HALO_2022_2203220501; P6_231_HALO_2022_2203260702; P6_231_HALO_2022_2203280801; P6_231_HALO_2022_2203290901; P6_231_HALO_2022_2203301001; P6_231_HALO_2022_2204011101; P6_231_HALO_2022_2204041201; P6_231_HALO_2022_2204051301; P6_231_HALO_2022_2204081401; P6_231_HALO_2022_2204091501; P6_231_HALO_2022_2204101601; P6-231_HALO_2022; Polar 6; POLAR 6; SPP1294; Svalbard
    Type: Dataset
    Format: text/tab-separated-values, 12 data points
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  • 50
    facet.materialart.
    Unknown
    PANGAEA
    In:  Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven
    Publication Date: 2024-06-21
    Description: Raw data acquired by position sensors on board RV Polarstern during expedition PS140 was processed to receive a validated master track which can be used as reference of further expedition data. During PS140 two Trimble Marine R750 GPS receivers and the iXBlue HYDRINS hydrographic survey inertial navigation system were used as navigation sensors. Data were downloaded from DAVIS SHIP data base (https://dship.awi.de) with a resolution of 1 sec. Processed data are provided as a master track with 1 sec resolution derived from the position sensors' data selected by priority and a generalized track with a reduced set of the most significant positions of the master track.
    Keywords: 1 sec resolution; CT; EASI-2; Polarstern; PS140; PS140-track; Underway cruise track measurements
    Type: Dataset
    Format: application/zip, 237.7 MBytes
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  • 51
    Publication Date: 2024-06-21
    Description: Sediment cores and pore water cores were taken in the Skagerrak and North Sea with a multicorer on cruise AL557 (June 2021). The sediment cores were sliced onboard into 1 cm slices and frozen directly (-20°C). Pore water samples were taken with rhizon samplers (0.15 µm pore size, CSS; Rhizosphere, Netherlands) from intact sediment cores and frozen directly (-20°C). In the laboratory, the sediments were freeze-dried, sieved (〈2mm) and milled. For organic carbon (after acidification) and total carbon and nitrogen contents, the samples were analyzed using an Euro EA 3000 (Euro Vector SPA) Elemental Analyzer, delta 15N was measured with a FlashEA 1112 elemental analyzer coupled to a MAT 252 (Thermo Fisher Scientific) isotope ratio mass spectrometer (https://doi.org/10.1016/j.orggeochem.2009.05.008; lab 3). For trace metal analysis, the sediments were digested with HBF4+HNO3+HCl (https://doi.org/10.1039/D0AY01049A) and the pore water samples were acidified with HNO3 prior to 10-fold dilution with HNO3. Trace elements were measured by ICP-MS/MS (Agilent 8800, Agilent Technologies, Japan).
    Keywords: AL557; AL557_11-3; AL557_15-4; AL557_25-2; AL557_3-3; AL557_43-3; AL557_65-8; AL557_65-9; Alkor (1990); Aluminium; Aluminium, uncertainty; Antimony; Antimony, uncertainty; Arsenic; Arsenic, uncertainty; Barium; Barium, uncertainty; Cadmium; Cadmium, uncertainty; Caesium; Caesium, uncertainty; Calcium; Calcium, uncertainty; Carbon, organic, total; Carbon, organic, total, uncertainty; Carbon, total; Carbon, total, uncertainty; Carbon Storage in German Coastal Seas - Stability, Vulnerability and Perspectives for Manageability; Carbostore; Cerium; Cerium, uncertainty; Chromium; Chromium, uncertainty; Cobalt; Cobalt, uncertainty; Copper; Copper, uncertainty; DAM sustainMare - MGF North Sea: Exclusion of mobile bottom-contact fishing in marine protected areas of the German Exclusive Economic Zone of the North Sea; DATE/TIME; DEPTH, sediment/rock; Device type; Dysprosium; Dysprosium, uncertainty; Element analyser (EA); Element analyzer, Thermo Scientific, Flash EA1112; coupled with a Finnigan MAT 252 IRMS; Erbium; Erbium, uncertainty; Europium; Europium, uncertainty; Event label; Gadolinium; Gadolinium, uncertainty; GC; Gravity corer; Holmium; Holmium, uncertainty; ICP-MS; Indium; Indium, uncertainty; Iron; Iron, uncertainty; Lanthanum; Lanthanum, uncertainty; LATITUDE; Lead; Lead, uncertainty; Lithium; Lithium, uncertainty; LONGITUDE; Lutetium; Lutetium, uncertainty; Magnesium; Magnesium, uncertainty; Manganese; Manganese, uncertainty; MGF_North_Sea; Molybdenum; Molybdenum, uncertainty; MUC; MultiCorer; Neodymium; Neodymium, uncertainty; Nickel; Nickel, uncertainty; Niobium; Niobium, uncertainty; Nitrogen, total; Nitrogen, total, uncertainty; North Sea; Phosphorus; Phosphorus, uncertainty; Potassium; Potassium, uncertainty; Praseodymium; Praseodymium, uncertainty; Research Mission of the German Marine Research Alliance (DAM): Protection and sustainable use of marine areas; Rubidium; Rubidium, uncertainty; Samarium; Samarium, uncertainty; Sample code/label; Sample elevation; Skagerrak; Strontium; Strontium, uncertainty; sustainMare; Tantalum; Tantalum, uncertainty; Terbium; Terbium, uncertainty; Thallium; Thallium, uncertainty; Thorium; Thorium, uncertainty; Thulium; Thulium, uncertainty; Titanium; Titanium, uncertainty; Uranium; Uranium, uncertainty; Vanadium; Vanadium, uncertainty; Ytterbium; Ytterbium, uncertainty; Yttrium; Yttrium, uncertainty; Zinc; Zinc, uncertainty; δ15N; δ15N, uncertainty
    Type: Dataset
    Format: text/tab-separated-values, 5767 data points
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  • 52
    facet.materialart.
    Unknown
    PANGAEA
    In:  Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven
    Publication Date: 2024-06-21
    Description: Raw data acquired by position sensors on board RV Polarstern during expedition PS140 was processed to receive a validated master track which can be used as reference of further expedition data. During PS140 two Trimble Marine R750 GPS receivers and the iXBlue HYDRINS hydrographic survey inertial navigation system were used as navigation sensors. Data were downloaded from DAVIS SHIP data base (https://dship.awi.de) with a resolution of 1 sec. Processed data are provided as a master track with 1 sec resolution derived from the position sensors' data selected by priority and a generalized track with a reduced set of the most significant positions of the master track.
    Keywords: Calculated; Course; CT; DATE/TIME; EASI-2; LATITUDE; LONGITUDE; Polarstern; PS140; PS140-track; Speed; Underway cruise track measurements
    Type: Dataset
    Format: text/tab-separated-values, 17932 data points
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  • 53
    Publication Date: 2024-06-21
    Description: Information on foraging behaviour is critical for modelling estimations of energy acquisition and requirements of top predators and consequently to predict how animals will be affected and respond to changes in marine ecosystems. We compiled estimates of prey capture attempt rates per hour of 11 female sperm whales, tagged using high-resolution multi-sensor tags (DTAGs, Johnson & Tyack, 2003; Oliveira et al. (2022) for detailed information about the tags and tagging procedures) in the Azores region between 2018 and 2020. These estimates were used in a bioenergetic model to estimate minimum foraging success rate (FSR), i.e., the lowest possible prey capture rate for individuals obtain the minimum energy intake needed to meet daily metabolic requirements (Silva et al., 2024). The model was based on whales' theoretical energetic requirements using foraging and prey characteristics from animal-borne tags and stomach contents, respectively. The present dataset consists of individual identification, location, date of tagging, latitude, longitude, maximum depth water and prey capture attempt rate (rPCA as the number of buzzes) per hour.
    Keywords: Azores; bioenergetics; Biologging; Calculated; DATE/TIME; Digital acoustic recording tag according to Johnson and Tyack (2003); Dive, maximum depth; Dive, number of buzzes, per hour; Dive number; DTAG; Eco-physiology; energy; Event label; Index; Latitude of event; Longitude of event; marine mammal; modelling; Pmacrocephalus_2018_2a; Pmacrocephalus_2018_3a; Pmacrocephalus_2019_4a; Pmacrocephalus_2019_5a; Pmacrocephalus_2019_6a; Pmacrocephalus_2019_7a; Pmacrocephalus_2019_8a; Pmacrocephalus_2020_10a; Pmacrocephalus_2020_12a; Pmacrocephalus_2020_13a; Pmacrocephalus_2020_9a; Species, unique identification; Species, unique identification (Semantic URI); Species, unique identification (URI); Specimen identification; SUMMER; Sustainable Management of Mesopelagic Resources; VID; Visual identification
    Type: Dataset
    Format: text/tab-separated-values, 504 data points
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  • 54
    Publication Date: 2024-06-21
    Description: Sediment cores and pore water cores were taken in the Skagerrak with a multicorer on cruise HE586 (October 2021). The sediment cores were sliced onboard into 1 cm slices and frozen directly (-20°C). Pore water samples were taken with rhizon samplers (0.15 µm pore size, CSS; Rhizosphere, Netherlands) from intact sediment cores and frozen directly (-20°C). In the laboratory, the sediments were freeze-dried, sieved (〈2mm) and milled. For organic carbon (after acidification) and total carbon and nitrogen contents, the samples were analyzed using an Euro EA 3000 (Euro Vector SPA) Elemental Analyzer, delta 15N was measured with a FlashEA 1112 elemental analyzer coupled to a MAT 252 (Thermo Fisher Scientific) isotope ratio mass spectrometer (https://doi.org/10.1016/j.orggeochem.2009.05.008; lab 3). The pore water nutrient concentrations (ammonia, silicate, phosphate, nitrite, nitrite+nitrate) were measured using a TECAN infinite 200 plate reader. Colorimetric methods according to Ringuet et al. (2011; https://doi.org/10.1039/C0EM00290A) for phosphate and silicate, Yu et al. (1994; http://www.sfjo-lamer.org/la_mer/32-2/32-2.pdf#page=19) for ammonia and Garcia-Robledo et al. (2014; https://doi.org/10.1016/j.marchem.2014.03.002) were applied. For trace metal analysis, the sediments were digested with HBF4+HNO3+HCl (https://doi.org/10.1039/D0AY01049A) and the pore water samples were acidified with HNO3 prior to 10-fold dilution with HNO3. Trace elements were measured by ICP-MS/MS (Agilent 8800, Agilent Technologies, Japan).
    Keywords: Aluminium; Aluminium, uncertainty; Ammonium; Ammonium, uncertainty; Antimony; Antimony, uncertainty; Arsenic; Arsenic, uncertainty; Barium; Barium, uncertainty; Caesium; Caesium, uncertainty; Calcium; Calcium, uncertainty; Carbon, organic, total; Carbon, organic, total, uncertainty; Carbon, total; Carbon, total, uncertainty; Carbon Storage in German Coastal Seas - Stability, Vulnerability and Perspectives for Manageability; Carbostore; Cerium; Cerium, uncertainty; Chromium; Chromium, uncertainty; Cobalt; Cobalt, uncertainty; Copper; Copper, uncertainty; DATE/TIME; DEPTH, sediment/rock; Device type; Dysprosium; Dysprosium, uncertainty; Element analyser (EA); Element analyzer, Thermo Scientific, Flash EA1112; coupled with a Finnigan MAT 252 IRMS; Erbium; Erbium, uncertainty; Europium; Europium, uncertainty; Event label; Gadolinium; Gadolinium, uncertainty; HE586; HE586_13-4; HE586_24-4; HE586_8-5; Heincke; Holmium; Holmium, uncertainty; ICBM-HS-EMD-LER_22; ICP-MS; Indium; Indium, uncertainty; Iron; Iron, uncertainty; Lanthanum; Lanthanum, uncertainty; LATITUDE; Lead; Lead, uncertainty; Lithium; Lithium, uncertainty; LONGITUDE; Lutetium; Lutetium, uncertainty; Magnesium; Magnesium, uncertainty; Manganese; Manganese, uncertainty; Microplate reader, Tecan Trading AG, Infinite 200; Molybdenum; Molybdenum, uncertainty; MUC; MultiCorer; Neodymium; Neodymium, uncertainty; Nickel; Nickel, uncertainty; Niobium; Niobium, uncertainty; Nitrate and Nitrite; Nitrate and Nitrite, uncertainty; Nitrite; Nitrite, uncertainty; Nitrogen, total; Nitrogen, total, uncertainty; Phosphate; Phosphate, uncertainty; Phosphorus; Phosphorus, uncertainty; Potassium; Potassium, uncertainty; Praseodymium; Praseodymium, uncertainty; Rubidium; Rubidium, uncertainty; Samarium; Samarium, uncertainty; Sample code/label; Sample elevation; Silicate; Silicate, dissolved, uncertainty; Skagerrak; Strontium; Strontium, uncertainty; Tantalum; Tantalum, uncertainty; Terbium; Terbium, uncertainty; Thallium; Thallium, uncertainty; Thorium; Thorium, uncertainty; Thulium; Thulium, uncertainty; Titanium; Titanium, uncertainty; Uranium; Uranium, uncertainty; Vanadium; Vanadium, uncertainty; Ytterbium; Ytterbium, uncertainty; Yttrium; Yttrium, uncertainty; Zinc; Zinc, uncertainty; δ15N; δ15N, uncertainty
    Type: Dataset
    Format: text/tab-separated-values, 11827 data points
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  • 55
    Publication Date: 2024-06-21
    Keywords: Calculated, 2 sigma; Climate change; Correlation coefficient, isotope ratio error; DEPTH, sediment/rock; Initial Osmium isotope composition; initial Osmium isotope composition, standard error; large igneous province; mid-Cretaceous; Northwestern Pacific; Nutrient supply; OAE2_OMZ; Osmium; Osmium, standard error; Osmium-187/Osmium-188, standard error; Osmium-187/Osmium-188 ratio; Osmium-192; Osmium-192, standard error; Rhenium; Rhenium, standard error; Rhenium-187/Osmium-188, standard error; Rhenium-187/Osmium-188 ratio; ROCK; Rock sample; Sample ID
    Type: Dataset
    Format: text/tab-separated-values, 686 data points
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  • 56
    Publication Date: 2024-06-21
    Keywords: AGE; Age, dated material; Age, standard deviation; Analytical method; Arubotaim; Arugot; Calculated, 2 sigma; CDRILL; Comment; Core drilling; David; Dead Sea; Dead Sea Basin, Israel; Depth, relative; DSDDP_5017-1-A; Eastern Mediterranean; Ein-Qedem; En-Gedi; Event label; Halite fluid inclusions; Lake level; Lake level, standard deviation; Late Quaternary; Lithology/composition/facies; Massada; Nahal-Darga; Paleolimnology; Perazim; Reference/source; Stratigraphic Unit; Subsidence; Subsidence corrected; West-escarpment-Cave_S-181; West-escarpment-Cave_S-215; West-escarpment-Cave_S-34; West-escarpment-Cave_S-42; West-escarpment-Cave_S-54; West-escarpment-Cave_S-66; West-escarpment-Cave_SQ-18; West-escarpment-Cave_SQ-4; West-escarpment-Cave_SQ-8; West-escarpment-Cave_SQ-9; West-escarpment-terraces; Yizrah; Zeelim
    Type: Dataset
    Format: text/tab-separated-values, 2015 data points
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  • 57
    Publication Date: 2024-06-21
    Description: Opinion formation within society follows complex dynamics. Towards its understanding, axiomatic theory can complement data analysis. To this end we propose an axiomatic model of opinion formation that aims to capture the interaction of individual conviction with social influence in a minimalist fashion. Despite only representing that (1) agents have an initial conviction with respect to a topic and are (2) influenced by their neighbours, the model shows emergence of opinion clusters from an initially unstructured state. Here, we show that increasing individual self-reliance makes agents more likely to align their socially influenced opinion with their inner conviction which concomitantly leads to increased polarisation. The opinion drift observed with increasing self-reliance may be a plausible analogue of polarisation trends in the real world. Modelling the basic traits of striving for individual versus group identity, we find a trade-off between individual fulfilment and societal cohesion. This finding from fundamental assumptions can serve as a building block to explain opinion polarisation.
    Language: English
    Type: info:eu-repo/semantics/article
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  • 58
    Publication Date: 2024-06-21
    Description: Wasserstoff wird eine entscheidende Rolle bei der Dekarbonisierung von schwer elektrifizierbaren Sektoren spielen, doch die Produktion von erneuerbarem Wasserstoff steckt noch in der Anfangsphase. Aus diesem Grund wird die Nutzung von kohlenstoffarmem Wasserstoff aus nicht-erneuerbaren Quellen als Übergangslösung auf dem Weg zu einer erneuerbaren Wasserstoffwirtschaft diskutiert. Kohlenstoffarmer Wasserstoff umfasst unterschiedliche Produktionsmethoden, wie die Herstellung aus fossilen Brennstoffen mit nachfolgender Kohlenstoffabscheidung und -speicherung (CCS) oder -nutzung (CCU), sowie die Elektrolyse mit Strom aus Kernenergie. Um eine positive Klimaschutzwirkung durch den Einsatz von kohlenstoffarmem Wasserstoff sicherzustellen, müssen signifikante Reduzierungen von Treibhausgasemissionen (THG) erzielt werden. Dies sollte durch einen kohärenten regulatorischen Rahmen für die Produktion und den Import von kohlenstoffarmem Wasserstoff auf EU-Ebene gewährleistet werden. Diese Analyse gibt demnach Einblicke in den aktuellen Stand der EU-Gesetzgebung zur Produktion und zum Import von kohlenstoffarmem Wasserstoff und untersucht, ob die verbundenen Risiken und Herausforderungen für einen wirksamen Klimaschutz durch den Rechtsrahmen abgedeckt sind. Da jede Produktionsmethode durch unterschiedliche Herausforderungen charakterisiert ist, untersucht die Analyse die jeweiligen Regelungen gasbasierter Wasserstoffproduktion mit CCS, gasbasierter Wasserstoffproduktion mit CCU, sowie die Wasserstoffproduktion mit Kernenergie im Einzelnen. Auf dieser Grundlage werden Empfehlungen für die Entwicklung des regulatorischen Rahmens für innereuropäisch produzierten und importierten kohlenstoffarmem Wasserstoff formuliert.
    Language: German
    Type: info:eu-repo/semantics/report
    Format: application/pdf
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  • 59
    facet.materialart.
    Unknown
    Potsdam Institute for Climate Impact Research
    In:  Ariadne-Analyse
    Publication Date: 2024-06-21
    Description: Renewable hydrogen is necessary for the decarbonization of sectors that are difficult to electrify, such as industry and aviation, and as a storage medium for surplus electricity from renewable sources.
    Language: English
    Type: info:eu-repo/semantics/report
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  • 60
    facet.materialart.
    Unknown
    Potsdam Institute for Climate Impact Research
    In:  Ariadne-Analyse
    Publication Date: 2024-06-21
    Description: Wasserstoff ist durch seine vielfältigen Nutzungsmöglichkeiten ein Schlüsselelement der Sektorenkopplung auf dem Weg zur Klimaneutralität. Damit Wasserstoff aber für unterschiedliche, momentan noch nicht abschließend definierte Anwendungsbereiche genutzt werden kann, sind entsprechende technologische Infrastrukturen notwendig. Diese umfassen die Produktion, die Speicherung und den Transport von Wasserstoff. Während bei der Bereitstellung von Wasserstoff konkrete Ziele formuliert wurden und auch hinsichtlich der Anwendungsbereiche deutliche, wenn auch konkurrierende Vorstellungen bestehen, sind bei der Wasserstoffinfrastruktur viele grundsätzliche Fragen offen. Vor diesem Hintergrund diskutiert diese Analyse, unbeschadet der Tatsache, dass bislang weder eine Systementwicklungsplanung noch ein abgeschlossenes Wasserstoffwirtschaftsrecht in Deutschland bestehen, wie viel „System“ und „Planung“ bereits jetzt durch Stakeholder und den einschlägigen Rechtsrahmen mit Blick auf Wasserstoff mitgedacht werden. Dabei orientiert sich die Analyse an folgenden Fragen: Erfolgt die Regulierung in Sachen Wasserstoff bereits jetzt aus der Sicht eines geschlossenen Energiesystems? Sehen die Stakeholder Wasserstoff bereits systemisch und interpretieren sie den bestehenden Rechtsrahmen zur Planung der Infrastrukturen entsprechend? Folgen die Vorstellungen der Wasserstoffinfrastruktur schon jetzt systemischen Ansätzen oder stellen sie vielmehr eine weitere sektorale Infrastruktur und Planung dar? Die vorliegende Analyse zeigt, dass Stakeholder nicht grundsätzlich einen systemischen Blick auf Wasserstoff haben und gerade bei wirtschaftlichen Akteuren teilweise eine sektorale Betrachtung überwiegt. Hier sollte beobachtet werden, in welcher Weise bei der Realisierung des seit dem Sommer 2023 vorliegenden Vorschlag des Wasserstoffkernnetzes (FNB Gas 2023), Nutzerbedarfe in die Planungsprozesse einbezogen werden. Noch weniger berücksichtigen einschlägige Rechtsvorschriften die systemische Bedeutung von Wasserstoff. Beachtenswert ist dabei unter anderem, dass die bestehenden nationalen Vorschriften zur Einführung einer Wasserstoffnetzplanung wenig bis gar keine Bezugnahme zur systemischen Funktionsweise von Wasserstoff aufweisen. Im europäischen Recht entfaltet die Erneuerbare-Energien-Richtlinie durch das Kriterium der Zusätzlichkeit bei neu in Betrieb genommenen Anlagen hingegen durchaus eine vorgelagerte systemische Entscheidungswirkung. In der deutschen Planungspraxis könnte der systemische Aspekt dadurch gestärkt werden, dass Strom- und Wasserstoffnetzplanungen über Einzelaspekte wie Power-to-Gas-Anlagen in Zukunft von vornherein integriert angelegt werden.
    Language: German
    Type: info:eu-repo/semantics/report
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  • 61
    Publication Date: 2024-06-21
    Description: The Skagerrak basin represents the main sink area for fine-grained sediment in the North Sea region and constitutes a natural deposition centre for sediments that are supplied from the Atlantic, the Baltic Sea and the surrounding continental margins and coasts. However, the exact sources and their proportional contributions to the North Sea sediments and to the Skagerrak deposits are not well understood.To trace the predominant sources of the sediment and to gain a better understanding of the sedimentary processes in the North Sea and the Skagerrak basin, radiogenic Sr, Nd, and Hf isotope signatures and clay mineral compositions of the detrital clay fraction of surface sediment samples from the North Sea, the Scandinavian margins and the Baltic Sea were measured.The results indicate that the major source for Skagerrak clay-size sediments is the northern North Sea but Scandinavia as well as the southern North Sea including the southern England coast also contribute material. Seabed and coastal erosion in the northern North Sea are enhanced by the inflowing Atlantic Currents, which provide the Skagerrak with high amounts of clay size sediments. In contrast, the southern North Sea, the Baltic Sea and mid-European rivers such as Weser, Elbe and Ems are only minor contributors. As Skagerrak deposits are dominated by clay sized material (up to 60%), the reconstructed sediment processes related to this study deviate from findings in previous sediment budget studies, which were based on both clay and silt fraction and indicated predominant influences from the southern North Sea. These results highlight that coastal and seabed erosion in the North Sea is a previously underestimated source of fine-grained sediments for depocenters in the entire North Sea.With regard to climate change, the global sea-level rise will likely enhance erosional processes and can therefore significantly influence the sediment budget of the entire North Sea.
    Type: Article , PeerReviewed
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  • 62
    Publication Date: 2024-06-21
    Type: Article , PeerReviewed
    Format: text
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  • 63
    Publication Date: 2024-06-21
    Description: The Mariana Trough is the youngest back-arc basin in a series of basins and arcs that developed behind the Mariana subduction zone in the western Pacific. Active seafloor spreading is ongoing at a spreading axis close the Mariana Arc resulting in a pronounced asymmetric configuration (double rate to the west 2:1) at 17° N. The formation of back-arc basins is controlled by the subducting slab, which regulates the temporal development of mantle flow, entrainment of fluids and hydrous melts together with the magma generation. To better understand the formation process of back-arc basins and the asymmetry of the central Mariana Trough, we combined 2-D P-wave traveltime tomography results together with high-resolution bathymetric data. Here, we show that the crust in the central Mariana Trough is 6.5-9.5 km thick, which is unusual for oceanic crust. The lower crust exhibits average seismic velocities of 6.5-7.2 km/s. High-velocity anomalies (7.4-7.9 km/s) in the lower crust at the margins of the Mariana Trough indicate that magmatic accretion process was affected by hydrous melting during rifting. While the Mariana Trough developed from a rather symmetric rifting (0.89:1) to a strongly asymmetric seafloor spreading stage (5.33:1), the contribution of hydrous melts declined and the opening direction changed. The asymmetric plate motions and the temporal change of the slab component influenced strongly the formation of the back-arc basin.
    Type: Article , NonPeerReviewed
    Format: text
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  • 64
    Publication Date: 2024-06-21
    Description: Although ~20% of global carbonate occurs on extra-tropical shelves, our understanding of these depositional environments still lags far behind that of tropical carbonate platforms. The Maltese shelf in the central Mediterranean offers an opportunity to study in situ facies distribution in a light-dominated extra-tropical carbonate platform and the factors controlling them. The Maltese shelf visually exhibits three main facies: seagrass meadows; sand flats/bedforms and maerl. While visually distinctive, the allochem composition of the sediment does not offer a clear differentiation of all three but rather a gradient. This gradient is marked by increasing grain size with depth, a transition from green to red calcareous algae and an increase in the fraction of low Mg calcite. While some of these features could be explained by changes in light availability, other factors are also in play. Internal waves, currents and baffling by seafloor vegetation appear to play important roles in governing the sedimentary texture and composition across the Maltese shelf. The role of vegetated substrate is of greater importance in Mediterranean C-type carbonate factories and could be an important marker to identify them in the geological record.
    Type: Article , NonPeerReviewed
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  • 65
    Publication Date: 2024-06-21
    Description: Sediment sampling is a prevalent approach for ex- ploring and understanding the ocean and its change over time. Unfortunately, the sampling process can be very costly due to the logistics that involve the transportation and deployment of the Remotely Operative Vehicle (ROV), specifically designed for this task. In a collaboration of marine scientists and engineers, this work focuses on developing a lightweight, modular and cost efficient actuation system for deep-sea suction-sampling. We propose a binary actuation system to manipulate the sampling tube directly instead of the tube being guided by a traditional manipulator. The core of the actuation system are bistable actuators that combine origami-inspired soft actuators with a bistable mechanism to form a lightweight but still robust system. This concept aims to lower the cost of deep-sea sediment sampling by offering the option to replace the currently used hydraulic titanium manipulator, that is traditionally used for deep-sea research. We present the design, manufacturing and proof of concept for the combination of a origami-inspired soft actuator with a bistable mechanism.
    Type: Book chapter , NonPeerReviewed
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  • 66
    Publication Date: 2024-06-21
    Type: Article , NonPeerReviewed , info:eu-repo/semantics/article
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  • 67
    Publication Date: 2024-06-21
    Description: Abstract
    Description: This data repository contains electrical and seismic tremor measurements, thermal infrared imagery, atmospheric conditions and information on plume heights that were recorded and collected during the 2021 Tajogaite eruption on La Palma, Canary Islands, Spain. The 2021 Tajogaite eruption lasted from 19 September until 13 December 2021. The "data description" file provides more detailed information on each dataset and the way the data is formatted. The electrical data was recorded using a Biral Thunderstorm Detector BTD-200. This sensor was installed at two consecutive locations: BTD1 (28.635°N, 17.876389°W) recorded from 11-26 October 2021 and BTD2 (28.602365°N, 17.880475°W) recorded from 27 October 2021 until the end of the eruption. The volcanic tremor measurements were recorded at seismic station PLPI (28.5722°N, 17.8654°W), which was operated by the Instituto Volcanológico de Canarias. Here we provide the seismic tremor amplitudes within the Very Long Period (0.4-0.6 Hz) and the Long Period (1-5 Hz) frequency bands between 10 September and 20 December 2021. Thermal infrared videography of the explosive volcanic activity was done using an InfraTec HD thermal infrared (TIR) video camera. This camera was installed in El Paso (28.649361°N, 17.882279°W) and recorded almost continuously between 3-8 November 2021. Here we provide individual thermal infrared frames. Atmospheric conditions were obtained from weather balloon measurements at Güímar (station nr. 60018) on Tenerife, which were provided by the University of Wyoming, Department of Atmospheric Science (http://weather.uwyo.edu/). In addition, atmospheric data was collected from ground-based weather stations at El Paso and Roque de los Muchachos, which were operated by the State Meteorological Agency (AEMET) of Spain on La Palma. Information on the volcanic plume heights was obtained from both the Toulouse Volcanic Ash Advisory Center (https://vaac.meteo.fr/volcanoes/la-palma/) as well as the Plan de Emergencias Volcánicas de Canarias.
    Keywords: Volcanic lightning ; Volcanic ash ; Biral Thunderstorm Detector ; Electrostatic measurements ; 2021 Tajogaite eruption ; Cumbre Vieja volcanic ridge ; La Palma ; Canary Islands ; Movement of charge ; Volcanic plume height ; Ice nucleation ; Lava fountaining ; Strombolian activity ; Ash emission ; Gas jetting ; Explosive volcanic activity ; Seismic tremor ; Thermal infrared rise diagram ; Isotherms ; Principal Component Analysis (PCA) ; Very Long Period (VLP) ; Long Period (LP) ; Balloons/Rockets 〉 RADIOSONDES ; EARTH SCIENCE 〉 ATMOSPHERE 〉 ATMOSPHERIC ELECTRICITY 〉 ELECTRIC FIELD ; EARTH SCIENCE 〉 ATMOSPHERE 〉 ATMOSPHERIC ELECTRICITY 〉 LIGHTNING ; EARTH SCIENCE 〉 SOLID EARTH 〉 TECTONICS 〉 EARTHQUAKES 〉 EARTHQUAKE MAGNITUDE/INTENSITY ; EARTH SCIENCE 〉 SOLID EARTH 〉 TECTONICS 〉 EARTHQUAKES 〉 EARTHQUAKE OCCURRENCES ; EARTH SCIENCE 〉 SOLID EARTH 〉 TECTONICS 〉 VOLCANIC ACTIVITY 〉 ERUPTION DYNAMICS 〉 ASH/DUST DISPERSION ; EARTH SCIENCE 〉 SOLID EARTH 〉 TECTONICS 〉 VOLCANIC ACTIVITY 〉 ERUPTION DYNAMICS 〉 VOLCANIC EXPLOSIVITY ; EARTH SCIENCE 〉 SOLID EARTH 〉 TECTONICS 〉 VOLCANIC ACTIVITY 〉 VOLCANO MAGNITUDE/INTENSITY ; EARTH SCIENCE 〉 SOLID EARTH 〉 TECTONICS 〉 VOLCANIC ACTIVITY 〉 VOLCANO PREDICTIONS ; EARTH SCIENCE 〉 SPECTRAL/ENGINEERING 〉 INFRARED WAVELENGTHS 〉 THERMAL INFRARED ; EARTH SCIENCE SERVICES 〉 ENVIRONMENTAL ADVISORIES 〉 GEOLOGICAL ADVISORIES 〉 VOLCANIC ACTIVITY ; EARTH SCIENCE SERVICES 〉 ENVIRONMENTAL ADVISORIES 〉 WEATHER/CLIMATE ADVISORIES 〉 DUST/ASH ADVISORIES ; EARTH SCIENCE SERVICES 〉 ENVIRONMENTAL ADVISORIES 〉 WEATHER/CLIMATE ADVISORIES 〉 PRESENT WEATHER ; geological process 〉 volcanism 〉 volcanic eruption ; hazard 〉 natural hazard ; In Situ Land-based Platforms 〉 GEOPHYSICAL STATIONS/NETWORKS 〉 SEISMOLOGICAL STATIONS ; In Situ Land-based Platforms 〉 GEOPHYSICAL STATIONS/NETWORKS 〉 VOLCANO OBSERVATORY ; In Situ Land-based Platforms 〉 WEATHER STATIONS/NETWORKS 〉 METEOROLOGICAL STATIONS ; In Situ Land-based Platforms 〉 WEATHER STATIONS/NETWORKS 〉 WWLLN ; In Situ/Laboratory Instruments 〉 Electrical Meters ; In Situ/Laboratory Instruments 〉 Magnetic/Motion Sensors 〉 Seismometers 〉 SEISMOMETERS ; monitoring 〉 seismic monitoring ; physical process 〉 transport (physics) 〉 mass transport (physics) ; physical property 〉 electricity ; science 〉 natural science 〉 earth science 〉 geology 〉 volcanology ; science 〉 natural science 〉 earth science 〉 geophysics ; science 〉 physical science 〉 physics 〉 atmospheric physics
    Type: Dataset , Dataset
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  • 68
    Publication Date: 2024-06-20
    Description: Over the last 25 years, Canadian scientists have studied the permafrost environmental archives in the Klondike Goldfields south of Dawson City (e.g. Fraser and Burn, 1997; Kotler and Burn, 2010; Froese et al., 2009; Porter et al., 2016; Monteath et al., 2023). In 2023, a small Canadian-German team visiting this area to sample mining exposures in the Klondike area (Figure 1A). The goal was to conduct studies on ground ice (ice wedges and pore ice) and frozen sediments to reconstruct past landscape and climate conditions. Detailed profiles were sampled at three sites at Little Blanche Creek, Whitman Gulch and Bear Creek. Ice wedges were described in terms of their size, the color of ice, internal structure, existence and form of gas bubbles and were sampled by chain saw as blocks. The frozen sediment was cleaned, and ice, sediment and cryostructures were described, followed by sediment sampling with an axe and hammer. Separately, sediment cores were collected with a battery driven drill for biomarker studies. In our presentation, we present the first results of new field and laboratory studies. This concerns age determinations, sediment data, stable isotopes and hydrochemistry of the ground ice. The mean ice content measured was 38 ± 10 wt%. We expect new knowledge regarding the reconstruction of Late Quaternary environment of Central Yukon. References Fraser, T.A. and Burn, C.R. 1997: On the nature and origin of "muck" deposits in the Klondike area, Yukon Territory, Canadian Journal of Earth Sciences 34(10), 1333-1344, https://doi.org/10.1139/e17-106. Froese, D., Zazula, G., Westgate, J., Preece, S., Sanborn, P. A., Reyes, A., and Pearce, N. 2009: The Klondike goldfields and Pleistocene environments of Beringia, GSA Today, 19, 4-10, https://doi.org/10.1130/GSATG54A.1. Kotler, E. and Burn, C. R. 2000: Cryostratigraphy of the Klondike "muck" deposits, west-central Yukon Territory, Can. J. Earth Sci., 37, 849-861, https://doi.org/10.1139/e00-013. Monteath, A. J., Kuzmina, S., Mahony, M., Calmels, F., Porter, T., Mathewes, R., Sanborn, P., Zazula, G., Shapiro, B., Murchie, T. J., Poinar, H. N., Sadoway, T., Hall, E., Hewitson, S., and Froese, D. 2023: Relict permafrost preserves megafauna, insects, pollen, soils and pore-ice isotopes of the mammoth steppe and its collapse in central Yukon, Quaternary Science Reviews, 299, 107878, https://doi.org/10.1016/j.quascirev.2022.107878. Porter, T. J., Froese, D. G., Feakins, S. J., Bindeman, I. N., Mahony, M. E., Pautler, B. G., Reichart, G. J., Sanborn, P. T., Simpson, M. J., and Weijers, J. W. H. 2016: Multiple water isotope proxy reconstruction of extremely low last glacial temperatures in Eastern Beringia (Western Arctic), Quaternary Science Reviews, 137, 113-125, https://doi.org/10.1016/j.quascirev.2016.02.006.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Conference , NonPeerReviewed
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  • 69
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    University of South Florida Libraries
    In:  EPIC3International Journal of Speleology, University of South Florida Libraries, 53(1), pp. 13-23, ISSN: 0392-6672
    Publication Date: 2024-06-20
    Description: The study of modern cave deposits forming under near isotopic equilibrium conditions can potentially help disentangle the processes influencing the oxygen isotope system and suitability of stalagmites as archives of past hydrological or thermal changes. We used cave monitoring to evaluate the impact of kinetic isotope fractionation and assess the conditions under which modern cave carbonates form in the Caumont cave and quarry system, located in Normandy, northwest France. Over 20 months, we collected climatological data, dripwater, and modern carbonate samples at 2–4-week intervals at three different stations inside the Caumont cave and quarry system. We find highly stable (10.4 ± 0.3 – 11.3 ± 0.1°C) temperature in the deeper sections of the Caumont cave and quarry system. The temporal dynamics of δ18 Odrip indicates that the drip water composition in Caumont reflects the original (though subdued) signal of precipitation, rather than the impact the seasonal to interannual cave air temperature has on isotopic fractionation. The monitoring reveals that δ13 C of modern carbonate is influenced by prior carbonate precipitation that occurs during the summer season when evapotranspiration can minimize effective infiltration. Comparison of δ18 O from dripwater and modern calcite, precipitated on glass plates and collected every two to four weeks, reveals that modern calcite forms near oxygen isotope equilibrium. A Hendy test on modern carbonate deposited on a stalagmite-shaped glass flask over 20 months confirms this finding because neither does δ13 C increase with distance from the apex, nor are δ13 C and δ18 O positively correlated. We conclude that the δ13 C signal in speleothems reflect summer (and longer-term) prior carbonate precipitation in response to effective infiltration dynamics, and that the δ18 O signal likely reflects annual to multi-annual changes in the composition of precipitation above the cave.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , peerRev
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  • 70
    Publication Date: 2024-06-20
    Description: Tropospheric reactive bromine (Bry) influences the oxidation capacity of the atmosphere by acting as a sink for ozone and nitrogen oxides. Aerosol acidity plays a crucial role in Bry abundances through acid-catalyzed debromination from sea-salt-aerosol, the largest global source. Bromine concentrations in a Russian Arctic ice-core, Akademii Nauk, show a 3.5-fold increase from pre-industrial (PI) to the 1970s (peak acidity, PA), and decreased by half to 1999 (present day, PD). Ice-core acidity mirrors this trend, showing robust correlation with bromine, especially after 1940 (r = 0.9). Model simulations considering anthropogenic emission changes alone show that atmospheric acidity is the main driver of Bry changes, consistent with the observed relationship between acidity and bromine. The influence of atmospheric acidity on Bry should be considered in interpretation of ice-core bromine trends.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
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  • 71
    Publication Date: 2024-06-20
    Description: Oxygen isotopes in biogenic silica (δ18OBSi) from lake sediments allow for quantitative reconstruction of past hydroclimate and proxy-model comparison in terrestrial environments. The signals of individual records have been attributed to different factors, such as air temperature (Tair), atmospheric circulation patterns, hydrological changes, and lake evaporation. While every lake has its own local set of drivers of δ18O variability, here we explore the extent to which regional or even global signals emerge from a series of paleoenvironmental records. This study provides a comprehensive compilation and combined statistical evaluation of the existing lake sediment δ18OBSi records, largely missing in other summary publications (i.e. PAGES network). For this purpose, we have identified and compiled 71 down-core records published to date and complemented these datasets with additional lake basin parameters (e.g. lake water residence time and catchment size) to best characterize the signal properties. Records feature widely different temporal coverage and resolution, ranging from decadal-scale records covering the past 150 years to records with multi-millennial-scale resolution spanning glacial-interglacial cycles. The best coverage in number of records (NCombining double low line37) and data points (NCombining double low line2112) is available for Northern Hemispheric (NH) extratropical regions throughout the Holocene (roughly corresponding to Marine Isotope Stage 1; MIS 1). To address the different variabilities and temporal offsets, records were brought to a common temporal resolution by binning and subsequently filtered for hydrologically open lakes with lake water residence times 〈100 years. For mid- to high-latitude (〉45°N) lakes, we find common δ18OBSi patterns among the lake records during both the Holocene and Common Era (CE). These include maxima and minima corresponding to known climate episodes, such as the Holocene Thermal Maximum (HTM), Neoglacial Cooling, Medieval Climate Anomaly (MCA) and the Little Ice Age (LIA). These patterns are in line with long-term air temperature changes supported by previously published climate reconstructions from other archives, as well as Holocene summer insolation changes. In conclusion, oxygen isotope records from NH extratropical lake sediments feature a common climate signal at centennial (for CE) and millennial (for Holocene) timescales despite stemming from different lakes in different geographic locations and hence constitute a valuable proxy for past climate reconstructions.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
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  • 72
    Publication Date: 2024-06-20
    Description: In 2021, more than 50 paroxysmal episodes occurred at the South-East Crater (SEC) of Mt Etna, Italy. The 23–24 March lava fountain was one of the longest episodes and began with weak Strombolian explosions, gradually transitioning to lava fountaining. The eruption intensity then dropped more slowly than in previous episodes, resulting in pulsating Strombolian explosions dominated by ash emission. Thirty-four tephra samples were used to reconstruct the fallout dispersal and estimate the total erupted mass. Grain size, textural, petrological and geochemical analyses indicate different features and were compared with the gas phase ( SO2 and HCl) in the volcanic plume. By applying stochastic global optimization to simulations of the temporal evolution of the eruption column height and tephra dispersal and deposition, the total erupted mass retrieved (6.76 × 108 kg) matches well the total erupted mass estimation by the ground-based deposit (8.03 ± 2.38 × 108 kg), reducing the column height throughout the episode from 6.44 to 4.5 km above sea level and resulting in a mass eruption rate ranging from 1.96 × 105 to 8.18 × 103 kg/s. The unusual duration of the March episode and the characteristics of the erupted products point to the change in explosive style and magma fragmentation from fountaining to ash emission phases, associated with a slower magma supply inducing a change in magma rheology and a final, prolonged ash generation. Furthermore, this study showed that using observational data and the variation in eruption source parameters for numerical simulations can improve the accuracy of predicting the dispersal plume, thus mitigating the potential impact of longer paroxysmal episodes.
    Description: Published
    Description: 56
    Description: OSV3: Sviluppo di nuovi sistemi osservazionali e di analisi ad alta sensibilità
    Description: JCR Journal
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
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  • 73
    Publication Date: 2024-06-20
    Description: The Azores archipelago, situated east of the Mid-Atlantic Ridge, comprises volcanic islands arranged along sub-parallel spreading systems and rests on a thick oceanic crust. Magma is supplied directly from the roots of the volcanic systems. Located at or nearby the boundary between the crust and the mantle, they consist of mafic cumulates and mafic mush layers. This work focuses on tephra samples and a submarine lava younger than 40.000 years, collected from both central volcanoes and fissure zones. Our report details a new dataset of major, trace, and volatile elements analysed in glassy melt inclusions trapped in olivine (Fo75.8–85.6) which are extracted from cumulative bodies at the vicinity of the crust-mantle boundary. Their compositions cover a range from subalkaline to mildly alkaline basalt, and trachybasalt, which match those of Azores lavas. They registered a chemical evolution through fractional crystallisation of olivine alone, as well as olivine and clinopyroxene, as both the FeOt/MgO (1.4–3.1) and CaO/Al2O3 (0.4–1.0) ratios of the melt decrease. Incompatible element ratios of Zr (40–352 ppm), Ba (135–612 ppm), and Rb (5–77 ppm), as compared to Nb (5–82 ppm), exhibit variability within a limited but significant range of values. The ranges in the Nb/Zr, Ba/Nb and Rb/Nb ratios recorded by melt inclusions possibly reveal distinct geochemical sources (at least two), and mixing between partial melts as they move upward. The halogen signature is characteristic of the shallow mantle. The majority of melt inclusions show Cl/K ratio (0.06) similar to E-MORB, although some of them are comparable to N-MORB (Cl/K = 0.03). Their F/Nd ratio may achieve a rather high value (27.8).
    Description: Published
    Description: 64
    Description: OSV2: Complessità dei processi vulcanici: approcci multidisciplinari e multiparametrici
    Description: JCR Journal
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
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  • 74
    Publication Date: 2024-06-20
    Description: Seed dispersal affects gene flow and hence genetic differentiation of plant populations. During the Late Quaternary, most fruit-eating and seed-dispersing megafauna went extinct, but whether these animals have left signatures in the population genetics of their food plants, particularly those with large, ‘megafaunal’ fruits (i.e. 〉4 cm—megafruits), remains unclear.Here, we assessed the population history, genetic differentiation and recent migration among populations of four animal-dispersed palm (Arecaceae) species with large (Borassus madagascariensis), medium-sized (Hyphaene coriacea, Bismarckia nobilis) and small (Chrysalidocarpus madagascariensis) fruits on Madagascar. We integrated double-digest restriction-site-associated DNA sequencing (ddRAD) of 167 individuals from 25 populations with (past) distribution ranges for extinct (e.g., giant lemurs and elephant birds) and extant seed-dispersing animals, landscape and human impact data, and applied linear mixed-effects models to explore the drivers of genetic variation in Malagasy palms.Palm populations that shared more megafrugivore species in the past had lower genetic differentiation than populations that shared fewer megafrugivore species. This suggests that megafrugivore-mediated seed dispersal in the past may have led to frequent gene flow among populations. In comparison, extant frugivore diversity only decreased genetic differentiation in the small-fruited palm. Furthermore, genetic differentiation of all palm species decreased with landscape connectivity (i.e. environmental suitability, forest cover and river density) and human impact (i.e. road density), while migration rates of the small-fruit palm increased with road density.Synthesis. Our results suggest that the legacy of megafrugivores regularly achieving long dispersal distances is still reflected in the population genetics of palms that were formerly dispersed by such animals. Furthermore, low genetic differentiation was possibly maintained after the megafauna extinctions through alternative dispersal (e.g. human- or river-mediated), long generation times and long lifespans of these megafruit palms. Our study illustrates how species interactions that happened 〉1000 years ago can leave imprints in their population genetics.
    Keywords: Arecaceae ; ddRAD ; genetic differentiation ; megafauna extinction ; population genomics ; recent migration rate ; seed dispersal
    Repository Name: National Museum of Natural History, Netherlands
    Type: info:eu-repo/semantics/article
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  • 75
    Publication Date: 2024-06-20
    Description: In this paper, two species of the water mite genus Kongsbergia Thor, 1899 (Aturidae), i.e., K. uttarakhandensis Pešić & Smit n. sp. and K. tuzovskiji Pešić & Smit n. sp. are described from streams in Uttarakhand State of India. The latter species was named after late Dr Petr Tuzovskij for his outstanding contribution to the research of water mites.
    Keywords: Acari ; water mites ; taxonomy ; Himalayas ; new species ; streams
    Repository Name: National Museum of Natural History, Netherlands
    Type: info:eu-repo/semantics/article
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  • 76
    Publication Date: 2024-06-20
    Description: Acanthodes has long been the primary source of information on the pharyngeal skeleton of ‘acanthodians’. Because of this its anatomy has played a disproportionate role in attempts to understand the evolution of the jawed vertebrate pharynx and the clade as a whole. However, the anatomy of the pharynx of Acanthodes, now understood to be a stem-group chondrichthyan, remains poorly characterized and subject to several com- peting interpretations. We used computed tomography to image the articulated pharyngeal skeletons of three specimens of Acanthodes confusus from Lebach, Germany. Acanthodes has a mélange of osteichthyan-like and chondrichthyan-like morphologies in its pharyngeal skeleton. Like many other chondrichthyans, Acanthodes lacked hypohyals, and had four pairs of posteriorly oriented pharyngobranchials. Like osteichthyans, Acanthodes possessed an interhyal, but lacked the separate infra- and supra-pharyngobranchial elements present in osteichthyans and the crown- chondrichthyan Ozarcus. Using these new data we built and animated a digital 3D model of the pharyngeal endoskeleton in Acanthodes, showing that the jaws could have swung outwards during the opening cycle, increasing the anteriorly facing area of the gape for suspension feeding. These new data provide a more definitive picture of the anatomy of a taxon that has long been of great significance in early vertebrate palaeontology.
    Keywords: acanthodian ; branchial skeleton ; chondrichthyan ; computed tomography ; Permian ; pharynx
    Repository Name: National Museum of Natural History, Netherlands
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  • 77
    Publication Date: 2024-06-20
    Description: This study presents the mathematical framework and experiments to achieve an orbit and clock combination using Multi-GNSS products. Over the past years, the International GNSS Service (IGS) has been putting efforts into extending its service by setting up and running the Multi-GNSS Experiment and Pilot Project (MGEX). Several MGEX Analysis Centers (ACs) contribute by providing solutions containing not only GPS and GLONASS but also Galileo, BeiDou, and QZSS. As the current IGS combination software can only handle one constellation at a time, obtaining a consistent MGEX orbit and clock product requires substantial modifications. Therefore is presented a least-squares framework for a Multi-GNSS orbit and clock combination, where the weights used to combine the ACs’ products are determined by least-squares variance component estimation. Two different weighting strategies are proposed and discussed: AC specific weights or AC and constellation specific weights. An automated Z-score test is implemented, yielding a common set of core satellites that are used to determine the weights. Both strategies are tested using MGEX orbit and clock solutions for a period of two and a half years, where the two data processing yielded similar results. The agreement with the ACs’ orbits is around one centimeter level for GPS and up to a few centimeters for the other constellations. The 3D-RMS is generally slightly better with the AC and constellation weighting. As a validation of the strategies, a comparison of our combination approach with the official IGS combination using three years of GPS and GLONASS orbits shows an agreement of better than 5 mm and 12 mm for GPS and GLONASS, respectively. An external validation using Satellite Laser Ranging (SLR) shows that the mean residuals of our combined products are around −3 mm for Galileo, 6 mm for GLONASS, −8 mm for BeiDou, and −31 mm for QZSS. For the clock products, the agreement with the IGS final product is around 32 ps and the Precise Point Positioning (PPP) analysis showed that the combined product agrees with the residuals of the ACs with values of less than 10 mm. The MGEX clock combination showed that most of the ACs agreement is below 80 ps for GPS and Galileo, and for the other constellations, the values are more sparse. In addition, it is noted that SHA and JAX presented big discrepancies compared with the other ACs. The validation is performed again in comparison IGS official combination where the agreement with the presented solutions is around 32 ps. A PPP processing is also performed using the combined solutions, showing the suitability of the products. The ACs products from the IGS third reprocessing campaign are also used as input in the combination and discussed. Finally, an extension of the orbit combination is done for the combination of Low Earth Orbit (LEO) satellites. The results show that the proposed combination can deliver reliable products following the standards of the IGS.
    Description: Diese Studie stellt den mathematischen Rahmen und die Experimente vor, um eine Kombination von Umlaufbahn und Uhr mit Hilfe von Multi-GNSS-Produkten zu erreichen. In den letzten Jahren hat der International GNSS Service (IGS) Anstrengungen unternommen, um seinen Dienst durch die Einrichtung und Durchführung des Multi-GNSS-Experiment- and Pilot Project (MGEX) zu erweitern. Mehrere MGEX Analysis Centers (ACs) tragen dazu bei, indem sie Lösungen anbieten, die nicht nur GPS und GLONASS, sondern auch Galileo, BeiDou und QZSS enthalten. Da die derzeitige IGS-Kombinationssoftware jeweils nur eine Konstellation verarbeiten kann, sind für den Erhalt eines konsistenten MGEX-Bahn und Uhrenprodukts erhebliche Änderungen erforderlich. Daher wird ein Least-Squares-Rahmen für eine Multi-GNSS-Bahn- und Uhrenkombination vorgestellt, bei dem die zur Kombination der AC-Produkte verwendeten Gewichte durch eine Least-Squares-Varianzkomponentenschätzung bestimmt werden. Es werden zwei verschiedene Gewichtungsstrategien vorgeschlagen und diskutiert: AC-spezifische Gewichte oder AC- und konstellationsspezifische Gewichte. Es wird ein automatischer Z-Score-Test durchgeführt, der einen gemeinsamen Satz von Kernsatelliten ergibt, die zur Bestimmung der Gewichte verwendet werden. Beide Strategien werden anhand von MGEX-Bahn- und Uhrenlösungen über einen Zeitraum von zweieinhalb Jahren getestet, wobei die beiden Datenverarbeitungen ähnliche Ergebnisse erbrachten. Die Übereinstimmung mit den Bahnen der ACs liegt bei GPS bei etwa einem Zentimeter und bei den anderen Konstellationen bei bis zu einigen Zentimetern. Der 3D-RMS ist im Allgemeinen etwas besser mit der AC- und Konstellationsgewichtung. Zur Validierung der Strategien zeigt ein Vergleich unseres Kombinationsansatzes mit der offiziellen IGS-Kombination unter Verwendung von GPS- und GLONASS-Umlaufbahnen aus drei Jahren eine Übereinstimmung von besser als 5 mm und 12 mm für GPS bzw. GLONASS. Eine externe Validierung mittels Satellite Laser Ranging (SLR) zeigt, dass die mittleren Residuen unserer kombinierten Produkte bei etwa −3 mm für Galileo, 6 mm für GLONASS, −8 mm für BeiDou und −31 mm für QZSS liegen. Bei den Uhrenprodukten liegt die Übereinstimmung mit dem IGS-Endprodukt bei etwa 32 ps, und die Analyse der präzisen Precise Point Positioning (PPP) ergab, dass das kombinierte Produkt mit den Residuen der ACs mit Werten von weniger als 10 mm übereinstimmt. Die MGEX-Uhrenkombination zeigte, dass die meisten ACs unter 80 ps für GPS und Galileo übereinstimmen, und für die anderen Konstellationen sind die Werte spärlicher. Darüber hinaus ist festzustellen, dass SHA und JAX im Vergleich zu den anderen ACs große Diskrepanzen aufweisen. Die Validierung erfolgt wiederum im Vergleich mit der offiziellen IGS-Kombination, bei der die Übereinstimmung mit den vorgestellten Lösungen bei etwa 32 ps liegt. Eine PPP-Verarbeitung wird ebenfalls unter Verwendung der kombinierten Lösungen durchgeführt, was die Eignung der Produkte zeigt. Die ACs-Produkte aus der dritten IGS-Reprocessing-Kampagne werden ebenfalls als Input für die Kombination verwendet und diskutiert. Schließlich wird eine Erweiterung der Orbit-Kombination für die Kombination von Low Earth Orbit (LEO)-Satelliten durchgeführt. Die Ergebnisse zeigen, dass die vorgeschlagene Kombination zuverlässige Produkte gemäß den Standards des IGS liefern kann.
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  • 78
    Publication Date: 2024-06-20
    Description: Watershed management requires an understanding of key hydrochemical processes. The Pra Basin is one of the five major river basins in Ghana with a population of over 4.2 million people. Currently, water resources management faces challenges due to surface water pollution caused by the unregulated release of untreated household and industrial waste into aquatic ecosystems and illegal mining activities. This has increased the need for groundwater as the most reliable water supply. Our understanding of groundwater recharge mechanisms and chemical evolution in the basin has been inadequate, making effective management difficult. Therefore, the main objective of this work is to gain insight into the processes that determine the hydrogeochemical evolution of groundwater quality in the Pra Basin. The combined use of stable isotope, hydrochemistry, and water level data provides the basis for conceptualizing the chemical evolution of groundwater in the Pra Basin. For this purpose, the origin and evaporation rates of water infiltrating into the unsaturated zone were evaluated. In addition, Chloride Mass Balance (CMB) and Water Table Fluctuations (WTF) were considered to quantify groundwater recharge for the basin. Indices such as water quality index (WQI), sodium adsorption ratio (SAR), Wilcox diagram, and salinity (USSL) were used in this study to determine the quality of the resource for use as drinking water and for irrigation purposes. Due to the heterogeneity of the hydrochemical data, the statistical techniques of hierarchical cluster and factor analysis were applied to subdivide the data according to their spatial correlation. A conceptual hydrogeochemical model was developed and subsequently validated by applying combinatorial inverse and reaction pathway-based geochemical models to determine plausible mineral assemblages that control the chemical composition of the groundwater. The interactions between water and rock determine the groundwater quality in the Pra Basin. The results underline that the groundwater is of good quality and can be used for drinking water and irrigation purposes. It was demonstrated that there is a large groundwater potential to meet the entire Pra Basin’s current and future water demands. The main recharge area was identified as the northern zone, while the southern zone is the discharge area. The predominant influence of weathering of silicate minerals plays a key role in the chemical evolution of the groundwater. The work presented here provides fundamental insights into the hydrochemistry of the Pra Basin and provides data important to water managers for informed decision-making in planning and allocating water resources for various purposes. A novel inverse modelling approach was used in this study to identify different mineral compositions that determine the chemical evolution of groundwater in the Pra Basin. This modelling technique has the potential to simulate the composition of groundwater at the basin scale with large hydrochemical heterogeneity, using average water composition to represent established spatial groupings of water chemistry.
    Description: Die Bewirtschaftung von Wassereinzugsgebieten erfordert ein Verständnis der wichtigsten hydrochemischen Prozesse. Das Pra-Becken ist eines der fünf großen Flusseinzugsgebiete Ghanas mit einer Bevölkerung von über 4,2 Millionen Menschen. Die Bewirtschaftung der Wasserressourcen wird derzeit durch die Verschmutzung der Oberflächengewässer erschwert, die durch die unkontrollierte Einleitung von unbehandelten Haushalts- und Industrieabfällen in die aquatischen Ökosysteme und durch illegale Bergbauaktivitäten entsteht. Dies hat den Bedarf an Grundwasser als zuverlässigste Wasserversorgung erhöht. Unser Verständnis der Mechanismen der Grundwasserneubildung und der chemischen Entwicklung im Einzugsgebiet ist bislang unzureichend, was eine wirksame Bewirtschaftung erschwert. Daher ist das Hauptziel dieser Arbeit Einblicke in die Prozesse zu bekommen, welche die hydrogeochemische Entwicklung der Grundwasserqualität im Pra-Becken bestimmen. Die kombinierte Verwendung von Daten stabiler Isotope, der Hydrochemie und von Wasserständen bildet die Grundlage für die Konzeption der chemischen Entwicklung des Grundwassers im Pra-Becken. Dafür wurden die Herkunft und die Verdunstungsraten des in die ungesättigte Zone infiltrierenden Wassers bewertet. Darüber hinaus wurden die Chlorid-Massenbilanz und die Wasserspiegelschwankungen betrachtet, um die Grundwasserneubildung für das Einzugsgebiet zu quantifizieren. Indizes wie der Wasserqualitätsindex (WQI), das Natriumadsorptionsverhältnis (SAR), das Wilcox-Diagramm und der Salzgehalt (USSL) wurden in dieser Studie verwendet, um die Qualität der Ressource für die Verwendung als Trinkwasser und zu Bewässerungszwecken zu bestimmen. Aufgrund der Heterogenität der hydrochemischen Daten wurden die statistischen Verfahren der hierarchischen Cluster- und Faktorenanalyse angewandt, um die Daten entsprechend ihrer räumlichen Korrelation zu unterteilen. Ein konzeptionelles hydrogeochemisches Modell wurde entwickelt und anschließend durch Anwendung kombinatorischer inverser und reaktionspfadbasierter geochemischer Modelle validiert, um plausible mineralische Assemblagen zu bestimmen, welche die chemische Zusammensetzung des Grundwassers kontrollieren. Die Wechselwirkungen zwischen Wasser und Gestein bestimmen die Grundwasserqualität im Pra-Becken. Die Ergebnisse unterstreichen, dass das Grundwasser eine gute Qualität aufweist und als Trinkwasser und für Bewässerungszwecke genutzt werden kann. Es wurde nachgewiesen, dass ein großes Grundwasserpotenzial vorhanden ist, um den derzeitigen und künftigen Wasserbedarf des gesamten Pra-Beckens zu decken. Als Hauptneubildungsgebiet wurde die nördliche Zone im Gebiet identifiziert, während die südliche Zone das Abflussgebiet ist. Der vorherrschende Einfluss der Verwitterung von Silikatmineralen spielt bei der chemischen Entwicklung des Grundwassers eine zentrale Rolle. Die hier vorgestellte Arbeit gibt grundlegende Einblicke in die Hydrochemie des Pra-Beckens und liefert für das Wassermanagement wichtige Daten für eine fundierte Entscheidungsfindung bei der Planung und Zuweisung von Wasserressourcen für verschiedene Zwecke. Ein neuartiger Ansatz zur inversen Modellierungwurde in dieser Studie eingesetzt, um unterschiedliche Mineralzusammensetzungen zu ermitteln, welche die chemische Entwicklung des Grundwassers im Pra-Becken bestimmen. Diese Modellierungstechnik hat das Potenzial, die Zusammensetzung eines Grundwassers auf der Skala eines Beckens mit großer hydrochemischer Heterogenität zu simulieren, wobei die durchschnittliche Wasserzusammensetzung zur Darstellung der etablierten räumlichen Gruppierungen der Wasserchemie verwendet wird.
    Description: Watershed management requires an understanding of key hydrochemical processes. The Pra Basin is one of the five major river basins in Ghana with a population of over 4.2 million people. Currently, water resources management faces challenges due to surface water pollution caused by the unregulated release of untreated household and industrial waste into aquatic ecosystems and illegal mining activities. This has increased the need for groundwater as the most reliable water supply. Our understanding of groundwater recharge mechanisms and chemical evolution in the basin has been inadequate, making effective management difficult. Therefore, the main objective of this work is to gain insight into the processes that determine the hydrogeochemical evolution of groundwater quality in the Pra Basin. The combined use of stable isotope, hydrochemistry, and water level data provides the basis for conceptualizing the chemical evolution of groundwater in the Pra Basin. For this purpose, the origin and evaporation rates of water infiltrating into the unsaturated zone were evaluated. In addition, Chloride Mass Balance (CMB) and Water Table Fluctuations (WTF) were considered to quantify groundwater recharge for the basin. Indices such as water quality index (WQI), sodium adsorption ratio (SAR), Wilcox diagram, and salinity (USSL) were used in this study to determine the quality of the resource for use as drinking water and for irrigation purposes. Due to the heterogeneity of the hydrochemical data, the statistical techniques of hierarchical cluster and factor analysis were applied to subdivide the data according to their spatial correlation. A conceptual hydrogeochemical model was developed and subsequently validated by applying combinatorial inverse and reaction pathway-based geochemical models to determine plausible mineral assemblages that control the chemical composition of the groundwater. The interactions between water and rock determine the groundwater quality in the Pra Basin. The results underline that the groundwater is of good quality and can be used for drinking water and irrigation purposes. It was demonstrated that there is a large groundwater potential to meet the entire Pra Basin’s current and future water demands. The main recharge area was identified as the northern zone, while the southern zone is the discharge area. The predominant influence of weathering of silicate minerals plays a key role in the chemical evolution of the groundwater. The work presented here provides fundamental insights into the hydrochemistry of the Pra Basin and provides data important to water managers for informed decision-making in planning and allocating water resources for various purposes. A novel inverse modelling approach was used in this study to identify different mineral compositions that determine the chemical evolution of groundwater in the Pra Basin. This modelling technique has the potential to simulate the composition of groundwater at the basin scale with large hydrochemical heterogeneity, using average water composition to represent established spatial groupings of water chemistry.
    Language: English
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  • 79
    Publication Date: 2024-06-20
    Description: Source rocks for oil and gas, and reservoir rocks represent two key elements of every petroleum system. Evaluating individual plays significantly benefits from an enhanced understanding of all processes that interact during the lifetime of petrogenic fluids. In particular, establishing relationships among oils and between oils and related source rocks can be challenging when geochemical signatures of all components show high similarities with some spatial and temporal variations. Furthermore, organic-inorganic interaction within carbonate reservoirs due to the effects of aqueous fluids on reservoir quality are yet poorly understood. In this thesis, both topics were investigated on (i) a petroleum system in the Western Desert area of Egypt and (ii) on Cretaceous carbonate reservoirs in the Central Oman basins from a modern analytical perspective together with various conventional geochemical methods, and the analysis of stable carbon and hydrogen isotopes of organic molecules. Principally, a petroleomic approach conducting high-resolution Fourier transform-ion cyclotron resonance-mass spectrometry (FT-ICR-MS) allowed recognizing minute geochemical differences. (1) The northern area of the Western Desert of Egypt hosts crude oils in different stratigraphic levels, mainly in Cretaceous strata, which likely derived from multiple sources given the variety of geochemical signatures. Five oil families were identified based on phenolic content, isotope patterns, polar (ESI-N), and low-polarity Ox-containing compounds (APPI-P). For further differentiation, a novel maturity-related molecular ratio was established, based on the increasing abundances of aromatic hydrocarbons with 10 and 13 double bond equivalents (DBEs) relative to the 7 DBE species with thermal maturity. This parameter efficiently covers the maturity range between 0.78 and 1.0 % vitrinite reflectance equivalent (VRe). The source resolution that was principally achieved using FT-ICR-MS highlights the importance of this petroleomics technique for studying petroleum systems with small compositional variability. (2) Cretaceous carbonate reservoirs of the lower Shuaiba Formation in Central Oman exhibit higher porosities and permeabilities in the topmost reservoir zone than in the underlying reservoir compartments. This yet open feature offered potential to study whether organic-inorganic interactions during petroleum emplacement which led to carbonate dissolution and porosity enhancement. The results of this study demeonstrated that depositional and early diagenetic conditions were the major controls on the lateral and vertical porosity distribution in the Shuaiba reservoir. Two successive depositional cycles led to a dissolution-susceptible grain-rich facies overlying a muddy facies, which significantly influenced the vertical variation in pore geometries. An early diagenetic fingerprint includes moderate karstification indicated by a thin film cement on carbonate clasts forming a meniscus pattern at the topmost Shuaiba carbonates during subaerial exposure in the study area. Three different oil families occur in the A, B, and C oilfields, and represent the central Oman Q, the South Oman Huqf, and the north Oman Huqf oil families, respectively. Results about biomarkers and their stable carbon isotopic composition suggest that these fluids were likely sourced from late Precambrian-Cambrian Tasmanite-rich carbonate source rocks. A number of 77 samples studied across the water leg into oil columns in the fields A, B, and C reflects a homogeneous composition toward the oil-water contact (OWC) and the water leg. The consistency in the saturated hydrocarbons concentration and ratios of isoprenoid/n-alkanes (〈1), pristane/phytane, and 9-methylphenanthrene (9-MP)/1-methylphenanthrene (1-MP) indicate that the Shuaiba reservoir is free of biodegradation. Thus the expected alteration due to bioactivity was excluded to cause an imbalance in the hydrogeological system (e.g., drop in pH, etc.) of the reservoir. Alternatively, the corrosive environment created by the petroleum accumulation that might increase porosity through extensive organic-inorganic interactions leading to carbonate dissolution was further considered. In such case, hydrolytic disproportionation caused by water phase -in the absence of mineral oxidants- may also represent an effective factor of generating acidic alteration products such as, CO2 and carboxylic acids. A late diagenetic event has been recorded from the Lower Shuaiba reservoir during the emplacement of hydrocarbons and the associated high-temperature aqueous fluids, which caused fluid-rock interactions during the mixing and cooling processes leading to a reduction in porosity. In the presence of formation water the petroleum emplacement caused; (a) dolomitization of reservoir rock, (b) hydrolysis of hydrocarbons and generation of acidic components that led to calcite dissolution and precipitation at the underlying reservoir compartments either by a higher pH due to increasing water saturation or mud content indicated by the precipitation of carbonate mud only at the OWC in shallower reservoirs, and (b) simultaneous precipitation of sulfide and calcite during thermochemical sulfate reduction. In water-dry reservoirs, the cooling of the hot aqueous fluid associated with petroleum caused; (a) recrystallization of the reservoir rock matrix and (b) porosity reduction by the precipitation of the suspended carbonate material in pore cavities which formed by the incoming aqueous fluids along migration pathways as well as the precipitation of sulfide and calcite by the thermochemical sulfate reduction mechanism in deeper reservoirs. Furthermore, the pattern of a cross-cutting vuggy pore-system enabled sulfide mineralization, and suggests that the emplacement of the mixture of a mineralizing fluid and associated hydrocarbons occurred later than the preserved early diagenetic porosity. Hence, different diagenetic processes and associated fluid-rock interactions can be unraveled by a multi-analytical approach using petrography of reservoir mineralogy besides organic geochemical analyses of the reservoir oil. In summary, this thesis provides results of interdisciplinary molecular geochemical investigations that enable the identification of five petroleum systems with five different oil families in various northern Western Desert basins. Such approach particularly in the Shushan Basin enabled an unravelling of oil-oil and oil-source correlations despite small compositional variability of oil and related source rock extracts. These accurate molecular investigations are afforded by combining results from FT-ICR-MS and stable isotopes of organic compounds together with imaging results. As a results, the key controls were identified causing a higher reservoir quality at the topmost zone of the lower Shuaiba Formation, as well as further organic-inorganic interactions which modify the reservoir properties of carbonate reservoirs.
    Description: Mutter- und Speichergestein für Öl und Gas stellen zwei Schlüsselelkomponenten in jedem Erdölsystem dar. Eine Evaluierung einzelner Erdölvorkommen profitiert erheblich von einem besseren Verständnis aller interagierenden Prozesse, die in einem Erdölsystem unter Beteiligung unterschiedlicher Fluide ablaufen. Insbesondere Öl-Öl- und Öl-BitumenKorrelationen sind komplexe Fragestellungen, wenn die organo-geochemische Zusammensetzung der Fluide sehr ähnlich sind und räumlich und zeitlich nur leichte Variationen aufweist. Darüber hinaus sind die organisch-anorganischen Wechselwirkungen in Karbonatlagerstätten aufgrund der Auswirkungen wässriger Fluide auf die Lagerstättenqualität noch nicht ausreichend erforscht. In dieser Arbeit wurden beide Themen untersucht am Beispiel (i) eines Erdölsystems in Ägypten und (ii) an karbonatischen Lagerstätten aus der Kreidezeit im zentralen Oman-Becken mit Helfe einer modernen analytischen Herangehensweise untersucht, bei der neben der Gesamtzusammensetzung auch einzele Biomarker und deren stabile Kohlenstoff- und Wasserstoffisotope-Signaturen analysiert wurden. Der Einsatz der hochauflösenden FourierTransformations-Ionenzyklotron-Resonanz-Massenspektrometrie (FT-ICR-MS), ermöglichte heir die Erkennung kleinster geochemischer Unterschiede („Petroleomics“). (1) Im nördlichen Gebiet der westlichen Wüste Ägyptens befinden sich Erdöle in verschiedenen stratigraphischen Schichten, hauptsächlich aus der Kreidezeit, deren unterschiedliche Zusammensetzung auf verschiedene Muttergesteine hindeutet. Fünf Ölfamilien wurden anhand des Phenolgehalts, der Kohlenstoffisotopensignatur der n-Alkane, sowie der Zusammensetzung der aciden (ESI-N) und der niedrigpolaren (APPI-P) sauerstoffhaltigen Verbindungen identifiziert. Zur weiteren Differenzierung wurde ein neuer Reifeparameter entwickelt, der auf der mit zunehmender thermischen Reife zunehmenden Häufigkeit von aromatischen Kohlenwasserstoffen mit 10 und 13 Doppelbindungsäquivalenten (DBE) relativ zu den 7 DBE-Spezies basiert. Dieser Parameter deckt den im untersuchten Probensatz abgedeckten Reifebereich von 0,7 bis 1,0 % berechneter Vitrinit-reflexion (VRe) effizient ab. Die Identifizierung der unterschiedlichen Herkunft der Öle, die hauptsächlich mit FT-ICR-MS erreicht wurde, unterstreicht die Bedeutung dieser petroleomischen Technik für die Untersuchung von Erdölsystemen mit geringer Variabilität in der Zusammensetzung. (2) Kretazische Karbonatreservoire in der unteren Shuaiba Formation in Zentral-Oman weisen in der obersten Lagerstättenzone höhere Porositäten und Permeabilitäten auf als in den Zusammenfassung VIII darunter liegenden Kompartimenten. Dies kann mit organisch-anorganischen Wechselwirkungen während der Erdöleinlagerung erklärt werden, die zur Auflösung von Karbonat und damit zur Erhöhung der Porosität führten. Ablagerungs- und frühe diagenetische Bedingungen haben die laterale und vertikale Porositätsverteilung in den Shuaiba-Lagerstätten maßgeblich beeinflusst. Zwei aufeinanderfolgende Ablagerungszyklen führten zu einer auflösungsanfälligen, kornreichen Fazies, die von einer schlammigen Fazies überlagert wird, was zu einer erheblichen vertikalen Variation der Porengeometrien führte. Ein früher diagenetischer Fingerabdruck umfasst eine mäßige Verkarstung der obersten ShuaibaKarbonate während einer Verlandungsphase im Untersuchungsgebiet, die durch einen dünnen Filmzement auf Karbonatklasten angezeigt wird, der ein Meniskusmuster bildet. In den Ölfeldern A, B und C befinden sich die drei Ölfamilien Zentral-Oman Q, SüdOman Huqf bzw. Nord-Oman Huqf. Die Ergebnisse zu den Biomarkern und der stabilen Kohlenstoff-Isotopenzusammensetzung der n-Alkane deuten darauf hin, dass diese Fluide wahrscheinlich aus spätpräkambrischen bis kambrischen tasmanitreichen karbonatischen Muttergesteinen mit niedrigem Reifegrad stammen. Die Untersuchung von 77 untersuchten Proben aus den Ölsäulen in den Feldern A, B und C zeigt eine homogene Zusammensetzung in Richtung des Öl-Wasser-Kontakts (OWC) und auch darunter. Die unveränderten Konzentrationen an gesättigten Kohlenwasserstoffen und die Verhältnisse von Isoprenoiden zu n-Alkanen (〈1), Pristan zu Phytan und 9-Methylphenanthren (9-MP) zu 1-Methylphenanthren (1-MP) deuten darauf hin, dass in der Shuaiba-Lagerstätte kein biologischer Abbau durch Mikroorgansimen stattgefunden hat. Somit kann ausgeschlossen werden, dass das hydrogeologische System im Reservoir Alterationen (wie z. B. ein Absinken des pH-Werts usw.) hervorgerufen hat. Alternativ kann die bei der frühen Erdölanreicherung entstehende korrosive Umgebung die Porosität durch umfangreiche organisch-anorganische Wechselwirkungen erhöhen und zur Karbonatauflösung führen, z.B. durch die hydrolytische Disproportionierung durch die Wasserphase, die in Abwesenheit von mineralischen Oxidationsmitteln zur Bildung saurer Alterationsprodukte wie CO2 und kurzkettigen organischen Säuren führen kann. In der unteren Shuaiba-Lagerstätte wurde während Befüllung mit Kohlenwasserstoffen und heißen wässrigen H Lösungen die Porosität reduziert, was Resultat von Mischungs- und Abkühlungsprozessen war. Das Vorhandensein von Formationswasser während der Einlagerung von Kohlenwasserstoffen bewirkte somit einerseits die Dolomitisierung des Lagerstättengesteins. Andererseits wurden durch die Hydrolyse von Kohlenwasserstoffen Zusammenfassung IX saure Komponenten erzeugt, die zur Kalzitauflösung und -ausfällung in den darunter liegenden Lagerstättenkompartimenten führen, entweder durch einen höheren pH-Wert oder durch einen höheren Schlammgehalt, der durch die Ausfällung von Karbonatschlamm nur im OWC in flacheren Lagerstätten angezeigt wird. Ein weiterer Faktor war die gleichzeitige Ausfällung von Sulfid und Kalzit während der thermochemischen Sulfatreduktion. In trockenen Lagerstättenbereichen führte die Abkühlung nachträglich infiltrierter heißer wässrigen Flüssigkeit zu (a) einer Rekristallisation der Gesteinsmatrix, und (b) einer Verringerung der Porosität durch die Ausfällung des suspendierten Karbonatmaterials, das von den einströmenden wässrigen Flüssigkeiten gelöst und entlang der Migrationspfade transportiert wurde, sowie durch die Ausfällung von Sulfid und Calcit durch thermochemische Sulfatreduktion in tieferen Lagerstätten. Darüber hinaus deutet das Muster eines quer verlaufenden, von einer Sulfidmineralisierung eingeschlossenen Porensystems darauf hin, dass die Einlagerung des Gemischs aus einem mineralisierenden Fluid und assoziierten Kohlenwasserstoffen später erfolgte als die erhaltene frühe diagenetische Porosität. Die verschiedenen diagenetischen Prozesse und die damit verbundenen Wechselwirkungen zwischen Fluid und Gestein können daher durch einen multianalytischen Ansatz entschlüsselt werden, bei dem neben der petrographischen Untersuchung der Lagerstättenmineralogie auch organisch-geochemische Analysen des Lagerstättenöls durchgeführt werden. Zusammenfassend liefert diese Arbeit Ergebnisse interdisziplinärer molekulargeochemischer Untersuchungen, die die Identifizierung von fünf Erdölsystemen mit fünf verschiedenen Ölfamilien in verschiedenen Becken der nördlichen Westwüste Ägyptens ermöglichen. Dieser Ansatz ermöglichte insbesondere im Shushan-Becken die Entschlüsselung von Öl-Öl- und Öl-Quellen-Korrelationen trotz einer geringen Variabilität in der Zusammensetzung des Öls und der zugehörigen Muttergesteinsextrakte. Diese präzisen molekularen Untersuchungen werden durch die Kombination von FT-ICR-MS-Ergebnissen und stabilen Isotopen organischer Verbindungen zusammen mit mikroskopischen Ergebnissen ermöglicht. Als Ergebnis wurden die wichtigsten Faktoren identifiziert, die eine höhere Lagerstättenqualität in der obersten Zone der unteren Shuaiba-Formation bewirken, sowie weitere organisch-anorganische Wechselwirkungen, die die Lagerstätteneigenschaften von karbonatischen Lagerstätten verändern.
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  • 80
    Publication Date: 2024-06-20
    Description: Volcanic hydrothermal systems are an integral part of most volcanoes and typically involve a heat source, adequate fluid supply, and fracture or pore systems through which the fluids can circulate within the volcanic edifice. Associated with this are subtle but powerful processes that can significantly influence the evolution of volcanic activity or the stability of the near-surface volcanic system through mechanical weakening, permeability reduction, and sealing of the affected volcanic rock. These processes are well constrained for rock samples by laboratory analyses but are still difficult to extrapolate and evaluate at the scale of an entire volcano. Advances in unmanned aircraft systems (UAS), sensor technology, and photogrammetric processing routines now allow us to image volcanic surfaces at the centimeter scale and thus study volcanic hydrothermal systems in great detail. This thesis aims to explore the potential of UAS approaches for studying the structures, processes, and dynamics of volcanic hydrothermal systems but also to develop methodological approaches to uncover secondary information hidden in the data, capable of indicating spatiotemporal dynamics or potentially critical developments associated with hydrothermal alteration. To accomplish this, the thesis describes the investigation of two near-surface volcanic hydrothermal systems, the El Tatio geyser field in Chile and the fumarole field of La Fossa di Vulcano (Italy), both of which are among the best-studied sites of their kind. Through image analysis, statistical, and spatial analyses we have been able to provide the most detailed structural images of both study sites to date, with new insights into the driving forces of such systems but also revealing new potential controls, which are summarized in conceptual site-specific models. Furthermore, the thesis explores methodological remote sensing approaches to detect, classify and constrain hydrothermal alteration and surface degassing from UAS-derived data, evaluated them by mineralogical and chemical ground-truthing, and compares the alteration pattern with the present-day degassing activity. A significant contribution of the often neglected diffuse degassing activity to the total amount of degassing is revealed and constrains secondary processes and dynamics associated with hydrothermal alteration that lead to potentially critical developments like surface sealing. The results and methods used provide new approaches for alteration research, for the monitoring of degassing and alteration effects, and for thermal monitoring of fumarole fields, with the potential to be incorporated into volcano monitoring routines
    Description: Vulkanische Hydrothermalsysteme sind ein integraler Bestandteil vieler Vulkane und erfordern allgemein eine ausreichende Wärmequelle, eine ausreichende Flüssigkeitszufuhr und Kluft- oder Porensysteme, durch die Flüssigkeiten zirkulieren können. Damit verbunden sind subtile, aber wirksame Prozesse, welche die Entwicklung der vulkanischen Aktivität oder die Stabilität des oberflächennahen Vulkansystems durch mechanische Schwächung, Verringerung der Durchlässigkeit und Versiegelung des betroffenen vulkanischen Gesteins erheblich beeinflussen können. Solche Prozesse sind für Gesteinsproben durch Laboranalysen gut definiert, aber es ist immer noch schwierig sie auf der Skala eines ganzen Vulkans zu bewerten. Fortschritte bei unbemannten Flugsystemen (UAS), Sensortechnologie und photogrammetrischen Prozessierungs-routinen ermöglichen es uns heute, Vulkanoberflächen im Zentimeterbereich abzubilden und damit vulkanische Hydrothermalsysteme sehr detailliert zu untersuchen. Ziel dieser Arbeit ist es, deren Potenzial für die Untersuchung der Strukturen, Prozesse und Dynamik solcher Systeme zu erforschen, aber auch methodische Ansätze zu finden, um in den Daten verborgene Sekundärinformationen zu analysieren, die auf raum-zeitliche Dynamiken oder potenziell kritische Entwicklungen im Zusammenhang mit hydrothermaler Alteration hinweisen können. Wir haben zwei oberflächennahe vulkanische hydrothermale Systeme analysiert, das Geysirfeld von El Tatio in Chile und das Fumarolenfeld von La Fossa di Vulcano in Italien, die beide zu den am besten untersuchten Systemen ihrer Art gehören. Durch Bildanalyse, statistische und räumliche Analysen konnten wir das bisher detaillierteste Abbild des strukturellen Aufbaus beider Standorte erstellen, neue Einblicke in die oft faszinierende Systematik solcher Systeme geben, aber auch neue potenzielle Kontrollfaktoren aufzeigen. Die Ergebnisse werden in konzeptionellen Modellen zusammengefasst. Darüber hinaus haben wir methodische Ansätze der Fernerkundung zur Erkennung, Klassifizierung und räumlichen Eingrenzung hydrothermaler Alteration aus UAS-Daten untersucht, durch mineralogisches und chemisches „Ground-Truthing“ bewertet und die Alterationsmuster mit der aktuellen Entgasungsaktivität verglichen. Wir zeigen dass die oft nicht berücksichtigte diffuse Aktivität einen signifikanten Beitrag zur Gesamtaktivität liefert, aber auch Bereiche in denen sekundäre Prozesse hydrothermaler Alteration scheinbar zu potenziell kritischen Entwicklungen wie Oberflächenversiegelung führen. Die Ergebnisse und die verwendeten Methoden bieten neue Ansätze für die Alterationsforschung, für die Überwachung von Entgasungs- und Alterationseffekten und für die thermische Überwachung von Fumarolenfeldern, und haben Potential in Vulkanüberwachungsroutinen integriert zu werden.
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  • 81
    Publication Date: 2024-06-20
    Description: Assessing the impact of global change on hydrological systems is one of the greatest hydrological challenges of our time. Changes in land cover, land use, and climate have an impact on water quantity, quality, and temporal availability. There is a widespread consensus that, given the far-reaching effects of global change, hydrological systems can no longer be viewed as static in their structure; instead, they must be regarded as entire ecosystems, wherein hydrological processes interact and coevolve with biological, geomorphological, and pedological processes. To accurately predict the hydrological response under the impact of global change, it is essential to understand this complex coevolution. The knowledge of how hydrological processes, in particular the formation of subsurface (preferential) flow paths, evolve within this coevolution and how they feed back to the other processes is still very limited due to a lack of observational data. At the hillslope scale, this intertwined system of interactions is known as the hillslope… Die Einschätzung der Auswirkungen des globalen Wandels auf die lokale Hydrologie stellt zweifellos eine der bedeutendsten hydrologischen Herausforderungen unserer Zeit dar. Die zuverlässige Vorhersage der zukünftigen Verfügbarkeit, Menge und Qualität des Wassers in Landschaften gewinnt dabei an höchster Bedeutung. Es herrscht weitgehender Konsens darüber, dass hydrologische Systeme aufgrund des globalen Wandels nicht mehr als statische Gebilde betrachtet werden können. Vielmehr sind sie als ganzheitliche Ökosysteme zu verstehen, in denen hydrologische Prozesse mit biologischen, geomorphologischen und pedologischen Faktoren interagieren und sich gemeinsam entwickeln. Allerdings ist das Wissen über die Entwicklung und die Rückkopplung hydrologischer Prozesse, insbesondere im Hinblick auf die Entstehung unterirdischer (präferenzieller) Fließwege, aufgrund mangelnder Beobachtungsdaten noch stark begrenzt. Das Hauptziel dieser Studie liegt daher darin, anhand von Untersuchungen auf der Hangskala die Wechselwirkung zwischen Struktur und…
    Description: Die Einschätzung der Auswirkungen des globalen Wandels auf die lokale Hydrologie stellt zweifellos eine der bedeutendsten hydrologischen Herausforderungen unserer Zeit dar. Die zuverlässige Vorhersage der zukünftigen Verfügbarkeit, Menge und Qualität des Wassers in Landschaften gewinnt dabei an höchster Bedeutung. Es herrscht weitgehender Konsens darüber, dass hydrologische Systeme aufgrund des globalen Wandels nicht mehr als statische Gebilde betrachtet werden können. Vielmehr sind sie als ganzheitliche Ökosysteme zu verstehen, in denen hydrologische Prozesse mit biologischen, geomorphologischen und pedologischen Faktoren interagieren und sich gemeinsam entwickeln. Allerdings ist das Wissen über die Entwicklung und die Rückkopplung hydrologischer Prozesse, insbesondere im Hinblick auf die Entstehung unterirdischer (präferenzieller) Fließwege, aufgrund mangelnder Beobachtungsdaten noch stark begrenzt. Das Hauptziel dieser Studie liegt daher darin, anhand von Untersuchungen auf der Hangskala die Wechselwirkung zwischen Struktur und hydrologischem Verhalten zu erforschen. Dadurch soll ein besseres Verständnis für den Rückkopplungszyklus gewonnen werden. Die vier in dieser Arbeit präsentierten Studien befassen sich mit der Entwicklung hydrologischer, biologischer und physikalischer Eigenschaften von Hängen sowie der Evolution hydrologischer Fließwege über einen Zeitraum von zehntausend Jahren in zwei unterschiedlichen geologischen Geologien. Durch die Analyse von Moränen-Chronosequenzen in zwei Gletschervorfeldern, die jeweils aus silikatreichem bzw. kalkreichem Geschiebemergel entstanden sind, wird die komplexe Koevolution in Abhängigkeit von der geologischen Beschaffenheit des Ausgangsmaterials beleuchtet. Die Ergebnisse zeigen, dass die verschiedenen Eigenschaften von silikatreichem und kalkhaltigem Ausgangsmaterial unter den gegebenen Klimabedingungen zu Unterschieden in Bodeneigenschaften, Durchlässigkeit und Wasserspeicherung führen. Dies wiederum begünstigt unterschiedliche Vegetationstypen und resultiert in vielfältigen Ökosystemen mit variierenden hydrologischen Dynamiken. Interessanterweise treibt das silikatreiche Ausgangsmaterial die Koevolution stärker an. Hierbei spielt der pH-Wert des Bodens eine Schlüsselrolle, da er Auswirkungen auf Vegetation, Bodenbildung und folglich auch auf die Hydrologie hat. Die saure Verwitterung des silikatreichen Materials begünstigt die Anreicherung organischer Substanz, was zu einer Erhöhung der Wasserspeicherkapazität des Bodens und zur Podsolisierung führt. Innerhalb weniger Jahrhunderte entwickelt sich das unterirdische Wassertransportsystem von einer vertikalen, heterogenen Matrixströmung zu fingerartigen Fließwegen und nach mehreren Jahrtausenden zu einem System aus Makroporen, wobei die Wasserspeicherung und die unterirdische, laterale Strömung überwiegen. Im Gegensatz dazu weist der kalkhaltige Standort eine hohe pH-Pufferkapazität auf. In dem basischen bis neutralen Milieu sammelt sich vergleichsweise wenig abgestorbene, organische Substanz an, was zu einer geringeren Wasserspeicherkapazität führt und die Ansiedlung von Grasvegetation begünstigt. Die Fließwege ändern lediglich ihre Form, nicht jedoch ihre Richtung. Es wurde lediglich ein Übergang von vertikaler, heterogener Matrixströmung zu vertikalen, fingerartigen Fließwegen beobachtet. Der schnelle vertikale Wassertransport mit geringer Speicherung begünstigt die Erhaltung der Grasvegetation. Die durchgeführten Studien verdeutlichen, dass die Entwicklung der Fließwege hauptsächlich von den Eigenschaften des Ausgangsgesteins und seinen Verwitterungsprodukten sowie von deren komplexen Interaktionen mit den ursprünglichen Fließwegen und der Entwicklung der Vegetation geprägt ist. Im Gegensatz dazu spielt die Zeit keine entscheidende Rolle bei der Beschreibung der Evolution der hydrologischen Reaktion. Diese Studie trägt wesentlich dazu bei, die bestehende Lücke in Beobachtungen für die Erforschung der Koevolution von hydrologischen, biologischen, geomorphologischen und pedologischen Prozessen zu schließen. Dies ist von großer Bedeutung, um Vorhersagen hydrologischer Prozesse in sich wandelnden Landschaften zu verbessern. Sie zeigt außerdem die Relevanz interdisziplinärer Studien auf, um den zukünftigen Herausforderungen in der Hydrologie im Zuge des globalen Wandels erfolgreich zu begegnen.
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  • 82
    Publication Date: 2024-06-20
    Description: Rapidly growing seismic and macroseismic databases and simplified access to advanced machine learning methods have in recent years opened up vast opportunities to address challenges in engineering and strong motion seismology from novel, datacentric perspectives. In this thesis, I explore the opportunities of such perspectives for the tasks of ground motion modeling and rapid earthquake impact assessment, tasks with major implications for long-term earthquake disaster mitigation. In my first study, I utilize the rich strong motion database from the Kanto basin, Japan, and apply the U-Net artificial neural network architecture to develop a deep learning based ground motion model. The operational prototype provides statistical estimates of expected ground shaking, given descriptions of a specific earthquake source, wave propagation paths, and geophysical site conditions. The U-Net interprets ground motion data in its spatial context, potentially taking into account, for example, the geological properties in the vicinity of observation sites. Predictions of ground motion intensity are thereby calibrated to individual observation sites and earthquake locations. The second study addresses the explicit incorporation of rupture forward directivity into ground motion modeling. Incorporation of this phenomenon, causing strong, pulse like ground shaking in the vicinity of earthquake sources, is usually associated with an intolerable increase in computational demand during probabilistic seismic hazard analysis (PSHA) calculations. I suggest an approach in which I utilize an artificial neural network to efficiently approximate the average, directivity-related adjustment to ground motion predictions for earthquake ruptures from the 2022 New Zealand National Seismic Hazard Model. The practical implementation in an actual PSHA calculation demonstrates the efficiency and operational readiness of my model. In a follow-up study, I present a proof of concept for an alternative strategy in which I target the generalizing applicability to ruptures other than those from the New Zealand National Seismic Hazard Model. In the third study, I address the usability of pseudo-intensity reports obtained from macroseismic observations by non-expert citizens for rapid impact assessment. I demonstrate that the statistical properties of pseudo-intensity collections describing the intensity of shaking are correlated with the societal impact of earthquakes. In a second step, I develop a probabilistic model that, within minutes of an event, quantifies the probability of an earthquake to cause considerable societal impact. Under certain conditions, such a quick and preliminary method might be useful to support decision makers in their efforts to organize auxiliary measures for earthquake disaster response while results from more elaborate impact assessment frameworks are not yet available. The application of machine learning methods to datasets that only partially reveal characteristics of Big Data, qualify the majority of results obtained in this thesis as explorative insights rather than ready-to-use solutions to real world problems. The practical usefulness of this work will be better assessed in the future by applying the approaches developed to growing and increasingly complex data sets.
    Description: Das rapide Wachstum seismischer und makroseismischer Datenbanken und der vereinfachte Zugang zu fortschrittlichen Methoden aus dem Bereich des maschinellen Lernens haben in den letzen Jahren die datenfokussierte Betrachtung von Fragestellungen in der Seismologie ermöglicht. In dieser Arbeit erforsche ich das Potenzial solcher Betrachtungsweisen im Hinblick auf die Modellierung erdbebenbedingter Bodenerschütterungen und der raschen Einschätzung von gesellschaftlichen Erdbebenauswirkungen, Disziplinen von erheblicher Bedeutung für den langfristigen Erdbebenkatastrophenschutz in seismisch aktiven Regionen. In meiner ersten Studie nutze ich die Vielzahl an Bodenbewegungsdaten aus der Kanto Region in Japan, sowie eine spezielle neuronale Netzwerkarchitektur (U-Net) um ein Bodenbewegungsmodell zu entwickeln. Der einsatzbereite Prototyp liefert auf Basis der Charakterisierung von Erdbebenherden, Wellenausbreitungspfaden und Bodenbeschaffenheiten statistische Schätzungen der zu erwartenden Bodenerschütterungen. Das U-Net interpretiert Bodenbewegungsdaten im räumlichen Kontext, sodass etwa die geologischen Beschaffenheiten in der Umgebung von Messstationen mit einbezogen werden können. Auch die absoluten Koordinaten von Erdbebenherden und Messstationen werden berücksichtigt. Die zweite Studie behandelt die explizite Berücksichtigung richtungsabhängiger Verstärkungseffekte in der Bodenbewegungsmodellierung. Obwohl solche Effekte starke, impulsartige Erschütterungen in der Nähe von Erdbebenherden erzeugen, die eine erhebliche seismische Beanspruchung von Gebäuden darstellen, wird deren explizite Modellierung in der seismischen Gefährdungsabschätzung aufgrund des nicht vertretbaren Rechenaufwandes ausgelassen. Mit meinem, auf einem neuronalen Netzwerk basierenden, Ansatz schlage ich eine Methode vor, umdieses Vorhaben effizient für Erdbebenszenarien aus dem neuseeländischen seismischen Gefährdungsmodell für 2022 (NSHM) umzusetzen. Die Implementierung in einer seismischen Gefährdungsrechnung unterstreicht die Praktikabilität meines Modells. In einer anschließenden Machbarkeitsstudie untersuche ich einen alternativen Ansatz der auf die Anwendbarkeit auf beliebige Erdbebeszenarien abzielt. Die abschließende dritte Studie befasst sich mit dem potenziellen Nutzen der von makroseismischen Beobachtungen abgeleiteten pseudo-Erschütterungsintensitäten für die rasche Abschätzung von gesellschaftlichen Erdbebenauswirkungen. Ich zeige, dass sich aus den Merkmalen solcher Daten Schlussfolgerungen über die gesellschaftlichen Folgen eines Erdbebens ableiten lassen. Basierend darauf formuliere ich ein statistisches Modell, welches innerhalb weniger Minuten nach einem Erdbeben die Wahrscheinlichkeit für das Auftreten beachtlicher gesellschaftlicher Auswirkungen liefert. Ich komme zu dem Schluss, dass ein solches Modell, unter bestimmten Bedingungen, hilfreich sein könnte, um EntscheidungsträgerInnen in ihren Bestrebungen Hilfsmaßnahmen zu organisieren zu unterstützen. Die Anwendung von Methoden des maschinellen Lernens auf Datensätze die sich nur begrenzt als Big Data charakterisieren lassen, qualifizieren die Mehrheit der Ergebnisse dieser Arbeit als explorative Einblicke und weniger als einsatzbereite Lösungen für praktische Fragestellungen. Der praktische Nutzen dieser Arbeit wird sich in erst in Zukunft an der Anwendung der erarbeiteten Ansätze auf wachsende und zunehmend komplexe Datensätze final abschätzen lassen.
    Language: English
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  • 83
    Publication Date: 2024-06-20
    Description: The new-generation satellite imaging spectrometers provide an unprecedented data stream to be processed into quantifiable vegetation traits. Hybrid models have gained widespread acceptance in recent years due to their versatility in converting spectral data into traits. In hybrid models, the retrieval is obtained through a machine learning regression algorithm (MLRA) trained on a wide range of simulated data. For instance, they are currently under development for trait retrieval in preparation for the upcoming Copernicus Hyperspectral Imaging Mission for the Environment (CHIME), among others targeting routine estimation of canopy nitrogen content (CNC). However, like any retrieval algorithm, the process is not error-free, and most MLRAs inherently lack an uncertainty estimation related to the retrieved traits, which implies a risk of misinterpretation when applying the model to real-world data. Therefore, this study aimed to assess epistemic uncertainty estimation strategies (Bayesian method, drop-out, quantile regression, and bootstrapping) alongside the estimation of CNC using competitive MLRAs. Each of the regression models was evaluated using three data sets: (1) simulated scenes with varying noise using the SCOPE 2.1 radiative transfer model, (2) hyperspectral images from the PRISMA sensor, and (3) field-measured data. Analysis of generated uncertainty intervals led to the following findings: First, Gaussian processes regression (GPR) offers meaningful uncertainties, primarily attributable to spectral data degradation, which provide supplementary insights into the quality of trait mapping. Second, bootstrapping uncertainties can be used as quality indicators of the reliability of the estimates retrieved by hybrid models. Yet, its variability depends on the used MLRA, which impedes trusting its variance as a confidence interval. Third, quantile regression forest (QRF), despite not being top-performing algorithm, exhibit outstanding robustness estimations and uncertainty when the spectral data is degraded, either by Gaussian noise or by striping, often occurring in satellite imagery. Fourth, bootstrapped kernel ridge regression (KRR) demonstrated comparable performance to the benchmark algorithm GPR; the retrievals and uncertainties of these two MLRAs were highly correlated. Fifth, bootstrapped partial least squares regression (PLSR) estimations and uncertainties exhibit poor robustness to noise degradation, with normalized root mean square error (NRMSE) increasing from 19% to 112%. Additionally, a GUI tool was integrated into the ARTMO software package for assessing epistemic uncertainties from the embedded regression algorithms, providing a trait mapping quality indicator for mapping applications, and improving decision-making.
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  • 84
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    Unknown
    Universität Potsdam
    Publication Date: 2024-06-20
    Description: Large parts of the Earth’s interior are inaccessible to direct observation, yet global geodynamic processes are governed by the physical material properties under extreme pressure and temperature conditions. It is therefore essential to investigate the deep Earth’s physical properties through in-situ laboratory experiments. With this goal in mind, the optical properties of mantle minerals at high pressure offer a unique way to determine a variety of physical properties, in a straight-forward, reproducible, and time-effective manner, thus providing valuable insights into the physical processes of the deep Earth. This thesis focusses on the system Mg-Fe-O, specifically on the optical properties of periclase (MgO) and its iron-bearing variant ferropericlase ((Mg,Fe)O), forming a major planetary building block. The primary objective is to establish links between physical material properties and optical properties. In particular the spin transition in ferropericlase, the second-most abundant phase of the lower mantle, is known to change the physical material properties. Although the spin transition region likely extends down to the core-mantle boundary, the ef-fects of the mixed-spin state, where both high- and low-spin state are present, remains poorly constrained. In the studies presented herein, we show how optical properties are linked to physical properties such as electrical conductivity, radiative thermal conductivity and viscosity. We also show how the optical properties reveal changes in the chemical bonding. Furthermore, we unveil how the chemical bonding, the optical and other physical properties are affected by the iron spin transition. We find opposing trends in the pres-sure dependence of the refractive index of MgO and (Mg,Fe)O. From 1 atm to ~140 GPa, the refractive index of MgO decreases by ~2.4% from 1.737 to 1.696 (±0.017). In contrast, the refractive index of (Mg0.87Fe0.13)O (Fp13) and (Mg0.76Fe0.24)O (Fp24) ferropericlase increases with pressure, likely because Fe Fe interactions between adjacent iron sites hinder a strong decrease of polarizability, as it is observed with increasing density in the case of pure MgO. An analysis of the index dispersion in MgO (decreasing by ~23% from 1 atm to ~103 GPa) reflects a widening of the band gap from ~7.4 eV at 1 atm to ~8.5 (±0.6) eV at ~103 GPa. The index dispersion (between 550 and 870 nm) of Fp13 reveals a decrease by a factor of ~3 over the spin transition range (~44–100 GPa). We show that the electrical band gap of ferropericlase significantly widens up to ~4.7 eV in the mixed spin region, equivalent to an increase by a factor of ~1.7. We propose that this is due to a lower electron mobility between adjacent Fe2+ sites of opposite spin, explaining the previously observed low electrical conductivity in the mixed spin region. From the study of absorbance spectra in Fp13, we show an increasing covalency of the Fe-O bond with pressure for high-spin ferropericlase, whereas in the low-spin state a trend to a more ionic nature of the Fe-O bond is observed, indicating a bond weakening effect of the spin transition. We found that the spin transition is ultimately caused by both an increase of the ligand field-splitting energy and a decreasing spin-pairing energy of high-spin Fe2+.
    Description: Geodynamische Prozesse werden von den physikalischen Materialeigenschaften unter den extremen Druck- und Temperaturbedingungen des Erdinneren gesteuert, gerade diese Areale sind aber faktisch nicht für direkte Beobachtungen zugänglich. Umso wichtiger ist es, die physikalischen Eigenschaften unter Bedingungen des Erdinneren zu untersuchen. Mit diesem Ziel vor Augen erlaubt das Studium der optischen Eigenschaften von Mineralen des Erdmantels, eine große Bandbreite an physikalischen Materialeigenschaften, in einer einfachen, reproduzierbaren und effizienten Art und Weise zu bestimmen. Dadurch bieten sich wichtige Einblicke in die physikalischen Prozessen des Erdinneren. Die vorliegende Arbeit konzentriert sich auf das System Mg-Fe-O, im Speziellen auf Periklas (MgO) und seine Eisen-haltige Variante Ferroperiklas ((Mg,Fe)O), ein wichtiger Baustein planetarer Körper. Das Hauptziel der Arbeit besteht darin Verbindungen zwischen optischen Eigenschaften und physikalischen Materialeigenschaften zu finden. Gerade der Spin-Übergang in Ferroperiklas, der zweithäufigsten Phase des unteren Erdmantels, ist dabei von Bedeutung, da damit Veränderungen in den physikalischen Materialeigenschaften einhergehen. Obwohl sich der Spinübergangsbereich vermutlich bis zur Kern-Mantel-Grenze erstreckt, sind die Auswirkungen des gemischten Spin-Zustandes, bei dem sowohl Hoch- als auch Tief-Spin präsent sind, nur unzureichend untersucht. Die hier vorgestellten Studien zeigen, wie optische Eigenschaften mit anderen wichtigen physikalischen Eigenschaften wie elektrischer und thermischer Leitfähigkeit, Viskosität oder auch mit der chemischen Bindung verbunden sind. Daraus lässt sich auch ableiten wie der Spin-Übergang in Ferroperiklas diese Eigenschaften beeinflusst. Von Raumbedingungen bis zu ~140 GPa sinkt der Brechungsindex von MgO um ~2.4 % von 1.737 auf 1.696 (±0.017). Im Gegensatz dazu steigt der Brechungsindex von (Mg0.87Fe0.13)O (Fp13) und (Mg0.76Fe0.24)O (Fp24) Ferroperiklas mit dem Druck an. Dies ist auf Fe-Fe Wechselwirkungen zwischen benachbarten Eisenpositionen zurückzuführen, die eine starke Verringerung der Polarisierbarkeit, wie im Falle von reinem MgO mit zunehmender Dichte, behindern. Eine Analyse der Dispersion des Brechungsindexes von MgO (Abnahme um ~23 % von 1 Atm zu ~103 GPa) offenbart eine Verbreiterung der Bandlücke von ~7.4 eV bei 1 Atm zu ~8.5 (±0.6) eV bei ~103 GPa. Die Messung der Dispersion (zwischen 550 und 870 nm) in Fp13 zeigt eine starke Abnahme über den Bereich des Spin-Überganges (~44–100 GPa) bis zu einem Faktor von ~3. Die Bandlücke nimmt in der Region des gemischten Spin-Zustandes signifikant auf bis zu ~4.7 eV zu (entspricht einer Zunahme um den Faktor ~1.7). Dies deutet auf eine Verringerung der Elektronen-Mobilität zwischen benachbarten Fe2+-Positionen mit unterschiedlichem Spin-Zustand hin, was die bereits in früheren Arbeiten beobachtete Abnahme der elektrischen Leitfähigkeit im Bereich des gemischten Spin-Zustandes erklärt. Absorptionsspektren an Fp13 zeigen eine Druck-bedingte Zunahme der Kovalenz der Fe-O Bindung für Ferroperiklas im Hoch-Spin Zustand, wohingegen Tief-Spin Ferroperiklas einen Trend zu einer mehr ionischen Fe-O Bindung auf-weist, was auf einen Bindungs-schwächenden Effekt des Spin-Wechsels hinweist. Der Übergang von Hoch- zu Tiefspin ist letztlich auf eine Zunahme der Ligandenfeldaufspaltungsenergie sowie eine abnehmende Spinpaarungsenergie von Hoch-Spin Fe2+ zurückzuführen.
    Language: English
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  • 85
    Publication Date: 2024-06-20
    Description: A natural gem quality, inclusion-free, U-poor xenotime has been metasomatically altered at 900 °C and 500–1000 MPa in a series of alkali-bearing fluids including 2 N KOH, 2 N NaOH, Na2Si2O5 + H2O, and NaF + H2O to which UO2 and SiO2 have been added. All experiments were buffered to CO2-CO-graphite with the exception of the NaF + H2O experiment at 900 °C and 500 MPa, which was buffered to magnetite-hematite. With the exception of the Na2Si2O5 + H2O experiment, the xenotime reacted with the fluid tried in all of the remaining experiments to varying degrees. The xenotime showed the greatest degree of reactivity in the two NaF + H2O experiments tried. This reactivity takes the form of a coupled dissolution-reprecipitation reaction, which involves enriching reacted areas of the xenotime in U + Si as well as remobilizing the HREE in these areas inherent to the original xenotime. One result was the formation of alternating bands of Y-rich and HREE- + U-rich bands in the NaF + H2O experiment when the system was oxidized, which are presumed to have formed due a combination of simple chemical zoning coupled with diffusion and coupled dissolution-reprecipitation in the altered areas of the xenotime. A total lack of fluid and mineral inclusions on the nano-scale, as well as no disturbances in the crystal lattice in the reacted areas of the xenotime under HRTEM imaging, indicated that total recrystallization of the reacted areas took place during the course of the NaF + H2O experiment. The results of these experiments has important implications for the metasomatic resetting of the xenotime geochromometer in the presence of alkali-bearing fluids, which would potentially allow metasomatised xenotime to time and record metasomatic events affecting the rock.
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  • 86
    Publication Date: 2024-06-20
    Description: The ongoing monitoring of terrestrial carbon fluxes (TCF) goes hand in hand with progress in technical capacities, such as the next-generation Earth observation missions of the Copernicus initiative and advanced machine learning algorithms. Proceeding along this line, we present a physically-based data-driven workflow for quantifying gross primary productivity (GPP) and net primary productivity (NPP) at a global scale from the synergy of Copernicus’ Sentinel-3 (S3) Ocean and Land Color Instrument (OLCI) and the TROPOspheric Monitoring Instrument (TROPOMI) onboard Sentinel-5 Precursor (S5P), along with meteorological variables from Copernicus ERA5-Land. Specifically, we created generic hybrid Gaussian process regression (GPR) retrieval models combining S3-OLCI-derived vegetation products with the TROPOMI solar-induced fluorescence (SIF) product to capture global GPP and NPP. First, the GPR algorithms were trained on theoretical simulations through the Soil-Canopy-Observation of Photosynthesis and Energy fluxes (SCOPE) model, with the final retrieval models termed SCOPE-GPR-TCF. Second, the SCOPE-GPR-TCF models were integrated in Google Earth Engine (GEE) and fed with satellite data and products (coming from Sentinel 3 & 5P and ERA5-Land), producing global and regional (Iberian Peninsula) maps at spatial resolutions of 5 km and 300 m during the year 2019. Moderate relative uncertainties in the range between 10%–40% of the GPP and NPP estimates were achieved by the SCOPE-GPR-TCF models. Analysis of the driving variables revealed that the S3-OLCI vegetation products, i.e., leaf area index (LAI), the fraction of absorbed photosynthetically active radiation (FAPAR), and SIF provided the highest prediction strengths. Validation of GPP temporal estimates from GPR against partitioned GPP estimates at 113 flux towers located in America and Europe highlighted a good overall consistency at the local scale, with performances varying depending on the site and vegetation type. The highest scores emerged for stations located in croplands, grasslands, deciduous broad-leaf and evergreen needle-leaf forests with top and values above 0.8 and below 2 respectively. Further, benchmarking spatiotemporal analysis revealed a strong intra-annual global correlation against reference products for the same year 2019: (i) Cross-comparison against LPJ-GUESS resulted in modal values of = 0.8 and = 1.93 for GPP. (ii) MOD17A2H GPP and NPP estimations cross-correlated with modal values of 0.94 and 0.92 and of 1.26 and 1.05 , respectively. We conclude that the hybrid models integrated into the GEE cloud-computing platform facilitate streamlining the global mapping of TCF products at efficient processing costs. This is particularly promising in preparation for the upcoming Fluorescence Explorer (FLEX) mission, where the SCOPE-GPR-TCF models are foreseen to be customized to 300 m resolution FLEX SIF data streams for high-resolution global productivity monitoring.
    Type: info:eu-repo/semantics/article
    Format: application/pdf
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  • 87
    Publication Date: 2024-06-20
    Description: The scientific program of the Meteor M184 expedition was dedicated to studies on the intensity of water mass transformation, a synoptic view of the hydrography in the Labrador Sea and the Irminger Basin, as well as submesoscale resolving surveys of fronts. Measurements of the vertical structure of temperature, salinity, density, oxygen, optical properties, and the flow along selected sections have been surveyed during the M184 expedition. Close to the surface, permanent registrations are carried out with the thermosalinograph (temperature, salinity), meteorological data are continuously collected, flow measurements up to 1000 m depth are performed with the ships installed ADCP and surface currents by a X-band marine radar. Detailed surveys on submesoscale fronts were done with autonomous underwater gliders and ship mounted gear. Furthermore, 40 Hereon drifters were deployed to sample the surface flow. One drifter did not collect any data.
    Keywords: Modular Observation Solutions for Earth Systems; MOSES
    Type: Dataset
    Format: application/zip, 39 datasets
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  • 88
    Publication Date: 2024-06-20
    Description: The data presented herein originates from a mesocosm study conducted as part of the EU H2020 OceanNETs project, aimed at investigating the ecological ramifications of ocean alkalinity enhancement. Nine mesocosms were deployed in Taliarte Harbour, Gran Canaria, Spain, and systematically sampled using integrated water samplers over the period spanning from September 10th to October 25th, 2021. Alkalinity was employed in a gradient design, ranging from ambient (0 µeq kg-1 added alkalinity, OAE0) to elevated levels of 2400 µeq kg-1 additional alkalinity (OAE2400) in increments of 300 µeq kg-1. The dataset encompasses a spectrum of sediment trap particle flux data, water column biogeochemistry variables, including inorganic nutrients, carbonate chemistry parameters, and particulate matter, alongside chlorophyll a concentrations. The study and data set offer insights into impacts of alkalinity enhancement on marine ecosystems and their associated biogeochemistry.
    Keywords: carbon sequestration; export flux; mesocosm study; ocean alkalinity enhancement; Ocean-based Negative Emission Technologies; OceanNETs; particle properties; remineralization rate
    Type: Dataset
    Format: application/zip, 12 datasets
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  • 89
    Publication Date: 2024-06-20
    Description: Ground-based electromagnetic induction (EM) measurements of land-fast sea ice and sub-ice platelet layer (SIPL) thickness distributions were carried out in McMurdo Sound, Antarctica in late spring (November 1-19) of 2018. Repeated west to east EM transects were carried out across McMurdo Sound along latitude 77.767°S. The EM data was acquired using a frequency-domain Geonics Ltd EM31-MK2 instrument mounted on a sledge and towed by skidoo. The thicknesses of consolidated ice (sea ice plus the snow layer) and the sub-ice platelet layer were simultaneously retrieved from the EM31 measured response using forward modelling and inversion methods of Irvin (2018). Variability in EM thicknesses detected significant growth of sub-ice platelet layer over the 18-day survey period (Brett et al., 2024).
    Keywords: Antarctic sea ice; DEEP SOUTH NATIONAL SCIENCE CHALLENGE: Targeted observation and process-informed modelling of Antarctic sea ice; electromagnetic induction; ice-ocean interaction; ice thickness; Sub-ice platelet layer; TOPIMASI
    Type: Dataset
    Format: application/zip, 6 datasets
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  • 90
    Publication Date: 2024-06-20
    Description: This is the measurement data from chemical analysis of archaeological Neolithic pottery using portable X-ray fluorescence analysis (p-XRF). The pottery came from the sites Wanna 1588, 1591, 1592, 1594 and 1603 (district of Cuxhaven, Lower Saxony, Germany) and belongs to the cultural group of the Funnel Beaker culture. The measurements are part of the research projects "Preserved in the bog - relics of prehistoric settlement landscapes in the Elbe-Weser triangle" funded by Niedersachsen Vorab and "Pottery traditions as a mirror of social structures of the 5th and 4th millennium BC in northern Central Europe" funded by the German Research Foundation (DFG project number 438036891). A handheld Niton XL3t XRF-Analyzer of the company analyticon was used. The device was held stationary in a stand. The measurements were taken on the edge of each sherd that have been previously cleaned and smoothed using abrasive paper. Each sherd was analysed in three different areas of the edge using the mode Mining and a small beam of 3 mm. The data consist of the average values of these measurements for each element. Each spot was analysed with four different filters. The total measuring time was 125 seconds.
    Keywords: Archaeological excavation; Archaeological find number; Archaeological site number; archaeology; archaeometry; Calcium; chemical data; Chromium; Excavation_Wanna_1588; Excavation_Wanna_1591; Excavation_Wanna_1592; Excavation_Wanna_1594; Excavation_Wanna_1603; Gallium; Iron; Niobium; Portable X-ray fluorescence analyzer (p-XRF), Niton, XL3t [handheld]; Potassium; Pottery unit; Rubidium; Strontium; Titanium; Vanadium; Wanna, Cuxhaven, Lower Saxony, Germany; Yttrium; Zirconium
    Type: Dataset
    Format: text/tab-separated-values, 330 data points
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  • 91
    Publication Date: 2024-06-20
    Description: This data publication contains maps resulting from spatial prioritisations conducted for the iAtlantic D5.3 report on Systematic Conservation Planning of the wider Atlantic Ocean based on results generated by the iAtlantic project. The maps were produced using the prioritizr R package (Hanson et al. 2023), which identifies priority areas for achieving specific conservation goals while minimising costs. The various prioritisations were developed to address multiple research questions related to: (1) identifying priority areas for conservation and restoration, (2) transboundary conservation, (3) climate-smart conservation planning, and (4) protecting 30% of the Atlantic Ocean, including 10% under strict protection. The results are organised into subfolders based on the research questions addressed and further categorised into data-rich and data-poor regions, along with aggregate results for each region. Further, the results are organised into subfolders representing multiple scenarios executed using various cost layers, including area-based, Global Fishing Watch (GFW, 2023) benthic, GFW total fishing, Global Fisheries Landings (GFL, Watson 2019) v4.0 benthic, and GFL v4.0 total landings. Each map filename provides descriptive information about the executed scenario.
    Keywords: AtlanticOcean; Atlantic Ocean; Binary Object; Binary Object (File Size); Binary Object (MD5 Hash); Binary Object (Media Type); Calculated using prioritizr R package; File content; File name; Horizontal datum; iAtlantic; Integrated Assessment of Atlantic Marine Ecosystems in Space and Time; Latitude, northbound; Latitude, southbound; Longitude, eastbound; Longitude, westbound; SAT; Satellite remote sensing; Spatial prioritisation; Systematic conservation planning
    Type: Dataset
    Format: text/tab-separated-values, 8 data points
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  • 92
    Publication Date: 2024-06-20
    Description: This is the measurement data from chemical analysis of archaeological Neolithic pottery using Inductively Coupled Plasma- Atomic Emission Spectrometry (ICP-AES). The pottery came from the sites Wanna 1588, 1591, 1592 and 1594 (district of Cuxhaven, Lower Saxony, Germany) and belongs to the cultural group of the Funnel Beaker culture. The measurements are part of the research projects "Preserved in the bog - relics of prehistoric settlement landscapes in the Elbe-Weser triangle" funded by Niedersachsen Vorab and "Pottery traditions as a mirror of social structures of the 5th and 4th millennium BC in northern Central Europe" funded by the German Research Foundation (DFG project number 438036891). The measurements were carried out by OMAC Laboratories Ltd. in Loughrea, Galway, Ireland. A minimum of 0.5 g of sample material was taken from each sherd. The sample material was grinded to a fine powder and solved in a 4-acid solution. These solutions were injected into an excited argon plasma.
    Keywords: Aluminium; Archaeological excavation; Archaeological find number; Archaeological site number; Archaeology; archaeometry; Calcium; Cerium; chemical data; Chromium; Cobalt; Excavation_Wanna_1588; Excavation_Wanna_1591; Excavation_Wanna_1592; Excavation_Wanna_1594; Gallium; Inductively coupled plasma atomic emission spectroscope (ICP-AES); Lanthanum; Magnesium; Manganese; Pottery unit; Sodium; Strontium; Vanadium; Wanna, Cuxhaven, Lower Saxony, Germany
    Type: Dataset
    Format: text/tab-separated-values, 195 data points
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  • 93
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    PANGAEA
    In:  Institute of Atmospheric Sciences and Climate of the Italian National Research Council, Bologna
    Publication Date: 2024-06-20
    Keywords: Air temperature at 2 m height; Antarctica; BARO; Barometer; Baseline Surface Radiation Network; BSRN; Concordia Station, Dome C; DATE/TIME; Diffuse radiation; Diffuse radiation, maximum; Diffuse radiation, minimum; Diffuse radiation, standard deviation; DOM; HEIGHT above ground; Long-wave downward radiation; Long-wave downward radiation, maximum; Long-wave downward radiation, minimum; Long-wave downward radiation, standard deviation; Long-wave upward radiation; Long-wave upward radiation, maximum; Long-wave upward radiation, minimum; Long-wave upward radiation, standard deviation; Monitoring station; MONS; Pyranometer, Kipp & Zonen, CM22, SN 050109, WRMC No. 74006; Pyranometer, Kipp & Zonen, CM22, SN 050110, WRMC No. 74001; Pyranometer, Kipp & Zonen, CM22, SN 050111, WRMC No. 74007; Pyrgeometer, Kipp & Zonen, CG4, SN 050366, WRMC No. 74011; Pyrgeometer, Kipp & Zonen, CG4, SN 050768, WRMC No. 74003; Short-wave downward (GLOBAL) radiation; Short-wave downward (GLOBAL) radiation, maximum; Short-wave downward (GLOBAL) radiation, minimum; Short-wave downward (GLOBAL) radiation, standard deviation; Short-wave upward (REFLEX) radiation; Short-wave upward (REFLEX) radiation, maximum; Short-wave upward (REFLEX) radiation, minimum; Short-wave upward (REFLEX) radiation, standard deviation; Station pressure; Thermometer
    Type: Dataset
    Format: text/tab-separated-values, 824192 data points
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  • 94
    Publication Date: 2024-06-20
    Description: The scientific program of the Meteor M184 expedition was dedicated to studies on the intensity of water mass transformation, a synoptic view of the hydrography in the Labrador Sea and the Irminger Basin, as well as submesoscale resolving surveys of fronts. Measurements of the vertical structure of temperature, salinity, density, oxygen, optical properties, and the flow along selected sections have been surveyed during the M184 expedition. Close to the surface, permanent registrations are carried out with the thermosalinograph (temperature, salinity), meteorological data are continuously collected, flow measurements up to 1000 m depth are performed with the ships installed ADCP and surface currents by a X-band marine radar. Detailed surveys on submesoscale fronts were done with autonomous underwater gliders and ship mounted gear. Furthermore, 40 Hereon drifters were deployed to sample the surface flow.
    Keywords: DATE/TIME; DEPTH, water; DRIFT; Drifter; LabSeaVar2022; LATITUDE; LONGITUDE; M184; M184_5-1; Meteor (1986); Modular Observation Solutions for Earth Systems; MOSES; Sample code/label
    Type: Dataset
    Format: text/tab-separated-values, 35916 data points
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  • 95
    Publication Date: 2024-06-20
    Description: The scientific program of the Meteor M184 expedition was dedicated to studies on the intensity of water mass transformation, a synoptic view of the hydrography in the Labrador Sea and the Irminger Basin, as well as submesoscale resolving surveys of fronts. Measurements of the vertical structure of temperature, salinity, density, oxygen, optical properties, and the flow along selected sections have been surveyed during the M184 expedition. Close to the surface, permanent registrations are carried out with the thermosalinograph (temperature, salinity), meteorological data are continuously collected, flow measurements up to 1000 m depth are performed with the ships installed ADCP and surface currents by a X-band marine radar. Detailed surveys on submesoscale fronts were done with autonomous underwater gliders and ship mounted gear. Furthermore, 40 Hereon drifters were deployed to sample the surface flow.
    Keywords: DATE/TIME; DEPTH, water; DRIFT; Drifter; LabSeaVar2022; LATITUDE; LONGITUDE; M184; M184_65-3; Meteor (1986); Modular Observation Solutions for Earth Systems; MOSES; Sample code/label
    Type: Dataset
    Format: text/tab-separated-values, 24481 data points
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  • 96
    Publication Date: 2024-06-20
    Description: The scientific program of the Meteor M184 expedition was dedicated to studies on the intensity of water mass transformation, a synoptic view of the hydrography in the Labrador Sea and the Irminger Basin, as well as submesoscale resolving surveys of fronts. Measurements of the vertical structure of temperature, salinity, density, oxygen, optical properties, and the flow along selected sections have been surveyed during the M184 expedition. Close to the surface, permanent registrations are carried out with the thermosalinograph (temperature, salinity), meteorological data are continuously collected, flow measurements up to 1000 m depth are performed with the ships installed ADCP and surface currents by a X-band marine radar. Detailed surveys on submesoscale fronts were done with autonomous underwater gliders and ship mounted gear. Furthermore, 40 Hereon drifters were deployed to sample the surface flow.
    Keywords: DATE/TIME; DEPTH, water; DRIFT; Drifter; LabSeaVar2022; LATITUDE; LONGITUDE; M184; M184_122-1; Meteor (1986); Modular Observation Solutions for Earth Systems; MOSES; Sample code/label
    Type: Dataset
    Format: text/tab-separated-values, 30849 data points
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  • 97
    Publication Date: 2024-06-20
    Description: The scientific program of the Meteor M184 expedition was dedicated to studies on the intensity of water mass transformation, a synoptic view of the hydrography in the Labrador Sea and the Irminger Basin, as well as submesoscale resolving surveys of fronts. Measurements of the vertical structure of temperature, salinity, density, oxygen, optical properties, and the flow along selected sections have been surveyed during the M184 expedition. Close to the surface, permanent registrations are carried out with the thermosalinograph (temperature, salinity), meteorological data are continuously collected, flow measurements up to 1000 m depth are performed with the ships installed ADCP and surface currents by a X-band marine radar. Detailed surveys on submesoscale fronts were done with autonomous underwater gliders and ship mounted gear. Furthermore, 40 Hereon drifters were deployed to sample the surface flow.
    Keywords: DATE/TIME; DEPTH, water; DRIFT; Drifter; LabSeaVar2022; LATITUDE; LONGITUDE; M184; M184_122-2; Meteor (1986); Modular Observation Solutions for Earth Systems; MOSES; Sample code/label
    Type: Dataset
    Format: text/tab-separated-values, 245 data points
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  • 98
    Publication Date: 2024-06-20
    Description: The scientific program of the Meteor M184 expedition was dedicated to studies on the intensity of water mass transformation, a synoptic view of the hydrography in the Labrador Sea and the Irminger Basin, as well as submesoscale resolving surveys of fronts. Measurements of the vertical structure of temperature, salinity, density, oxygen, optical properties, and the flow along selected sections have been surveyed during the M184 expedition. Close to the surface, permanent registrations are carried out with the thermosalinograph (temperature, salinity), meteorological data are continuously collected, flow measurements up to 1000 m depth are performed with the ships installed ADCP and surface currents by a X-band marine radar. Detailed surveys on submesoscale fronts were done with autonomous underwater gliders and ship mounted gear. Furthermore, 40 Hereon drifters were deployed to sample the surface flow.
    Keywords: DATE/TIME; DEPTH, water; DRIFT; Drifter; LabSeaVar2022; LATITUDE; LONGITUDE; M184; M184_122-3; Meteor (1986); Modular Observation Solutions for Earth Systems; MOSES; Sample code/label
    Type: Dataset
    Format: text/tab-separated-values, 31452 data points
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  • 99
    Publication Date: 2024-06-20
    Description: The scientific program of the Meteor M184 expedition was dedicated to studies on the intensity of water mass transformation, a synoptic view of the hydrography in the Labrador Sea and the Irminger Basin, as well as submesoscale resolving surveys of fronts. Measurements of the vertical structure of temperature, salinity, density, oxygen, optical properties, and the flow along selected sections have been surveyed during the M184 expedition. Close to the surface, permanent registrations are carried out with the thermosalinograph (temperature, salinity), meteorological data are continuously collected, flow measurements up to 1000 m depth are performed with the ships installed ADCP and surface currents by a X-band marine radar. Detailed surveys on submesoscale fronts were done with autonomous underwater gliders and ship mounted gear. Furthermore, 40 Hereon drifters were deployed to sample the surface flow.
    Keywords: DATE/TIME; DEPTH, water; DRIFT; Drifter; LabSeaVar2022; LATITUDE; LONGITUDE; M184; M184_13-2; Meteor (1986); Modular Observation Solutions for Earth Systems; MOSES; Sample code/label
    Type: Dataset
    Format: text/tab-separated-values, 32016 data points
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  • 100
    Publication Date: 2024-06-20
    Description: The scientific program of the Meteor M184 expedition was dedicated to studies on the intensity of water mass transformation, a synoptic view of the hydrography in the Labrador Sea and the Irminger Basin, as well as submesoscale resolving surveys of fronts. Measurements of the vertical structure of temperature, salinity, density, oxygen, optical properties, and the flow along selected sections have been surveyed during the M184 expedition. Close to the surface, permanent registrations are carried out with the thermosalinograph (temperature, salinity), meteorological data are continuously collected, flow measurements up to 1000 m depth are performed with the ships installed ADCP and surface currents by a X-band marine radar. Detailed surveys on submesoscale fronts were done with autonomous underwater gliders and ship mounted gear. Furthermore, 40 Hereon drifters were deployed to sample the surface flow.
    Keywords: DATE/TIME; DEPTH, water; DRIFT; Drifter; LabSeaVar2022; LATITUDE; LONGITUDE; M184; M184_59-3; Meteor (1986); Modular Observation Solutions for Earth Systems; MOSES; Sample code/label
    Type: Dataset
    Format: text/tab-separated-values, 25534 data points
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