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  • 1
    Publication Date: 2021-03-15
    Description: A high-quality hydrographic CTD and Argo float data was used to study the property changes along the westward branch of the Mediterranean Outflow Water (MOW) in the northeast Atlantic between 1981 and 2018. In this period, the temperature and salinity are marked by periods of cooling/freshening and warming/salinification. Since 1981, the MOW properties at the core decreased by −0.015 ± 0.07 °C year−1 and −0.003 ± 0.002 year−1. The different phases of the North Atlantic Oscillation (NAO) influence the main propagation pathways of the MOW into the North Atlantic basin, thus affecting the trends determined within different NAO-phases. The temperature and salinity show a strong correlation with NAO, with NAO leading the properties by 8 and 7 years, respectively, indicating a delayed response of the ocean to different forcing conditions. A decrease in oxygen concentration (−0.426 ± 0.276 μmol kg−1 year−1) was calculated for the same period; however, no connection with the NAO was found.
    Electronic ISSN: 2673-1924
    Topics: Geosciences
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  • 2
    Publication Date: 2024-02-07
    Description: Highlights: • Unique 30-years data of currents and temperature below 1000 m in the Madeira Basin. • Inter-decadal and long term changes were examined between 1000 m and the bottom. • Temperature increase by 0.03 ± 0.01 °C/year (1000 m) and 0.02 ± 0.02 °C/year at 1600 m. • No significant changes at 3000 m and 5000 m at long-term scale. • The currents and kinetic energy increased in the entire water column over 30-years. Abstract: Data from the deep-sea mooring Kiel 276 (33 N, 22W), 5300 m water depth in the northeast Atlantic, was used to investigate the temporal variability of temperature and currents below the main thermocline (1000 m, 1600 m, 3000 m, 5000 m) in the 30-year period (between 1980 and 2009). Daily averages were the basis to assess the temperature and currents changes, as well as kinetic energy, from annual to decadal and long-term scales. Below the main thermocline, no seasonal signal was identified for both, temperature and currents, during the 30 years. The record-length linear temperature trends at 1000 m and 1600 m are 0.03 ± 0.01 °C year−1 and 0.02 ± 0.02 °C year−1, respectively. The mean currents also intensified within the decades in the entire water column, and as a consequence, the mean kinetic energy increased. The fluctuating kinetic energy increased on a decadal scale only at 1000 m, as a possible consequence of the increase in the strength of Mediterranean Water lenses (MEDDIES) that crossed the mooring site. During the period 2001–2009, six MEDDIES crossed the Kiel 276 site, in addition to the 10 MEDDIES identified earlier during the previous 20 years, between 1980 and 2000 (Siedler et al., 2005). The integral time scales are of the same order in all depths (between 30 to 40 days), indicating that events occur on similar time scales, with mesoscale signals dominating and being present within the entire water column.
    Type: Article , PeerReviewed
    Format: text
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  • 3
    Publication Date: 2022-04-04
    Description: The influence of the exceptionally strong typhoon Mangkhut on the availability of nutrients and changes in primary production were studied in the northern South China Sea in September 2018. A tight station grid was sampled to analyze major nutrients, chlorophyll_a, particulate and dissolved organic carbon and nitrogen. Based on interpolated profiles, nutrients and organic matter budgets were determined for the upper 100 m of the water column prior to and after Mangkhut's passage. An upper layer of 100 m was found to reflect the important changes by the typhoon. Considerable differences between the on‐shelf, shelf edge and the deep‐sea stations were determined. Nitrate and phosphate increased by about 80% and 36% on the shelf, respectively, and both by almost 40% at the shelf edge. The open deep‐sea part of the study area reflects some deviating results that may be caused by just displacement of water or by mixing water of different origin. However, right on Mangkhut's track on the shelf even contact between surface waters and bottom waters was enabled, increasing phosphate and silicate, but declining nitrate. The inventory of organic carbon of the upper 100 m of the study area (138,000 km2) of 92 Gmol had increased within a few days after the typhoon's passage by 5 Gmol on the shelf and about 2 Gmol in the shelf edge area. Chlorophyll_a doubled during our stay and might have reached a factor of 3 increase in the subsequent time by nitrate supply and excess phosphate.
    Description: Plain Language Summary: The influence of the super typhoon Mangkhut on the waters of the northern South China Sea was studied in September 2018. Nutrients and organic material were measured on 63 stations from the Chinese research vessel HAI YANG DI ZHI SHI HAO. Amounts of nutrients and biogenic matter were calculated for the on‐shelf, shelf edge and deep‐sea stations for the pre‐ and post‐Mangkhut period. An important finding was that the stations of the different areas, on‐shelf, shelf edge and the deep‐sea appeared to be differently impacted by Mangkhut. Even differences between the stations right on its track and in the other parts of the study area were found. In general, nutrients were supplied in enormous amounts and caused immediate algae growth. Moreover, enough nutrients were supplied to support algae growth for a couple of weeks. In summary, it was found that Manghut's upper water column mixing and shifting caused an almost tripling of primary production compared to the normal situation.
    Description: Key Points: The typhoon Mangkhut clearly impacted the water column differently on the continental shelf, at the shelf edge and in the deep sea. On Mangkhut's track a maximum nitrate supply of 162 mmol m−2 was caused by induced upwelling at the shelf edge. The chlorophyll inventory of 2.8 Gg was almost tripled by contributing 4.7 Gg estimated from an additional nutrient supply.
    Description: Federal Ministry of Education and Research, BMBF http://dx.doi.org/10.13039/501100002347
    Description: National Natural Science Foundation of China http://dx.doi.org/10.13039/501100001809
    Description: https://doi.pangaea.de/10.1594/PANGAEA.936352
    Description: https://doi.pangaea.de/10.1594/PANGAEA.936096
    Keywords: ddc:577.7
    Language: English
    Type: doc-type:article
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  • 4
    Publication Date: 2024-04-17
    Repository Name: EPIC Alfred Wegener Institut
    Type: Article , isiRev
    Format: application/pdf
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  • 5
    Publication Date: 2024-05-08
    Description: This dataset provides 131 CTD profiles measured on board of the German R/V Sonne (cruise SO269) in the northern South China Sea, under the project SOCLIS – South China Sea Natural Laboratory under Climatic and Anthropogenic Stress, in August and September 2019. The 131 profiles of temperature, salinity, dissolved oxygen, fluorescence, turbidity, surface irradiance (SPAR) and Photosynthetically active radiation (PAR), and sound velocity were measured using a CTD Sea-Bird SBE 911 plus, together with oxygen sensor (SBE 43), PAR sensor (Biospherical, QCP-2350 + QSR-2200), and a fluorometer (WET Labs ECO-FLNTU(RT)D). Additionally, oxygen saturation, potential temperature and sigma-theta (with reference to the surface) were calculated. The 131 CTD profiles are distributed by 81 stations and aim to study the impact of a growing anthropogenic pressure around the Pearl River Estuary into the northern shelf of the South China Sea towards the deep sea. The dataset was used to study the presence and spatial distribution of natural and synthetic estrogenic compounds and pharmaceutical and personal care products (PPCPs) in the Pearl River Estuary and northern shelf of the South China Sea.
    Keywords: Calculated; Chlorophyll a; Conductivity; CTD, Sea-Bird SBE 911plus; CTD/Rosette; CTD-RO; DATE/TIME; Density, sigma-theta (0); DEPTH, water; File name; Fluorometer/scattering meter, WET Labs ECO-FLNTU(RT)D; LATITUDE; LONGITUDE; Oxygen, dissolved; Oxygen saturation, per unit volume of the liquid; Oxygen sensor, SBE 43; PAR sensor, Biospherical, QCP-2350 + QSR-2200; physical oceanography; Pressure, water; Radiation, photosynthetically active; Radiation, photosynthetically active, surface; Salinity; SCS19_12; SO269; SO269_180-2-12; SOCLIS; Sonne_2; Sound velocity in water; South China Sea; South China Sea Natural Laboratory under Climatic and Anthropogenic Stress; Station label; Temperature, water; Temperature, water, potential; Turbidity (Nephelometric turbidity unit)
    Type: Dataset
    Format: text/tab-separated-values, 2505 data points
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  • 6
    Publication Date: 2024-05-08
    Description: This dataset provides 131 CTD profiles measured on board of the German R/V Sonne (cruise SO269) in the northern South China Sea, under the project SOCLIS – South China Sea Natural Laboratory under Climatic and Anthropogenic Stress, in August and September 2019. The 131 profiles of temperature, salinity, dissolved oxygen, fluorescence, turbidity, surface irradiance (SPAR) and Photosynthetically active radiation (PAR), and sound velocity were measured using a CTD Sea-Bird SBE 911 plus, together with oxygen sensor (SBE 43), PAR sensor (Biospherical, QCP-2350 + QSR-2200), and a fluorometer (WET Labs ECO-FLNTU(RT)D). Additionally, oxygen saturation, potential temperature and sigma-theta (with reference to the surface) were calculated. The 131 CTD profiles are distributed by 81 stations and aim to study the impact of a growing anthropogenic pressure around the Pearl River Estuary into the northern shelf of the South China Sea towards the deep sea. The dataset was used to study the presence and spatial distribution of natural and synthetic estrogenic compounds and pharmaceutical and personal care products (PPCPs) in the Pearl River Estuary and northern shelf of the South China Sea.
    Keywords: Calculated; Chlorophyll a; Conductivity; CTD, Sea-Bird SBE 911plus; CTD/Rosette; CTD-RO; DATE/TIME; Density, sigma-theta (0); DEPTH, water; File name; Fluorometer/scattering meter, WET Labs ECO-FLNTU(RT)D; LATITUDE; LONGITUDE; Oxygen, dissolved; Oxygen saturation, per unit volume of the liquid; Oxygen sensor, SBE 43; PAR sensor, Biospherical, QCP-2350 + QSR-2200; physical oceanography; Pressure, water; Radiation, photosynthetically active; Radiation, photosynthetically active, surface; Salinity; SCS85; SO269; SO269_121-1; SOCLIS; Sonne_2; Sound velocity in water; South China Sea; South China Sea Natural Laboratory under Climatic and Anthropogenic Stress; Station label; Temperature, water; Temperature, water, potential; Turbidity (Nephelometric turbidity unit)
    Type: Dataset
    Format: text/tab-separated-values, 103036 data points
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  • 7
    Publication Date: 2024-05-08
    Description: This dataset provides 131 CTD profiles measured on board of the German R/V Sonne (cruise SO269) in the northern South China Sea, under the project SOCLIS – South China Sea Natural Laboratory under Climatic and Anthropogenic Stress, in August and September 2019. The 131 profiles of temperature, salinity, dissolved oxygen, fluorescence, turbidity, surface irradiance (SPAR) and Photosynthetically active radiation (PAR), and sound velocity were measured using a CTD Sea-Bird SBE 911 plus, together with oxygen sensor (SBE 43), PAR sensor (Biospherical, QCP-2350 + QSR-2200), and a fluorometer (WET Labs ECO-FLNTU(RT)D). Additionally, oxygen saturation, potential temperature and sigma-theta (with reference to the surface) were calculated. The 131 CTD profiles are distributed by 81 stations and aim to study the impact of a growing anthropogenic pressure around the Pearl River Estuary into the northern shelf of the South China Sea towards the deep sea. The dataset was used to study the presence and spatial distribution of natural and synthetic estrogenic compounds and pharmaceutical and personal care products (PPCPs) in the Pearl River Estuary and northern shelf of the South China Sea.
    Keywords: Calculated; Chlorophyll a; Conductivity; CTD, Sea-Bird SBE 911plus; CTD/Rosette; CTD-RO; DATE/TIME; Density, sigma-theta (0); DEPTH, water; File name; Fluorometer/scattering meter, WET Labs ECO-FLNTU(RT)D; LATITUDE; LONGITUDE; Oxygen, dissolved; Oxygen saturation, per unit volume of the liquid; Oxygen sensor, SBE 43; PAR sensor, Biospherical, QCP-2350 + QSR-2200; physical oceanography; Pressure, water; Radiation, photosynthetically active; Radiation, photosynthetically active, surface; Salinity; SCS88; SO269; SO269_178-1; SOCLIS; Sonne_2; Sound velocity in water; South China Sea; South China Sea Natural Laboratory under Climatic and Anthropogenic Stress; Station label; Temperature, water; Temperature, water, potential; Turbidity (Nephelometric turbidity unit)
    Type: Dataset
    Format: text/tab-separated-values, 2610 data points
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  • 8
    Publication Date: 2024-05-15
    Description: Current velocities of the upper water column along the cruise track of R/V Sonne cruise SO296/1 were collected by a vessel-mounted 75 kHz RDI Ocean Surveyor ADCP. The ADCP transducer was located at 6.0 m below the water line. The instrument was operated in narrowband mode (WM10) with a bin size of 8.00 m, a blanking distance of 8.00 m, and a total of 100 bins, covering the depth range between 22.0 m and 814.0 m. Heading, pitch and roll data from the ship's motion reference unit and the navigation data from the Global Positioning systems were used by the data acquisition software VmDAS internally to convert ADCP velocities into earth coordinates. Single-ping data were screened for bottom signals and, where appropriate, a bottom mask was manually processed. The ship's velocity was calculated from position fixes obtained by the Global Positioning System (GPS). Accuracy of the ADCP velocities mainly depends on the quality of the position fixes and the ship's heading data. Further errors stem from a misalignment of the transducer with the ship's centerline. Data post-processing included water track calibration of the misalignment angle (-0.1252° +/- 0.4024°) and scale factor (1.0042 +/- 0.0075) of the Ocean Surveyor signal. The velocity data were averaged in time using an average interval of 60 s. Velocity quality flagging is based on different threshold criteria: Depth cells with ensemble-averaged percent-good values below 25% are marked as 'bad data'. Depth cells with velocities above 1.5 m/s are flagged as 'bad data'. Depth cells with a root-mean-square deviation between the measured ensemble-average velocity and a cell-wise running-mean velocity above 0.3 m/s are flagged as 'probably bad data'.
    Keywords: Current velocity, east-west; Current velocity, north-south; DAM_Underway; DAM Underway Research Data; DATE/TIME; DEPTH, water; Echo intensity, relative; LATITUDE; LONGITUDE; MAPUCHE; Pings, averaged to a double ensemble value; Quality flag, current velocity; Seadatanet flag: Data quality control procedures according to SeaDataNet (2010); SO296/1; SO296/1_0_Underway-4; Sonne_2; Vessel mounted Acoustic Doppler Current Profiler [75 kHz]; VMADCP-75
    Type: Dataset
    Format: text/tab-separated-values, 11235790 data points
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  • 9
    Publication Date: 2024-06-12
    Description: During the cruise SO269 (August/September 2019) on board of the German RV SONNE, we collected water with a CTD SBE911 rosette system at 81 stations (resulting in more than 600 water samples) distributed along the shelf, shelf edge and deep-sea of the northern South China Sea. We measured concentrations of chlorophyll a, phaeopigments, suspended particulate material (SPM) and nutrients as nitrate, nitrite, phosphate and silicate. Also, we determined concentrations of particulate organic carbon (POC) and particulate organic nitrogen (PON) as well as dissolved organic carbon (DOC) and dissolved organic nitrogen (DON). The hydrographic data collected during this survey is available at PANGAEA (Waniek et al. 2021). Brief description of the methodology used: Nitrate, nitrite, phosphate and silicate were measured by continuous flow analysis. DOC and DON were measured by catalytic oxidation after filtration through GF/F-filter. POC and PON were measured by means of an elemental analyser after filtration through pre-combusted GF/F-filters. SPM was determined gravimetrically after by determining the difference between empty pre-combusted and loaded (sample filtrate) weighted GF/F-filter. Chlorophyll a and phaeopigments were measured using a fluorometer after ethanol extraction of the GF/F-filters.
    Keywords: biogeochemistry; Carbon, organic, dissolved; Carbon, organic, particulate; catalytic oxidation (GF/F-filtered) (Grasshoff et al., 1999); Chlorophyll a; CTD, Sea-Bird SBE 911plus; CTD/Rosette; CTD-RO; DATE/TIME; Depth, bottom/max; DEPTH, water; elemental analyzer (GF/F- filtered) (Grasshoff et al., 1999); Event label; File name; fluorometer (ethanol extraction; GF/F-filtered) (Grasshoff et al., 1999); gravimetrically (GF/F-filtered) (Grasshoff et al., 1999); LATITUDE; LONGITUDE; Nitrate; Nitrite; Nitrogen, organic, dissolved; Nitrogen, organic, particulate; nutrients; Phaeopigments; Phosphate; PUMP; Salinity; SCS01; SCS02; SCS03; SCS04; SCS05; SCS06; SCS07; SCS08; SCS09; SCS10; SCS11; SCS12; SCS13; SCS14; SCS15; SCS16; SCS17; SCS18; SCS19; SCS19_02; SCS19_04; SCS19_06; SCS19_08; SCS19_10; SCS19_12; SCS19_14; SCS19_16; SCS19_17; SCS20; SCS21; SCS22; SCS23; SCS24; SCS25; SCS26; SCS27; SCS28; SCS29; SCS30; SCS31; SCS32; SCS33; SCS34; SCS35; SCS36; SCS37; SCS38; SCS39; SCS40; SCS41; SCS41_2; SCS42; SCS43; SCS44; SCS45; SCS46; SCS47; SCS48; SCS49; SCS50; SCS51; SCS52; SCS53; SCS54; SCS55; SCS56; SCS57; SCS58_01; SCS58_03; SCS58_05; SCS58_07; SCS58_09; SCS58_11; SCS58_13; SCS58_15; SCS58_17; SCS58_19; SCS58_21; SCS58_23; SCS58_25; SCS58_27; SCS59; SCS60; SCS61; SCS62; SCS63; SCS64; SCS64_1; SCS65; SCS66; SCS67; SCS68; SCS69; SCS70; SCS72; SCS80; SCS81; SCS82; SCS83; SCS85; Silicate; SO269; SO269_101-1; SO269_103-1; SO269_105-1; SO269_107-1; SO269_107-4; SO269_109-1; SO269_1-1; SO269_11-1; SO269_111-1; SO269_113-1; SO269_115-1; SO269_117-1; SO269_121-1; SO269_123-1; SO269_125-1; SO269_127-1; SO269_129-1; SO269_13-1; SO269_133-1; SO269_137-1; SO269_15-1; SO269_153-1; SO269_153-4; SO269_153-6; SO269_154-1; SO269_155-1; SO269_156-1; SO269_157-1; SO269_158-1; SO269_163-1; SO269_163-4-10; SO269_163-4-12; SO269_163-4-14; SO269_163-4-16; SO269_163-4-18; SO269_163-4-2; SO269_163-4-20; SO269_163-4-22; SO269_163-4-24; SO269_163-4-26; SO269_163-4-4; SO269_163-4-6; SO269_163-4-8; SO269_166-1; SO269_168-1; SO269_169-1; SO269_170-1; SO269_17-1; SO269_171-1; SO269_172-1; SO269_180-1; SO269_180-2-10; SO269_180-2-12; SO269_180-2-14; SO269_180-2-16; SO269_180-2-17; SO269_180-2-2; SO269_180-2-4; SO269_180-2-6; SO269_180-2-8; SO269_19-1; SO269_21-1; SO269_23-1; SO269_25-1; SO269_27-1; SO269_29-1; SO269_3-1; SO269_31-1; SO269_33-1; SO269_35-1; SO269_37-1; SO269_39-1; SO269_41-1; SO269_43-1; SO269_45-1; SO269_47-1; SO269_49-1; SO269_49-2; SO269_5-1; SO269_51-1; SO269_53-1; SO269_55-1; SO269_57-1; SO269_59-1; SO269_61-1; SO269_62-1; SO269_63-1-1; SO269_63-1-2; SO269_65-1; SO269_67-1; SO269_69-1; SO269_7-1; SO269_71-1; SO269_73-1; SO269_75-1; SO269_77-1; SO269_81-1; SO269_83-1; SO269_87-1; SO269_89-1; SO269_9-1; SO269_91-1; SO269_93-1; SO269_95-1; SO269_99-1; SOCLIS; Sonne_2; South China Sea; South China Sea Natural Laboratory under Climatic and Anthropogenic Stress; Station label; Suspended particulate matter; Temperature, water; Water pump; wet chemical treatment; Continuous flow analysis (Grasshoff et al., 1999)
    Type: Dataset
    Format: text/tab-separated-values, 9312 data points
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  • 10
    Publication Date: 2024-06-12
    Description: During the cruise POS459 on board the German R/V Poseidon, we collected water with a CTD SBE 11plus equipped with 14 Hydrobios free flow bottles of 10 L each in 9 stations (resulting in almost 100 samples) in the Madeira basin region, Northeast Atlantic. We aimed to study the physical and biogeochemical conditions of the water column along the 22°W meridian, north and south of the Azores Front, in September 2013. We measured concentrations of chlorophyll a, phaeopigments, suspended particulate material (SPM), and nutrients such as nitrate, nitrite, phosphate and silicate. Also, we determined concentrations of particulate organic carbon (POC) and particulate organic nitrogen (PON). The physical oceanography associated with this dataset can be found at https://doi.org/10.1594/PANGAEA.949122. Brief description of the methodology used: - Nitrate, nitrite, phosphate, and silicate were measured by continuous flow analysis. - POC and PON were measured by means of an elemental analyser after filtered with pre-combusted GF/F-filters. - Suspended particulate material (SPM) was determined gravimetrically after pre-combusted and weighted GF/F-filters filtration. - Chlorophyll a and phaeopigments were measured using a fluorometer after ethanol extraction of the GF/F-filters.
    Keywords: Azores Front; biogeochemistry; Carbon, organic, particulate; Chlorophyll a; CTD/Rosette; CTD-RO; DATE/TIME; DEPTH, water; elemental analyzer (GF/F- filtered) (Grasshoff et al., 1999); ELEVATION; Event label; File name; fluorometer (ethanol extraction; GF/F-filtered) (Grasshoff et al., 1999); gravimetrically (GF/F-filtered) (Grasshoff et al., 1999); LATITUDE; LONGITUDE; Nitrate; Nitrite; Nitrogen, organic, particulate; Northeast Atlantic; Phaeopigments; Phosphate; POS459; POS459_0996-1; POS459_0997-1; POS459_0999-1; POS459_1002-1; POS459_1003-1; POS459_1004-1; POS459_1006-1; POS459_1007-1; POS459_1008-2; Poseidon; Salinity; Silicate; Suspended particulate matter; Temperature, water; Water volume, filtered; wet chemical treatment; Continuous flow analysis (Grasshoff et al., 1999)
    Type: Dataset
    Format: text/tab-separated-values, 971 data points
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