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  • 2020-2024  (15,692)
  • 1990-1994  (15)
  • 2020  (15,692)
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  • 1
    Publication Date: 2024-06-14
    Description: The shallow meridional overturning cells of the Atlantic Ocean, the Subtropical Cells (STCs), consist of poleward Ekman transport at the surface, subduction in the subtropics, equatorward flow at thermocline level and upwelling along the equator and at the eastern boundary. In this study we provide the first observational estimate of transport variability associated with the horizontal branches of the Atlantic STCs in both hemispheres based on Argo float data and supplemented by reanalysis products. Thermocline layer transport convergence and surface layer transport divergence between 10°N and 10°S are dominated by seasonal variability. Meridional thermocline layer transport anomalies at the western boundary and in the interior basin are anti-correlated and partially compensate each other at all resolved time scales. It is suggested that the seesaw-like relation is forced by the large-scale off-equatorial wind stress changes through low-baroclinic-mode Rossby wave adjustment. We further show that anomalies of the thermocline layer interior transport convergence modulate sea surface temperature (SST) variability in the upwelling regions along the equator and at the eastern boundary at time scales longer than 5 years. Phases of weaker (stronger) interior transport are associated with phases of higher (lower) equatorial SST. At these time scales, STC transport variability is forced by off-equatorial wind stress changes, especially by those in the southern hemisphere. At shorter time scales, equatorial SST anomalies are, instead, mainly forced by local changes of zonal wind stress.
    Keywords: BANINO; Benguela Niños: Physikalische Prozesse und langperiodische Variabilität; Climate - Biogeochemistry Interactions in the Tropical Ocean; RACE; Regional Atlantic Circulation and global Change; SFB754; TRIATLAS; Tropical and South Atlantic climate-based marine ecosystem predictions for sustainable management
    Type: Dataset
    Format: 16 datasets
    Location Call Number Expected Availability
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  • 2
    Publication Date: 2024-06-14
    Description: Carbon export (from the epipelagic towards the mesopelagic zone) and sequestration (from the mesopelagic towards the bathypelagic zone) in the ocean are reviewed. Particulate organic carbon (POC) flux, and active flux due to migrant zooplankton and micronekton are shown from the epipelagic to the mesopelagic zone, and from the latter to the bathypelagic zone. Values towards the meso- and bathypelagic zones are compared in oligotrophic and productive systems. Zooplankton and prokaryote respiration in the meso- and bathypelagic zones of the ocean are also reviewed for oligotrophic and productive systems. Values were integrated over a depth layer and are given as the flux or respiration under one square meter (in g/m**2/a) between e.g. 100 m and 1000 m depth.
    Keywords: 29HE20101215; 29HE20110117; 29HE20110211; 29HE20110317; 29HE20110416; 29HE20110513; 29HE20110619; bathypelagic; Date/Time of event; DEPTH, water; epipelagic; Event label; Hespérides; Image analysis; Latitude of event; Longitude of event; MALASPINA_LEG1; MALASPINA_LEG1_005-1; MALASPINA_LEG1_007-1; MALASPINA_LEG1_010-1; MALASPINA_LEG1_012-1; MALASPINA_LEG1_013-1; MALASPINA_LEG1_015-1; MALASPINA_LEG1_017-1; MALASPINA_LEG1_019-1; MALASPINA_LEG1_022-1; MALASPINA_LEG1_024-1; MALASPINA_LEG2; MALASPINA_LEG2_027-1; MALASPINA_LEG2_029-1; MALASPINA_LEG2_031-1; MALASPINA_LEG2_033-1; MALASPINA_LEG2_037-1; MALASPINA_LEG2_039-1; MALASPINA_LEG2_041-1; MALASPINA_LEG3; MALASPINA_LEG3_045-1; MALASPINA_LEG3_047-1; MALASPINA_LEG3_049-1; MALASPINA_LEG3_055-1; MALASPINA_LEG3_058-1; MALASPINA_LEG3_062-1; MALASPINA_LEG3_064-1; MALASPINA_LEG3_066-1; MALASPINA_LEG4; MALASPINA_LEG4_069-1; MALASPINA_LEG4_071-1; MALASPINA_LEG4_076-1; MALASPINA_LEG4_077-1; MALASPINA_LEG5; MALASPINA_LEG5_084-1; MALASPINA_LEG5_086-1; MALASPINA_LEG5_088-1; MALASPINA_LEG5_090-1; MALASPINA_LEG5_092-1; MALASPINA_LEG5_096-1; MALASPINA_LEG5_100-1; MALASPINA_LEG6; MALASPINA_LEG6_101-1; MALASPINA_LEG6_103-1; MALASPINA_LEG6_106-1; MALASPINA_LEG6_112-1; MALASPINA_LEG6_114-1; MALASPINA_LEG6_115-1; MALASPINA_LEG6_117-1; MALASPINA_LEG6_119-1; MALASPINA_LEG6_121-1; MALASPINA_LEG6_126-1; MALASPINA_LEG7; MALASPINA_LEG7_131-1; MALASPINA_LEG7_135-1; MALASPINA_LEG7_140-1; MALASPINA_LEG7_142-1; MALASPINA_LEG7_146-1; MALASPINA-2010; Malaspina circumnavigation expedition; Malaspina cruise; mesopelagic; MH007_005; MH009_007; MH012_010; MH014_012; MH015_013; MH017_015; MH019_017; MH021_019; MH024_022; MH026_024; MH036_027; MH038_029; MH040_031; MH042_033; MH046_037; MH048_039; MH050_041; MH061_045; MH063_047; MH065_049; MH075_055; MH078_058; MH082_062; MH086_066; MH095_069; MH097_071; MH102_076; MH103_077; MH128_084; MH130_086; MH132_088; MH134_090; MH136_092; MH140_096; MH144_100; MH150_101; MH152_103; MH155_106; MH161_112; MH163_114; MH164_115; MH166_117; MH168_119; MH170_121; MH175_126; MH193_131; MH197_135; MH202_140; MH204_142; MH208_146; MSN300; Multiple opening/closing net, 300 µm meshsize; Norther Equatorial Pacific Ocean; Northern Equatorial Pacific Ocean; Optional event label; Southern Indian Ocean; Southern Pacific Ocean; Southern Subtropical Indian Ocean; Southern Subtropical Pacific Ocean; Southern Tropical Pacific Ocean; South Indian Ocean; Subtropical North Atlantic; SUMMER; Sustainable Management of Mesopelagic Resources; TRIATLAS; Tropical and South Atlantic climate-based marine ecosystem predictions for sustainable management; Zooplankton, biomass as carbon; Zooplankton biomass
    Type: Dataset
    Format: text/tab-separated-values, 124 data points
    Location Call Number Expected Availability
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  • 3
    Publication Date: 2024-06-14
    Description: Carbon export (from the epipelagic towards the mesopelagic zone) and sequestration (from the mesopelagic towards the bathypelagic zone) in the ocean are reviewed. Particulate organic carbon (POC) flux, and active flux due to migrant zooplankton and micronekton are shown from the epipelagic to the mesopelagic zone, and from the latter to the bathypelagic zone. Values towards the meso- and bathypelagic zones are compared in oligotrophic and productive systems. Zooplankton and prokaryote respiration in the meso- and bathypelagic zones of the ocean are also reviewed for oligotrophic and productive systems. Values were integrated over a depth layer and are given as the flux or respiration under one square meter (in g/m**2/a) between e.g. 100 m and 1000 m depth.
    Keywords: active flux; biological carbon pump; Calculated, integrated over layer depth; Carbon, flux; Carbon, flux per year; Comment; Deep sea; Depth, description; DEPTH, water; MALASPINA-2010; Malaspina circumnavigation expedition; Ocean; Organisms; Parameter; passive flux; Reference/source; Respiration; Respiration rate, carbon; SUMMER; Sustainable Management of Mesopelagic Resources; TRIATLAS; Tropical and South Atlantic climate-based marine ecosystem predictions for sustainable management; Uniform resource locator/link to reference
    Type: Dataset
    Format: text/tab-separated-values, 902 data points
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  • 4
    Publication Date: 2024-06-14
    Description: Long-term predictability of the North Atlantic sea surface temperature (SST) is commonly attributed to buoyancy-forced changes of the Atlantic Meridional Overturning Circulation. Here we investigate the role of surface wind stress forcing in decadal hindcasts as another source of extratropical North Atlantic SST predictability. For this purpose, a global climate model is forced by reanalysis (ERA-interim) wind stress anomalies over the period 1979-2017. The simulated climate states serve as initial conditions for decadal hindcasts. Significant skill in predicting detrended observed annual SST anomalies is observed over the extratropical central North Atlantic with anomaly correlation coefficients exceeding 0.6 at lead times of 4 to 7 years. The skill is insensitive to the calendar month of initialization and linked to upper-ocean heat content anomalies that lead anomalous SSTs by several years.
    Keywords: Binary Object; Binary Object (File Size); Binary Object (Media Type); Description
    Type: Dataset
    Format: text/tab-separated-values, 36 data points
    Location Call Number Expected Availability
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  • 5
    Publication Date: 2024-06-14
    Description: Carbon export (from the epipelagic towards the mesopelagic zone) and sequestration (from the mesopelagic towards the bathypelagic zone) in the ocean are reviewed. Particulate organic carbon (POC) flux, and active flux due to migrant zooplankton and micronekton are shown from the epipelagic to the mesopelagic zone, and from the latter to the bathypelagic zone. Values towards the meso- and bathypelagic zones are compared in oligotrophic and productive systems. Zooplankton and prokaryote respiration in the meso- and bathypelagic zones of the ocean are also reviewed for oligotrophic and productive systems. Values were integrated over a depth layer and are given as the flux or respiration under one square meter (in g/m**2/a) between e.g. 100 m and 1000 m depth.
    Keywords: 29HE20101215; 29HE20110117; 29HE20110211; 29HE20110317; 29HE20110416; 29HE20110513; bathypelagic; Carbon/Nitrogen ratio; DATE/TIME; DEPTH, water; epipelagic; Event label; Hespérides; Latitude of event; Longitude of event; MALASPINA_LEG1; MALASPINA_LEG1_005-1; MALASPINA_LEG1_010-1; MALASPINA_LEG1_013-1; MALASPINA_LEG1_015-1; MALASPINA_LEG1_017-1; MALASPINA_LEG2; MALASPINA_LEG2_035-1; MALASPINA_LEG2_043-1; MALASPINA_LEG3; MALASPINA_LEG3_045-1; MALASPINA_LEG3_049-1; MALASPINA_LEG3_064-1; MALASPINA_LEG3_066-1; MALASPINA_LEG4; MALASPINA_LEG4_069-1; MALASPINA_LEG4_071-1; MALASPINA_LEG4_076-1; MALASPINA_LEG4_077-1; MALASPINA_LEG5; MALASPINA_LEG5_084-1; MALASPINA_LEG5_086-1; MALASPINA_LEG5_092-1; MALASPINA_LEG5_096-1; MALASPINA_LEG5_100-1; MALASPINA_LEG6; MALASPINA_LEG6_103-1; MALASPINA_LEG6_117-1; MALASPINA_LEG6_119-1; MALASPINA-2010; Malaspina circumnavigation expedition; mesopelagic; MH007_005; MH012_010; MH015_013; MH017_015; MH019_017; MH044_035; MH052_043; MH061_045; MH065_049; MH086_066; MH095_069; MH097_071; MH102_076; MH103_077; MH128_084; MH130_086; MH136_092; MH140_096; MH144_100; MH152_103; MH166_117; MH168_119; MSN300; Multiple opening/closing net, 300 µm meshsize; Norther Equatorial Pacific Ocean; Northern Equatorial Pacific Ocean; Observation; ocean; Optional event label; South Atlantic; Southern Indian Ocean; Southern Pacific Ocean; Southern Subtropical Indian Ocean; Southern Subtropical Pacific Ocean; Southern Tropical Pacific Ocean; South Indian Ocean; Stable isotopes; Subtropical North Atlantic; Subtropical South Atlantic; SUMMER; Sustainable Management of Mesopelagic Resources; Taxon/taxa; TRIATLAS; Tropical and South Atlantic climate-based marine ecosystem predictions for sustainable management; Zooplankton; δ13C; δ15N
    Type: Dataset
    Format: text/tab-separated-values, 855 data points
    Location Call Number Expected Availability
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  • 6
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    PANGAEA
    In:  Izaña Atmospheric Research Center, Meteorological State Agency of Spain
    Publication Date: 2024-06-14
    Keywords: Air temperature at 2 m height; BARO; Barometer; Baseline Surface Radiation Network; BSRN; DATE/TIME; Diffuse radiation; Diffuse radiation, maximum; Diffuse radiation, minimum; Diffuse radiation, standard deviation; Direct radiation; Direct radiation, maximum; Direct radiation, minimum; Direct radiation, standard deviation; EKO Instruments, MR-60, SN S15115.07, WRMC No. 61013; HEIGHT above ground; Humidity, relative; HYGRO; Hygrometer; IZA; Izaña; 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; Net radiation; Net radiation, maximum; Net radiation, minimum; Net radiation, standard deviation; Pyranometer, EKO, MS-802F, SN F15508FR, WRMC No. 61010; Pyranometer, EKO, MS-802F, SN F15509FR, WRMC No. 61011; Pyrgeometer, Kipp & Zonen, CGR4, SN 050783, WRMC No. 61008; Pyrheliometer, Kipp & Zonen, CH1, SN 080050, WRMC No. 61003; 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; Tenerife, Spain; Thermometer
    Type: Dataset
    Format: text/tab-separated-values, 1307245 data points
    Location Call Number Expected Availability
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  • 7
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    PANGAEA
    In:  Izaña Atmospheric Research Center, Meteorological State Agency of Spain
    Publication Date: 2024-06-14
    Keywords: Air temperature at 2 m height; BARO; Barometer; Baseline Surface Radiation Network; BSRN; DATE/TIME; Diffuse radiation; Diffuse radiation, maximum; Diffuse radiation, minimum; Diffuse radiation, standard deviation; Direct radiation; Direct radiation, maximum; Direct radiation, minimum; Direct radiation, standard deviation; EKO Instruments, MR-60, SN S15115.07, WRMC No. 61013; HEIGHT above ground; Humidity, relative; HYGRO; Hygrometer; IZA; Izaña; 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; Net radiation; Net radiation, maximum; Net radiation, minimum; Net radiation, standard deviation; Pyranometer, EKO, MS-802F, SN F15508FR, WRMC No. 61010; Pyranometer, EKO, MS-802F, SN F15509FR, WRMC No. 61011; Pyrgeometer, Kipp & Zonen, CGR4, SN 050783, WRMC No. 61008; Pyrheliometer, Kipp & Zonen, CH1, SN 080050, WRMC No. 61003; 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; Tenerife, Spain; Thermometer
    Type: Dataset
    Format: text/tab-separated-values, 1301468 data points
    Location Call Number Expected Availability
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  • 8
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    PANGAEA
    In:  Izaña Atmospheric Research Center, Meteorological State Agency of Spain
    Publication Date: 2024-06-14
    Keywords: Air temperature at 2 m height; BARO; Barometer; Baseline Surface Radiation Network; BSRN; DATE/TIME; Diffuse radiation; Diffuse radiation, maximum; Diffuse radiation, minimum; Diffuse radiation, standard deviation; Direct radiation; Direct radiation, maximum; Direct radiation, minimum; Direct radiation, standard deviation; EKO Instruments, MR-60, SN S15115.07, WRMC No. 61013; HEIGHT above ground; Humidity, relative; HYGRO; Hygrometer; IZA; Izaña; 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; Net radiation; Net radiation, maximum; Net radiation, minimum; Net radiation, standard deviation; Pyranometer, EKO, MS-802F, SN F15508FR, WRMC No. 61010; Pyranometer, EKO, MS-802F, SN F15509FR, WRMC No. 61011; Pyrgeometer, Kipp & Zonen, CGR4, SN 050783, WRMC No. 61008; Pyrheliometer, Kipp & Zonen, CH1, SN 080050, WRMC No. 61003; 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; Tenerife, Spain; Thermometer
    Type: Dataset
    Format: text/tab-separated-values, 1259971 data points
    Location Call Number Expected Availability
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  • 9
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    PANGAEA
    In:  Izaña Atmospheric Research Center, Meteorological State Agency of Spain
    Publication Date: 2024-06-14
    Keywords: Air temperature at 2 m height; BARO; Barometer; Baseline Surface Radiation Network; BSRN; DATE/TIME; Diffuse radiation; Diffuse radiation, maximum; Diffuse radiation, minimum; Diffuse radiation, standard deviation; Direct radiation; Direct radiation, maximum; Direct radiation, minimum; Direct radiation, standard deviation; EKO Instruments, MR-60, SN S15115.07, WRMC No. 61013; HEIGHT above ground; Humidity, relative; HYGRO; Hygrometer; IZA; Izaña; 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; Net radiation; Net radiation, maximum; Net radiation, minimum; Net radiation, standard deviation; Pyranometer, EKO, MS-802F, SN F15508FR, WRMC No. 61010; Pyranometer, EKO, MS-802F, SN F15509FR, WRMC No. 61011; Pyrgeometer, Kipp & Zonen, CGR4, SN 050783, WRMC No. 61008; Pyrheliometer, EKO, MS-56, SN P15048, WRMC No. 61012; 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; Tenerife, Spain; Thermometer
    Type: Dataset
    Format: text/tab-separated-values, 1232604 data points
    Location Call Number Expected Availability
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  • 10
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    PANGAEA
    In:  Meteorology Climatology Remote Sensing, Dep. Umweltwissenschaften, Universität Basel
    Publication Date: 2024-06-14
    Description: In Gobabeb, Namibia SWD, LWD and DIR are each measured redundant with two instruments of the same make (not in this data base). The differences between the pairs are used in the quality control. This is done manually by inspecting plots of half-day diurnal courses of the pairs and their differences. Values are removed mostly in the morning due to daily cleaning. Other reasons for larger differences are birds, insects, or people at the station. There are regular fog events varying in frequency over the year. Usually, the fog appears in the second half of the night and disappears a few hours after sunrise. The case temperatures of pyrgeometers practically never drop below dewpoint but there can be water deposition of the dome.
    Keywords: Air temperature at 2 m height; BARO; Barometer; Baseline Surface Radiation Network; BSRN; DATE/TIME; Diffuse radiation; Diffuse radiation, standard deviation; Direct radiation; Direct radiation, standard deviation; GOB; Gobabeb; HEIGHT above ground; Humidity, relative; HYGRO; Hygrometer; Long-wave downward radiation; Long-wave downward radiation, standard deviation; Long-wave upward radiation; Monitoring station; MONS; Namib Desert, Namibia; Pyranometer, Kipp & Zonen, CMP22, SN 110315, WRMC No. 20100; Pyranometer, Kipp & Zonen, CMP22, SN 110316, WRMC No. 20101; Pyranometer, Kipp & Zonen, CMP22, SN 120330, WRMC No. 20102; Pyrgeometer, Kipp & Zonen, CGR4, SN 110408, WRMC No. 20200; Pyrgeometer, Kipp & Zonen, CGR4, SN 120457, WRMC No. 20201; Pyrheliometer, Kipp & Zonen, CHP 1, SN 110764, WRMC No. 20000; Short-wave downward (GLOBAL) radiation; Short-wave downward (GLOBAL) radiation, standard deviation; Short-wave upward (REFLEX) radiation; Station pressure; Thermometer
    Type: Dataset
    Format: text/tab-separated-values, 579516 data points
    Location Call Number Expected Availability
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  • 11
    Publication Date: 2024-06-14
    Keywords: 29HE20101215; Acoustic Doppler Current Profiling (LADCP) [lowered with CTD]; Backscatter; Date/time start; DEPTH, water; Echo backscatter; Event label; Global positioning system; GPS; Hespérides; LADCP; LATITUDE; LONGITUDE; MALASPINA_LEG1; MALASPINA_LEG1_012-4; MALASPINA_LEG1_013-4; MALASPINA_LEG1_014-4; MALASPINA_LEG1_015-4; MALASPINA_LEG1_016-4; MALASPINA_LEG1_017-4; MALASPINA_LEG1_018-4; MALASPINA_LEG1_019-4; MALASPINA_LEG1_020-4; MALASPINA_LEG1_021-4; MALASPINA_LEG1_022-4; MALASPINA_LEG1_023-4; MALASPINA_LEG1_024-4; MALASPINA_LEG1_025-4; MALASPINA_LEG1_026-4; MALASPINA-2010; Malaspina circumnavigation expedition; Malaspina Expedition; MH014_012; MH015_013; MH016_014; MH017_015; MH018_016; MH019_017; MH020_018; MH021_019; MH022_020; MH023_021; MH024_022; MH025_023; MH026_024; MH027_025; MH028_026; Station label; SUMMER; Sustainable Management of Mesopelagic Resources; TRIATLAS; Tropical and South Atlantic climate-based marine ecosystem predictions for sustainable management
    Type: Dataset
    Format: text/tab-separated-values, 17331 data points
    Location Call Number Expected Availability
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  • 12
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    Unknown
    PANGAEA
    In:  Meteorology Climatology Remote Sensing, Dep. Umweltwissenschaften, Universität Basel
    Publication Date: 2024-06-14
    Description: In Gobabeb, Namibia SWD, LWD and DIR are each measured redundant with two instruments of the same make (not in this data base). The differences between the pairs are used in the quality control. This is done manually by inspecting plots of half-day diurnal courses of the pairs and their differences. Values are removed mostly in the morning due to daily cleaning. Other reasons for larger differences are birds, insects, or people at the station. There are regular fog events varying in frequency over the year. Usually, the fog appears in the second half of the night and disappears a few hours after sunrise. The case temperatures of pyrgeometers practically never drop below dewpoint but there can be water deposition of the dome.
    Keywords: Air temperature at 2 m height; BARO; Barometer; Baseline Surface Radiation Network; BSRN; DATE/TIME; Diffuse radiation; Diffuse radiation, standard deviation; Direct radiation; Direct radiation, standard deviation; GOB; Gobabeb; HEIGHT above ground; Humidity, relative; HYGRO; Hygrometer; Long-wave downward radiation; Long-wave downward radiation, standard deviation; Long-wave upward radiation; Monitoring station; MONS; Namib Desert, Namibia; Pyranometer, Kipp & Zonen, CMP22, SN 110315, WRMC No. 20100; Pyranometer, Kipp & Zonen, CMP22, SN 110316, WRMC No. 20101; Pyranometer, Kipp & Zonen, CMP22, SN 120330, WRMC No. 20102; Pyrgeometer, Kipp & Zonen, CGR4, SN 110408, WRMC No. 20200; Pyrgeometer, Kipp & Zonen, CGR4, SN 120457, WRMC No. 20201; Pyrheliometer, Kipp & Zonen, CHP 1, SN 110764, WRMC No. 20000; Short-wave downward (GLOBAL) radiation; Short-wave downward (GLOBAL) radiation, standard deviation; Short-wave upward (REFLEX) radiation; Station pressure; Thermometer
    Type: Dataset
    Format: text/tab-separated-values, 561382 data points
    Location Call Number Expected Availability
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  • 13
    Publication Date: 2024-06-14
    Keywords: 29HE20110211; Acoustic Doppler Current Profiling (LADCP) [lowered with CTD]; Backscatter; Date/time start; DEPTH, water; Echo backscatter; Event label; Global positioning system; GPS; Hespérides; LADCP; LATITUDE; LONGITUDE; MALASPINA_LEG3; MALASPINA_LEG3_046-4; MALASPINA_LEG3_047-4; MALASPINA_LEG3_048-4; MALASPINA_LEG3_049-4; MALASPINA_LEG3_050-4; MALASPINA_LEG3_051-4; MALASPINA_LEG3_052-4; MALASPINA_LEG3_053-4; MALASPINA_LEG3_054-4; MALASPINA_LEG3_055-4; MALASPINA_LEG3_056-4; MALASPINA_LEG3_057-4; MALASPINA_LEG3_058-4; MALASPINA_LEG3_059-4; MALASPINA_LEG3_060-4; MALASPINA_LEG3_061-4; MALASPINA_LEG3_062-4; MALASPINA_LEG3_063-4; MALASPINA_LEG3_064-4; MALASPINA_LEG3_065-4; MALASPINA-2010; Malaspina circumnavigation expedition; Malaspina Expedition; MH062_046; MH063_047; MH064_048; MH065_049; MH066_050; MH067_051; MH073_053; MH074_054; MH075_055; MH076_056; MH077_057; MH078_058; MH079_059; MH081_061; MH082_062; MH083_063; MH084_064; Station label; SUMMER; Sustainable Management of Mesopelagic Resources; TRIATLAS; Tropical and South Atlantic climate-based marine ecosystem predictions for sustainable management
    Type: Dataset
    Format: text/tab-separated-values, 19986 data points
    Location Call Number Expected Availability
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  • 14
    Publication Date: 2024-06-14
    Keywords: 29HE20110317; Acoustic Doppler Current Profiling (LADCP) [lowered with CTD]; Backscatter; Date/time start; DEPTH, water; Echo backscatter; Event label; Global positioning system; GPS; Hespérides; LADCP; LATITUDE; LONGITUDE; MALASPINA_LEG4; MALASPINA_LEG4_069-4; MALASPINA_LEG4_070-4; MALASPINA_LEG4_071-4; MALASPINA_LEG4_072-4; MALASPINA_LEG4_073-4; MALASPINA_LEG4_074-4; MALASPINA_LEG4_075-4; MALASPINA_LEG4_076-4; MALASPINA_LEG4_077-4; MALASPINA_LEG4_078-4; MALASPINA-2010; Malaspina circumnavigation expedition; Malaspina Expedition; MH095_069; MH096_070; MH097_071; MH098_072; MH099_073; MH100_074; MH101_075; MH103_077; MH104_078; Station label; SUMMER; Sustainable Management of Mesopelagic Resources; TRIATLAS; Tropical and South Atlantic climate-based marine ecosystem predictions for sustainable management
    Type: Dataset
    Format: text/tab-separated-values, 11469 data points
    Location Call Number Expected Availability
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  • 15
    Publication Date: 2024-06-14
    Keywords: 29HE20110416; Acoustic Doppler Current Profiling (LADCP) [lowered with CTD]; Backscatter; Date/time start; DEPTH, water; Echo backscatter; Event label; Global positioning system; GPS; Hespérides; LADCP; LATITUDE; LONGITUDE; MALASPINA_LEG5; MALASPINA_LEG5_079-4; MALASPINA_LEG5_081-4; MALASPINA_LEG5_082-4; MALASPINA_LEG5_083-4; MALASPINA_LEG5_084-4; MALASPINA_LEG5_085-4; MALASPINA_LEG5_086-4; MALASPINA_LEG5_087-4; MALASPINA_LEG5_088-4; MALASPINA_LEG5_089-4; MALASPINA_LEG5_090-4; MALASPINA_LEG5_091-4; MALASPINA_LEG5_092-4; MALASPINA_LEG5_093-4; MALASPINA_LEG5_094-4; MALASPINA_LEG5_095-4; MALASPINA_LEG5_096-4; MALASPINA_LEG5_097-4; MALASPINA_LEG5_098-4; MALASPINA_LEG5_099-4; MALASPINA_LEG5_100-4; MALASPINA-2010; Malaspina circumnavigation expedition; Malaspina Expedition; MH124_080; MH125_081; MH126_082; MH127_083; MH128_084; MH129_085; MH130_086; MH131_087; MH132_088; MH133_089; MH134_090; MH135_091; MH136_092; MH137_093; MH138_094; MH139_095; MH140_096; MH141_097; MH142_098; MH143_099; MH144_100; Station label; SUMMER; Sustainable Management of Mesopelagic Resources; TRIATLAS; Tropical and South Atlantic climate-based marine ecosystem predictions for sustainable management
    Type: Dataset
    Format: text/tab-separated-values, 19233 data points
    Location Call Number Expected Availability
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  • 16
    Publication Date: 2024-06-14
    Keywords: 29HE20110513; Acoustic Doppler Current Profiling (LADCP) [lowered with CTD]; Backscatter; Date/time start; DEPTH, water; Echo backscatter; Event label; Global positioning system; GPS; Hespérides; LADCP; LATITUDE; LONGITUDE; MALASPINA_LEG6; MALASPINA_LEG6_101-4; MALASPINA_LEG6_102-4; MALASPINA_LEG6_103-4; MALASPINA_LEG6_104-4; MALASPINA_LEG6_106-4; MALASPINA_LEG6_107-4; MALASPINA_LEG6_108-4; MALASPINA_LEG6_109-4; MALASPINA_LEG6_110-4; MALASPINA_LEG6_111-4; MALASPINA_LEG6_112-4; MALASPINA_LEG6_113-4; MALASPINA_LEG6_114-4; MALASPINA_LEG6_115-4; MALASPINA_LEG6_116-4; MALASPINA_LEG6_118-4; MALASPINA_LEG6_119-4; MALASPINA_LEG6_120-4; MALASPINA_LEG6_121-4; MALASPINA_LEG6_122-4; MALASPINA_LEG6_123-4; MALASPINA_LEG6_124-4; MALASPINA_LEG6_125-4; MALASPINA_LEG6_126-4; MALASPINA-2010; Malaspina circumnavigation expedition; Malaspina Expedition; MH150_101; MH151_102; MH152_103; MH153_104; MH155_106; MH156_107; MH157_108; MH158_109; MH159_110; MH160_111; MH161_112; MH162_113; MH163_114; MH164_115; MH165_116; MH167_118; MH168_119; MH169_120; MH170_121; MH171_122; MH172_123; MH173_124; MH174_125; MH175_126; Station label; SUMMER; Sustainable Management of Mesopelagic Resources; TRIATLAS; Tropical and South Atlantic climate-based marine ecosystem predictions for sustainable management
    Type: Dataset
    Format: text/tab-separated-values, 25293 data points
    Location Call Number Expected Availability
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  • 17
    facet.materialart.
    Unknown
    PANGAEA
    In:  Meteorology Climatology Remote Sensing, Dep. Umweltwissenschaften, Universität Basel
    Publication Date: 2024-06-14
    Description: In Gobabeb, Namibia SWD, LWD and DIR are each measured redundant with two instruments of the same make (not in this data base). The differences between the pairs are used in the quality control. This is done manually by inspecting plots of half-day diurnal courses of the pairs and their differences. Values are removed mostly in the morning due to daily cleaning. Other reasons for larger differences are birds, insects, or people at the station. There are regular fog events varying in frequency over the year. Usually, the fog appears in the second half of the night and disappears a few hours after sunrise. The case temperatures of pyrgeometers practically never drop below dewpoint but there can be water deposition of the dome.
    Keywords: Air temperature at 2 m height; BARO; Barometer; Baseline Surface Radiation Network; BSRN; DATE/TIME; Diffuse radiation; Diffuse radiation, standard deviation; Direct radiation; Direct radiation, standard deviation; GOB; Gobabeb; HEIGHT above ground; Humidity, relative; HYGRO; Hygrometer; Long-wave downward radiation; Long-wave downward radiation, standard deviation; Long-wave upward radiation; Monitoring station; MONS; Namib Desert, Namibia; Pyranometer, Kipp & Zonen, CMP22, SN 110315, WRMC No. 20100; Pyranometer, Kipp & Zonen, CMP22, SN 110316, WRMC No. 20101; Pyranometer, Kipp & Zonen, CMP22, SN 120330, WRMC No. 20102; Pyrgeometer, Kipp & Zonen, CGR4, SN 110408, WRMC No. 20200; Pyrgeometer, Kipp & Zonen, CGR4, SN 120457, WRMC No. 20201; Pyrheliometer, Kipp & Zonen, CHP 1, SN 110764, WRMC No. 20000; Short-wave downward (GLOBAL) radiation; Short-wave downward (GLOBAL) radiation, standard deviation; Short-wave upward (REFLEX) radiation; Station pressure; Thermometer
    Type: Dataset
    Format: text/tab-separated-values, 580072 data points
    Location Call Number Expected Availability
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  • 18
    Publication Date: 2024-06-14
    Keywords: 29HE20110619; Acoustic Doppler Current Profiling (LADCP) [lowered with CTD]; Backscatter; Date/time start; DEPTH, water; Echo backscatter; Event label; Global positioning system; GPS; Hespérides; LADCP; LATITUDE; LONGITUDE; MALASPINA_LEG7; MALASPINA_LEG7_127-4; MALASPINA_LEG7_128-4; MALASPINA_LEG7_129-4; MALASPINA_LEG7_130-4; MALASPINA_LEG7_131-4; MALASPINA_LEG7_132-4; MALASPINA_LEG7_133-4; MALASPINA_LEG7_134-4; MALASPINA_LEG7_135-4; MALASPINA_LEG7_136-4; MALASPINA_LEG7_138-4; MALASPINA_LEG7_139-4; MALASPINA_LEG7_140-4; MALASPINA_LEG7_141-4; MALASPINA_LEG7_142-4; MALASPINA_LEG7_143-4; MALASPINA_LEG7_144-4; MALASPINA_LEG7_145-4; MALASPINA_LEG7_146-4; MALASPINA_LEG7_147-4; MALASPINA-2010; Malaspina circumnavigation expedition; Malaspina Expedition; MH188_127; MH189_128; MH190_129; MH191_130; MH193_131; MH194_132; MH195_133; MH196_134; MH197_135; MH198_136; MH200_138; MH201_139; MH202_140; MH203_141; MH204_142; MH205_143; MH206_144; MH207_145; MH208_146; MH209_147; Station label; SUMMER; Sustainable Management of Mesopelagic Resources; TRIATLAS; Tropical and South Atlantic climate-based marine ecosystem predictions for sustainable management
    Type: Dataset
    Format: text/tab-separated-values, 21957 data points
    Location Call Number Expected Availability
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  • 19
    facet.materialart.
    Unknown
    PANGAEA
    In:  Meteorology Climatology Remote Sensing, Dep. Umweltwissenschaften, Universität Basel
    Publication Date: 2024-06-14
    Description: In Gobabeb, Namibia SWD, LWD and DIR are each measured redundant with two instruments of the same make (not in this data base). The differences between the pairs are used in the quality control. This is done manually by inspecting plots of half-day diurnal courses of the pairs and their differences. Values are removed mostly in the morning due to daily cleaning. Other reasons for larger differences are birds, insects, or people at the station. There are regular fog events varying in frequency over the year. Usually, the fog appears in the second half of the night and disappears a few hours after sunrise. The case temperatures of pyrgeometers practically never drop below dewpoint but there can be water deposition of the dome.
    Keywords: Air temperature at 2 m height; BARO; Barometer; Baseline Surface Radiation Network; BSRN; DATE/TIME; Diffuse radiation; Diffuse radiation, standard deviation; Direct radiation; Direct radiation, standard deviation; GOB; Gobabeb; HEIGHT above ground; Humidity, relative; HYGRO; Hygrometer; Long-wave downward radiation; Long-wave downward radiation, standard deviation; Long-wave upward radiation; Monitoring station; MONS; Namib Desert, Namibia; Pyranometer, Kipp & Zonen, CMP22, SN 110315, WRMC No. 20100; Pyranometer, Kipp & Zonen, CMP22, SN 110316, WRMC No. 20101; Pyranometer, Kipp & Zonen, CMP22, SN 120330, WRMC No. 20102; Pyrgeometer, Kipp & Zonen, CGR4, SN 110408, WRMC No. 20200; Pyrgeometer, Kipp & Zonen, CGR4, SN 120457, WRMC No. 20201; Pyrheliometer, Kipp & Zonen, CHP 1, SN 110764, WRMC No. 20000; Short-wave downward (GLOBAL) radiation; Short-wave downward (GLOBAL) radiation, standard deviation; Short-wave upward (REFLEX) radiation; Station pressure; Thermometer
    Type: Dataset
    Format: text/tab-separated-values, 560778 data points
    Location Call Number Expected Availability
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  • 20
    facet.materialart.
    Unknown
    PANGAEA
    In:  Izaña Atmospheric Research Center, Meteorological State Agency of Spain
    Publication Date: 2024-06-14
    Keywords: Air temperature at 2 m height; BARO; Barometer; Baseline Surface Radiation Network; BSRN; DATE/TIME; Diffuse radiation; Diffuse radiation, maximum; Diffuse radiation, minimum; Diffuse radiation, standard deviation; Direct radiation; Direct radiation, maximum; Direct radiation, minimum; Direct radiation, standard deviation; EKO Instruments, MR-60, SN S15115.07, WRMC No. 61013; HEIGHT above ground; Humidity, relative; HYGRO; Hygrometer; IZA; Izaña; 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; Net radiation; Net radiation, maximum; Net radiation, minimum; Net radiation, standard deviation; Pyranometer, EKO, MS-802F, SN F15508FR, WRMC No. 61010; Pyranometer, EKO, MS-802F, SN F15509FR, WRMC No. 61011; Pyrgeometer, Kipp & Zonen, CGR4, SN 050783, WRMC No. 61008; Pyrheliometer, Kipp & Zonen, CH1, SN 080050, WRMC No. 61003; 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; Tenerife, Spain; Thermometer
    Type: Dataset
    Format: text/tab-separated-values, 1310294 data points
    Location Call Number Expected Availability
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  • 21
    facet.materialart.
    Unknown
    PANGAEA
    In:  Meteorology Climatology Remote Sensing, Dep. Umweltwissenschaften, Universität Basel
    Publication Date: 2024-06-14
    Description: In Gobabeb, Namibia SWD, LWD and DIR are each measured redundant with two instruments of the same make (not in this data base). The differences between the pairs are used in the quality control. This is done manually by inspecting plots of half-day diurnal courses of the pairs and their differences. Values are removed mostly in the morning due to daily cleaning. Other reasons for larger differences are birds, insects, or people at the station. There are regular fog events varying in frequency over the year. Usually, the fog appears in the second half of the night and disappears a few hours after sunrise. The case temperatures of pyrgeometers practically never drop below dewpoint but there can be water deposition of the dome.
    Keywords: Air temperature at 2 m height; BARO; Barometer; Baseline Surface Radiation Network; BSRN; DATE/TIME; Diffuse radiation; Diffuse radiation, standard deviation; Direct radiation; Direct radiation, standard deviation; GOB; Gobabeb; HEIGHT above ground; Humidity, relative; HYGRO; Hygrometer; Long-wave downward radiation; Long-wave downward radiation, standard deviation; Long-wave upward radiation; Monitoring station; MONS; Namib Desert, Namibia; Pyranometer, Kipp & Zonen, CMP22, SN 110315, WRMC No. 20100; Pyranometer, Kipp & Zonen, CMP22, SN 110316, WRMC No. 20101; Pyranometer, Kipp & Zonen, CMP22, SN 120330, WRMC No. 20102; Pyrgeometer, Kipp & Zonen, CGR4, SN 110408, WRMC No. 20200; Pyrgeometer, Kipp & Zonen, CGR4, SN 120457, WRMC No. 20201; Pyrheliometer, Kipp & Zonen, CHP 1, SN 110764, WRMC No. 20000; Short-wave downward (GLOBAL) radiation; Short-wave downward (GLOBAL) radiation, standard deviation; Short-wave upward (REFLEX) radiation; Station pressure; Thermometer
    Type: Dataset
    Format: text/tab-separated-values, 579938 data points
    Location Call Number Expected Availability
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  • 22
    Publication Date: 2024-06-14
    Description: As a proxy for zooplankton and micronekton biomass in the water column, acoustic backscatter intensity (dB), acquired using a Lowered Acoustic Doppler Current Profiler (LADCP) down to ca. 4000 m depth along the Malaspina Expedition (CSD2008-00077). Datasets are from 7 different legs around the World (1-7): 1 Spain-Brazil, 2 Brazil-South Africa, 3 South Africa-West Australia, 4 West Australia-East Australia, 5 East Australia-Hawaii, 6 Hawaii-Panamá, 7 Panamá-Spain.
    Keywords: Backscatter; Bioacoustics; LADCP; MALASPINA-2010; Malaspina circumnavigation expedition; Malaspina Expedition; SUMMER; Sustainable Management of Mesopelagic Resources; TRIATLAS; Tropical and South Atlantic climate-based marine ecosystem predictions for sustainable management
    Type: Dataset
    Format: application/zip, 7 datasets
    Location Call Number Expected Availability
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  • 23
    Publication Date: 2024-06-14
    Description: We reviewed 274 profiles of zooplankton biomass smaller than 5 mm when this information was available but always excluding macrozooplankton and micronekton. Due to the different mesh sizes (200, 300 or 500 µm) used by the different authors in our review, the obtained values are in some cases an underestimation of mesozooplankton biomass for the smaller size classes. Data not available in Tables were obtained from data points of figures using GraphClick software v3.0. This data is marked with an asterisk in the Supplementary Table 5 of Hernández-León et al. (submitted). Biomass in different units were converted to carbon using different published conversion factors (Cushing et al., 1958). Values from different depth layers were centred at the mean depth, averaged in each profile, and expressed as standing stock below one square meter.
    Keywords: bathypelagic; Biomass; Calculated using Cushing et al. (1958), integrated over layer depth; DEPTH, water; Domain, biology; global; LATITUDE; LONGITUDE; MALASPINA-2010; Malaspina circumnavigation expedition; Ocean; Province; Reference/source; Station label; SUMMER; Sustainable Management of Mesopelagic Resources; TRIATLAS; Tropical and South Atlantic climate-based marine ecosystem predictions for sustainable management; Uniform resource locator/link to reference; Year of observation; Zooplankton; Zooplankton, biomass as carbon
    Type: Dataset
    Format: text/tab-separated-values, 3348 data points
    Location Call Number Expected Availability
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  • 24
    facet.materialart.
    Unknown
    PANGAEA
    In:  Meteorology Climatology Remote Sensing, Dep. Umweltwissenschaften, Universität Basel
    Publication Date: 2024-06-14
    Description: In Gobabeb, Namibia SWD, LWD and DIR are each measured redundant with two instruments of the same make (not in this data base). The differences between the pairs are used in the quality control. This is done manually by inspecting plots of half-day diurnal courses of the pairs and their differences. Values are removed mostly in the morning due to daily cleaning. Other reasons for larger differences are birds, insects, or people at the station. There are regular fog events varying in frequency over the year. Usually, the fog appears in the second half of the night and disappears a few hours after sunrise. The case temperatures of pyrgeometers practically never drop below dewpoint but there can be water deposition of the dome.
    Keywords: Air temperature at 2 m height; BARO; Barometer; Baseline Surface Radiation Network; BSRN; DATE/TIME; Diffuse radiation; Diffuse radiation, standard deviation; Direct radiation; Direct radiation, standard deviation; GOB; Gobabeb; HEIGHT above ground; Humidity, relative; HYGRO; Hygrometer; Long-wave downward radiation; Long-wave downward radiation, standard deviation; Long-wave upward radiation; Monitoring station; MONS; Namib Desert, Namibia; Pyranometer, Kipp & Zonen, CMP22, SN 110315, WRMC No. 20100; Pyranometer, Kipp & Zonen, CMP22, SN 110316, WRMC No. 20101; Pyranometer, Kipp & Zonen, CMP22, SN 120330, WRMC No. 20102; Pyrgeometer, Kipp & Zonen, CGR4, SN 110408, WRMC No. 20200; Pyrgeometer, Kipp & Zonen, CGR4, SN 120457, WRMC No. 20201; Pyrheliometer, Kipp & Zonen, CHP 1, SN 110764, WRMC No. 20000; Short-wave downward (GLOBAL) radiation; Short-wave downward (GLOBAL) radiation, standard deviation; Short-wave upward (REFLEX) radiation; Station pressure; Thermometer
    Type: Dataset
    Format: text/tab-separated-values, 561508 data points
    Location Call Number Expected Availability
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  • 25
    facet.materialart.
    Unknown
    PANGAEA
    In:  Izaña Atmospheric Research Center, Meteorological State Agency of Spain
    Publication Date: 2024-06-14
    Keywords: Air temperature at 2 m height; BARO; Barometer; Baseline Surface Radiation Network; BSRN; DATE/TIME; Diffuse radiation; Diffuse radiation, maximum; Diffuse radiation, minimum; Diffuse radiation, standard deviation; Direct radiation; Direct radiation, maximum; Direct radiation, minimum; Direct radiation, standard deviation; EKO Instruments, MR-60, SN S15115.07, WRMC No. 61013; HEIGHT above ground; Humidity, relative; HYGRO; Hygrometer; IZA; Izaña; 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; Net radiation; Net radiation, maximum; Net radiation, minimum; Net radiation, standard deviation; Pyranometer, EKO, MS-802F, SN F15508FR, WRMC No. 61010; Pyranometer, EKO, MS-802F, SN F15509FR, WRMC No. 61011; Pyrgeometer, Kipp & Zonen, CGR4, SN 050783, WRMC No. 61008; Pyrheliometer, Kipp & Zonen, CH1, SN 080050, WRMC No. 61003; 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; Tenerife, Spain; Thermometer
    Type: Dataset
    Format: text/tab-separated-values, 1360150 data points
    Location Call Number Expected Availability
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  • 26
    facet.materialart.
    Unknown
    PANGAEA
    In:  Izaña Atmospheric Research Center, Meteorological State Agency of Spain
    Publication Date: 2024-06-14
    Keywords: Air temperature at 2 m height; BARO; Barometer; Baseline Surface Radiation Network; BSRN; DATE/TIME; Diffuse radiation; Diffuse radiation, maximum; Diffuse radiation, minimum; Diffuse radiation, standard deviation; Direct radiation; Direct radiation, maximum; Direct radiation, minimum; Direct radiation, standard deviation; EKO Instruments, MR-60, SN S15115.07, WRMC No. 61013; HEIGHT above ground; Humidity, relative; HYGRO; Hygrometer; IZA; Izaña; 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; Net radiation; Net radiation, maximum; Net radiation, minimum; Net radiation, standard deviation; Pyranometer, EKO, MS-802F, SN F15508FR, WRMC No. 61010; Pyranometer, EKO, MS-802F, SN F15509FR, WRMC No. 61011; Pyrgeometer, Kipp & Zonen, CGR4, SN 050783, WRMC No. 61008; Pyrheliometer, EKO, MS-56, SN P15048, WRMC No. 61012; 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; Tenerife, Spain; Thermometer
    Type: Dataset
    Format: text/tab-separated-values, 1310587 data points
    Location Call Number Expected Availability
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  • 27
    facet.materialart.
    Unknown
    PANGAEA
    In:  Izaña Atmospheric Research Center, Meteorological State Agency of Spain
    Publication Date: 2024-06-14
    Keywords: Air temperature at 2 m height; BARO; Barometer; Baseline Surface Radiation Network; BSRN; DATE/TIME; Diffuse radiation; Diffuse radiation, maximum; Diffuse radiation, minimum; Diffuse radiation, standard deviation; Direct radiation; Direct radiation, maximum; Direct radiation, minimum; Direct radiation, standard deviation; EKO Instruments, MR-60, SN S15115.07, WRMC No. 61013; HEIGHT above ground; Humidity, relative; HYGRO; Hygrometer; IZA; Izaña; 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; Net radiation; Net radiation, maximum; Net radiation, minimum; Net radiation, standard deviation; Pyranometer, EKO, MS-802F, SN F15508FR, WRMC No. 61010; Pyranometer, EKO, MS-802F, SN F15509FR, WRMC No. 61011; Pyrgeometer, Kipp & Zonen, CGR4, SN 050783, WRMC No. 61008; Pyrheliometer, Kipp & Zonen, CH1, SN 080050, WRMC No. 61003; 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; Tenerife, Spain; Thermometer
    Type: Dataset
    Format: text/tab-separated-values, 1295474 data points
    Location Call Number Expected Availability
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  • 28
    facet.materialart.
    Unknown
    PANGAEA
    In:  Meteorology Climatology Remote Sensing, Dep. Umweltwissenschaften, Universität Basel
    Publication Date: 2024-06-14
    Description: In Gobabeb, Namibia SWD, LWD and DIR are each measured redundant with two instruments of the same make (not in this data base). The differences between the pairs are used in the quality control. This is done manually by inspecting plots of half-day diurnal courses of the pairs and their differences. Values are removed mostly in the morning due to daily cleaning. Other reasons for larger differences are birds, insects, or people at the station. There are regular fog events varying in frequency over the year. Usually, the fog appears in the second half of the night and disappears a few hours after sunrise. The case temperatures of pyrgeometers practically never drop below dewpoint but there can be water deposition of the dome.
    Keywords: Air temperature at 2 m height; BARO; Barometer; Baseline Surface Radiation Network; BSRN; DATE/TIME; Diffuse radiation; Diffuse radiation, standard deviation; Direct radiation; Direct radiation, standard deviation; GOB; Gobabeb; HEIGHT above ground; Humidity, relative; HYGRO; Hygrometer; Long-wave downward radiation; Long-wave downward radiation, standard deviation; Long-wave upward radiation; Monitoring station; MONS; Namib Desert, Namibia; Pyranometer, Kipp & Zonen, CMP22, SN 110315, WRMC No. 20100; Pyranometer, Kipp & Zonen, CMP22, SN 110316, WRMC No. 20101; Pyranometer, Kipp & Zonen, CMP22, SN 120330, WRMC No. 20102; Pyrgeometer, Kipp & Zonen, CGR4, SN 110408, WRMC No. 20200; Pyrgeometer, Kipp & Zonen, CGR4, SN 120457, WRMC No. 20201; Pyrheliometer, Kipp & Zonen, CHP 1, SN 110764, WRMC No. 20000; Short-wave downward (GLOBAL) radiation; Short-wave downward (GLOBAL) radiation, standard deviation; Short-wave upward (REFLEX) radiation; Station pressure; Thermometer
    Type: Dataset
    Format: text/tab-separated-values, 580143 data points
    Location Call Number Expected Availability
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  • 29
    facet.materialart.
    Unknown
    PANGAEA
    In:  Meteorology Climatology Remote Sensing, Dep. Umweltwissenschaften, Universität Basel
    Publication Date: 2024-06-14
    Description: In Gobabeb, Namibia SWD, LWD and DIR are each measured redundant with two instruments of the same make (not in this data base). The differences between the pairs are used in the quality control. This is done manually by inspecting plots of half-day diurnal courses of the pairs and their differences. Values are removed mostly in the morning due to daily cleaning. Other reasons for larger differences are birds, insects, or people at the station. There are regular fog events varying in frequency over the year. Usually, the fog appears in the second half of the night and disappears a few hours after sunrise. The case temperatures of pyrgeometers practically never drop below dewpoint but there can be water deposition of the dome.
    Keywords: Air temperature at 2 m height; BARO; Barometer; Baseline Surface Radiation Network; BSRN; DATE/TIME; Diffuse radiation; Diffuse radiation, standard deviation; Direct radiation; Direct radiation, standard deviation; GOB; Gobabeb; HEIGHT above ground; Humidity, relative; HYGRO; Hygrometer; Long-wave downward radiation; Long-wave downward radiation, standard deviation; Long-wave upward radiation; Monitoring station; MONS; Namib Desert, Namibia; Pyranometer, Kipp & Zonen, CMP22, SN 110315, WRMC No. 20100; Pyranometer, Kipp & Zonen, CMP22, SN 110316, WRMC No. 20101; Pyranometer, Kipp & Zonen, CMP22, SN 120330, WRMC No. 20102; Pyrgeometer, Kipp & Zonen, CGR4, SN 110408, WRMC No. 20200; Pyrgeometer, Kipp & Zonen, CGR4, SN 120457, WRMC No. 20201; Pyrheliometer, Kipp & Zonen, CHP 1, SN 110764, WRMC No. 20000; Short-wave downward (GLOBAL) radiation; Short-wave downward (GLOBAL) radiation, standard deviation; Short-wave upward (REFLEX) radiation; Station pressure; Thermometer
    Type: Dataset
    Format: text/tab-separated-values, 579976 data points
    Location Call Number Expected Availability
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  • 30
    facet.materialart.
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    PANGAEA
    In:  Meteorology Climatology Remote Sensing, Dep. Umweltwissenschaften, Universität Basel
    Publication Date: 2024-06-14
    Description: In Gobabeb, Namibia SWD, LWD and DIR are each measured redundant with two instruments of the same make (not in this data base). The differences between the pairs are used in the quality control. This is done manually by inspecting plots of half-day diurnal courses of the pairs and their differences. Values are removed mostly in the morning due to daily cleaning. Other reasons for larger differences are birds, insects, or people at the station. There are regular fog events varying in frequency over the year. Usually, the fog appears in the second half of the night and disappears a few hours after sunrise. The case temperatures of pyrgeometers practically never drop below dewpoint but there can be water deposition of the dome.
    Keywords: Air temperature at 2 m height; BARO; Barometer; Baseline Surface Radiation Network; BSRN; DATE/TIME; Diffuse radiation; Diffuse radiation, standard deviation; Direct radiation; Direct radiation, standard deviation; GOB; Gobabeb; HEIGHT above ground; Humidity, relative; HYGRO; Hygrometer; Long-wave downward radiation; Long-wave downward radiation, standard deviation; Long-wave upward radiation; Monitoring station; MONS; Namib Desert, Namibia; Pyranometer, Kipp & Zonen, CMP22, SN 110315, WRMC No. 20100; Pyranometer, Kipp & Zonen, CMP22, SN 110316, WRMC No. 20101; Pyranometer, Kipp & Zonen, CMP22, SN 120330, WRMC No. 20102; Pyrgeometer, Kipp & Zonen, CGR4, SN 110408, WRMC No. 20200; Pyrgeometer, Kipp & Zonen, CGR4, SN 120457, WRMC No. 20201; Pyrheliometer, Kipp & Zonen, CHP 1, SN 110764, WRMC No. 20000; Short-wave downward (GLOBAL) radiation; Short-wave downward (GLOBAL) radiation, standard deviation; Short-wave upward (REFLEX) radiation; Station pressure; Thermometer
    Type: Dataset
    Format: text/tab-separated-values, 561212 data points
    Location Call Number Expected Availability
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  • 31
    facet.materialart.
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    PANGAEA
    In:  Meteorology Climatology Remote Sensing, Dep. Umweltwissenschaften, Universität Basel
    Publication Date: 2024-06-14
    Description: In Gobabeb, Namibia SWD, LWD and DIR are each measured redundant with two instruments of the same make (not in this data base). The differences between the pairs are used in the quality control. This is done manually by inspecting plots of half-day diurnal courses of the pairs and their differences. Values are removed mostly in the morning due to daily cleaning. Other reasons for larger differences are birds, insects, or people at the station. There are regular fog events varying in frequency over the year. Usually, the fog appears in the second half of the night and disappears a few hours after sunrise. The case temperatures of pyrgeometers practically never drop below dewpoint but there can be water deposition of the dome.
    Keywords: Air temperature at 2 m height; BARO; Barometer; Baseline Surface Radiation Network; BSRN; DATE/TIME; Diffuse radiation; Diffuse radiation, standard deviation; Direct radiation; Direct radiation, standard deviation; GOB; Gobabeb; HEIGHT above ground; Humidity, relative; HYGRO; Hygrometer; Long-wave downward radiation; Long-wave downward radiation, standard deviation; Long-wave upward radiation; Monitoring station; MONS; Namib Desert, Namibia; Pyranometer, Kipp & Zonen, CMP22, SN 110315, WRMC No. 20100; Pyranometer, Kipp & Zonen, CMP22, SN 110316, WRMC No. 20101; Pyranometer, Kipp & Zonen, CMP22, SN 120330, WRMC No. 20102; Pyrgeometer, Kipp & Zonen, CGR4, SN 110408, WRMC No. 20200; Pyrgeometer, Kipp & Zonen, CGR4, SN 120457, WRMC No. 20201; Pyrheliometer, Kipp & Zonen, CHP 1, SN 110764, WRMC No. 20000; Short-wave downward (GLOBAL) radiation; Short-wave downward (GLOBAL) radiation, standard deviation; Short-wave upward (REFLEX) radiation; Station pressure; Thermometer
    Type: Dataset
    Format: text/tab-separated-values, 542676 data points
    Location Call Number Expected Availability
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  • 32
    facet.materialart.
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    PANGAEA
    In:  Meteorology Climatology Remote Sensing, Dep. Umweltwissenschaften, Universität Basel
    Publication Date: 2024-06-14
    Description: In Gobabeb, Namibia SWD, LWD and DIR are each measured redundant with two instruments of the same make (not in this data base). The differences between the pairs are used in the quality control. This is done manually by inspecting plots of half-day diurnal courses of the pairs and their differences. Values are removed mostly in the morning due to daily cleaning. Other reasons for larger differences are birds, insects, or people at the station. There are regular fog events varying in frequency over the year. Usually, the fog appears in the second half of the night and disappears a few hours after sunrise. The case temperatures of pyrgeometers practically never drop below dewpoint but there can be water deposition of the dome.
    Keywords: Air temperature at 2 m height; BARO; Barometer; Baseline Surface Radiation Network; BSRN; DATE/TIME; Diffuse radiation; Diffuse radiation, standard deviation; Direct radiation; Direct radiation, standard deviation; GOB; Gobabeb; HEIGHT above ground; Humidity, relative; HYGRO; Hygrometer; Long-wave downward radiation; Long-wave downward radiation, standard deviation; Long-wave upward radiation; Monitoring station; MONS; Namib Desert, Namibia; Pyranometer, Kipp & Zonen, CMP22, SN 110315, WRMC No. 20100; Pyranometer, Kipp & Zonen, CMP22, SN 110316, WRMC No. 20101; Pyranometer, Kipp & Zonen, CMP22, SN 120330, WRMC No. 20102; Pyrgeometer, Kipp & Zonen, CGR4, SN 110408, WRMC No. 20200; Pyrgeometer, Kipp & Zonen, CGR4, SN 120457, WRMC No. 20201; Pyrheliometer, Kipp & Zonen, CHP 1, SN 110764, WRMC No. 20000; Short-wave downward (GLOBAL) radiation; Short-wave downward (GLOBAL) radiation, standard deviation; Short-wave upward (REFLEX) radiation; Station pressure; Thermometer
    Type: Dataset
    Format: text/tab-separated-values, 579982 data points
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  • 33
    Publication Date: 2024-06-14
    Keywords: 29HE20110117; Acoustic Doppler Current Profiling (LADCP) [lowered with CTD]; Backscatter; Date/time start; DEPTH, water; Echo backscatter; Event label; Global positioning system; GPS; Hespérides; LADCP; LATITUDE; LONGITUDE; MALASPINA_LEG2; MALASPINA_LEG2_027-4; MALASPINA_LEG2_028-4; MALASPINA_LEG2_029-4; MALASPINA_LEG2_030-4; MALASPINA_LEG2_031-4; MALASPINA_LEG2_032-4; MALASPINA_LEG2_033-4; MALASPINA_LEG2_034-4; MALASPINA_LEG2_035-4; MALASPINA_LEG2_037-4; MALASPINA_LEG2_038-4; MALASPINA_LEG2_039-4; MALASPINA_LEG2_040-4; MALASPINA_LEG2_041-4; MALASPINA_LEG2_042-4; MALASPINA_LEG2_043-4; MALASPINA_LEG2_044-4; MALASPINA-2010; Malaspina circumnavigation expedition; Malaspina Expedition; MH036_027; MH037_028; MH038_029; MH039_030; MH040_031; MH041_032; MH042_033; MH043_034; MH044_035; MH046_037; MH047_038; MH048_039; MH049_040; MH050_041; MH051_042; MH052_043; MH053_044; Station label; SUMMER; Sustainable Management of Mesopelagic Resources; TRIATLAS; Tropical and South Atlantic climate-based marine ecosystem predictions for sustainable management
    Type: Dataset
    Format: text/tab-separated-values, 19386 data points
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  • 34
    facet.materialart.
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    PANGAEA
    In:  Meteorology Climatology Remote Sensing, Dep. Umweltwissenschaften, Universität Basel
    Publication Date: 2024-06-14
    Description: In Gobabeb, Namibia SWD, LWD and DIR are each measured redundant with two instruments of the same make (not in this data base). The differences between the pairs are used in the quality control. This is done manually by inspecting plots of half-day diurnal courses of the pairs and their differences. Values are removed mostly in the morning due to daily cleaning. Other reasons for larger differences are birds, insects, or people at the station. There are regular fog events varying in frequency over the year. Usually, the fog appears in the second half of the night and disappears a few hours after sunrise. The case temperatures of pyrgeometers practically never drop below dewpoint but there can be water deposition of the dome.
    Keywords: Air temperature at 2 m height; BARO; Barometer; Baseline Surface Radiation Network; BSRN; DATE/TIME; Diffuse radiation; Diffuse radiation, standard deviation; Direct radiation; Direct radiation, standard deviation; GOB; Gobabeb; HEIGHT above ground; Humidity, relative; HYGRO; Hygrometer; Long-wave downward radiation; Long-wave downward radiation, standard deviation; Long-wave upward radiation; Monitoring station; MONS; Namib Desert, Namibia; Pyranometer, Kipp & Zonen, CMP22, SN 110315, WRMC No. 20100; Pyranometer, Kipp & Zonen, CMP22, SN 110316, WRMC No. 20101; Pyranometer, Kipp & Zonen, CMP22, SN 120330, WRMC No. 20102; Pyrgeometer, Kipp & Zonen, CGR4, SN 110408, WRMC No. 20200; Pyrgeometer, Kipp & Zonen, CGR4, SN 120457, WRMC No. 20201; Pyrheliometer, Kipp & Zonen, CHP 1, SN 110764, WRMC No. 20000; Short-wave downward (GLOBAL) radiation; Short-wave downward (GLOBAL) radiation, standard deviation; Short-wave upward (REFLEX) radiation; Station pressure; Thermometer
    Type: Dataset
    Format: text/tab-separated-values, 579976 data points
    Location Call Number Expected Availability
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  • 35
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    PANGAEA
    In:  Izaña Atmospheric Research Center, Meteorological State Agency of Spain
    Publication Date: 2024-06-14
    Keywords: Air temperature at 2 m height; BARO; Barometer; Baseline Surface Radiation Network; BSRN; DATE/TIME; Diffuse radiation; Diffuse radiation, maximum; Diffuse radiation, minimum; Diffuse radiation, standard deviation; Direct radiation; Direct radiation, maximum; Direct radiation, minimum; Direct radiation, standard deviation; EKO Instruments, MR-60, SN S15115.07, WRMC No. 61013; HEIGHT above ground; Humidity, relative; HYGRO; Hygrometer; IZA; Izaña; 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; Net radiation; Net radiation, maximum; Net radiation, minimum; Net radiation, standard deviation; Pyranometer, EKO, MS-802F, SN F15508FR, WRMC No. 61010; Pyranometer, EKO, MS-802F, SN F15509FR, WRMC No. 61011; Pyrgeometer, Kipp & Zonen, CGR4, SN 050783, WRMC No. 61008; Pyrheliometer, Kipp & Zonen, CH1, SN 080050, WRMC No. 61003; 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; Tenerife, Spain; Thermometer
    Type: Dataset
    Format: text/tab-separated-values, 1350390 data points
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  • 36
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    PANGAEA
    In:  Izaña Atmospheric Research Center, Meteorological State Agency of Spain
    Publication Date: 2024-06-14
    Keywords: Air temperature at 2 m height; BARO; Barometer; Baseline Surface Radiation Network; BSRN; DATE/TIME; Diffuse radiation; Diffuse radiation, maximum; Diffuse radiation, minimum; Diffuse radiation, standard deviation; Direct radiation; Direct radiation, maximum; Direct radiation, minimum; Direct radiation, standard deviation; EKO Instruments, MR-60, SN S15115.07, WRMC No. 61013; HEIGHT above ground; Humidity, relative; HYGRO; Hygrometer; IZA; Izaña; 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; Net radiation; Net radiation, maximum; Net radiation, minimum; Net radiation, standard deviation; Pyranometer, EKO, MS-802F, SN F15508FR, WRMC No. 61010; Pyranometer, EKO, MS-802F, SN F15509FR, WRMC No. 61011; Pyrgeometer, Kipp & Zonen, CGR4, SN 050783, WRMC No. 61008; Pyrheliometer, Kipp & Zonen, CH1, SN 080050, WRMC No. 61003; 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; Tenerife, Spain; Thermometer
    Type: Dataset
    Format: text/tab-separated-values, 1273884 data points
    Location Call Number Expected Availability
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  • 37
    facet.materialart.
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    PANGAEA
    In:  Izaña Atmospheric Research Center, Meteorological State Agency of Spain
    Publication Date: 2024-06-14
    Keywords: Air temperature at 2 m height; BARO; Barometer; Baseline Surface Radiation Network; BSRN; DATE/TIME; Diffuse radiation; Diffuse radiation, maximum; Diffuse radiation, minimum; Diffuse radiation, standard deviation; Direct radiation; Direct radiation, maximum; Direct radiation, minimum; Direct radiation, standard deviation; EKO Instruments, MR-60, SN S15115.07, WRMC No. 61013; HEIGHT above ground; Humidity, relative; HYGRO; Hygrometer; IZA; Izaña; 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; Net radiation; Net radiation, maximum; Net radiation, minimum; Net radiation, standard deviation; Pyranometer, EKO, MS-802F, SN F15508FR, WRMC No. 61010; Pyranometer, EKO, MS-802F, SN F15509FR, WRMC No. 61011; Pyrgeometer, Kipp & Zonen, CGR4, SN 050783, WRMC No. 61008; Pyrheliometer, Kipp & Zonen, CH1, SN 080050, WRMC No. 61003; 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; Tenerife, Spain; Thermometer
    Type: Dataset
    Format: text/tab-separated-values, 1306309 data points
    Location Call Number Expected Availability
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  • 38
    facet.materialart.
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    Naturalis Biodiversity Center
    In:  Blumea: Biodiversity, Evolution and Biogeography of Plants vol. 65 no. 1, pp. 25-52
    Publication Date: 2024-06-14
    Description: The Trigonostemon species outside Malesia are taxonomically revised based on herbarium collections and fresh material. The research history in the concerning regions, i.e., the Indian subcontinent (including S India, Sri Lanka, Bangladesh and Myanmar), China, Thailand, Indochina, NE Australia and New Caledonia, is briefly summarised. A total of 32 species are accepted (including one doubtful species) and 17 names are newly treated as synonyms. Trigonostemon montanus is newly described for India. Regional identification keys, nomenclature, descriptions, geographic distributions and taxonomic notes are provided. Together with our previous work, the genus is now fully revised. A total of 59 species are accepted. A full identification list of all Trigonostemon collections seen is presented.
    Keywords: Plant Science ; Ecology ; Evolution ; Behavior and Systematics ; Euphorbiaceae ; identification ; morphological revision ; non-Malesian ; taxonomy ; Trigonostemon
    Repository Name: National Museum of Natural History, Netherlands
    Type: info:eu-repo/semantics/article
    Format: application/pdf
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  • 39
    Publication Date: 2024-06-13
    Description: Baffin Bay is a semi-enclosed basin connecting the Arctic Ocean and the western North Atlantic, thus making out a significant pathway for heat exchange. Here we reconstruct the alternating advection of relatively warmer and saline Atlantic waters versus the incursion of colder Arctic water masses entering Baffin Bay through the multiple gateways in the Canadian Arctic Archipelago and the Nares Strait during the Holocene. We carried out benthic foraminiferal assemblage analyses, X-ray fluorescence scanning, and radiocarbon dating of a 738 cm long marine sediment core retrieved from eastern Baffin Bay near Upernavik, Greenland (Core AMD14-204C; 987m water depth). Results reveal that eastern Baffin Bay was subjected to several oceanographic changes during the last 9.2 kyrCE1. Waning deglacial conditions with enhanced meltwater influxes and an extensive sea-ice cover prevailed in eastern Baffin Bay from 9.2 to 7.9 ka. A transition towards bottom water amelioration is recorded at 7.9 ka by increased advection of Atlantic water masses, encompassing the Holocene Thermal Maximum. A cold period with growing sea-ice cover at 6.7 ka interrupts the overall warm subsurface water conditions, promoted by a weaker northward flow of Atlantic waters. The onset of the neoglaciation at ca. 2.9 ka is marked by an abrupt transition towards a benthic fauna dominated by agglutinated species, likely in part explained by a reduction of the influx of Atlantic Water, allowing an increased influx of the cold, corrosive Baffin Bay Deep Water originating from the Arctic Ocean to enter Baffin Bay through the Nares Strait. These cold subsurface water conditions persisted throughout the Late Holocene, only interrupted by short-lived warmings superimposed on this cooling trend.
    Keywords: AGE; AMD14_1b; AMD14-204_CASQ; AMD14-204C; ArcticNet; Astrononion gallowayi; Baffin Bay; Benthic foraminifera; Bolivina pseudopunctata; Buliminella elegantissima; Calypso square corer; CASQ; Cassidulina neoteretis; Cassidulina reniforme; CCGS Amundsen; DEPTH, sediment/rock; Elphidium clavatum; Epistominella arctica; Epistominella vitrea; Foraminifera, benthic; Foraminifera, benthic agglutinated; Foraminifera, benthic atlantic species; Foraminifera, benthic calcareous; Foraminifera, planktic; Foraminifera, sea ice species; Holocene; Islandiella norcrossi; Nonionellina labradorica; Portatrochammina bipolaris; Psammosphaera fusca; Ratio; Recurvoides trochamminiformis; Reophax subfusiformis; Stainforthia feylingi; Textularia earlandi; Textularia kattegatensis; Textularia torquata
    Type: Dataset
    Format: text/tab-separated-values, 2106 data points
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  • 40
    Publication Date: 2024-06-13
    Keywords: Age; Astrononion gallowayi; Cassidulina neoteretis; Cassidulina reniforme; Cibicidoides lobatulus; DEPTH, sediment/rock; Elphidium spp.; Foraminifera, benthic; Foraminifera, benthic atlantic species; GEO8144/3144; Helmer Hanssen; HH15-1252PC; Melonis barleeanus; Nonionella spp.; PC; Piston corer; Stainforthia spp.; Vestnesa Ridge
    Type: Dataset
    Format: text/tab-separated-values, 1935 data points
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  • 41
    Publication Date: 2024-06-13
    Description: Salinity and Oxygen were not calibrated beyond the manufacturer's calibration coefficients. Compared to climatological values (WOA18) salinity appears to be 0.05 PSU too low. Both CTD sensors and the two TSG sensors do however agree. Oxygen values are in the range of the climatological values, possibly 5 umol/kg too low. Some deep profiles show consistently low oxygen values that is not represented in the climatology. Use this data with caution.
    Keywords: CTD/Rosette; CTD-RO; DATE/TIME; Density, potential; DEPTH, water; Event label; Fluorescence; LATITUDE; LONGITUDE; M150; M150_1-1; M150_113-1; M150_128-1; M150_139-1; M150_14-1; M150_143-1; M150_145-1; M150_155-1; M150_165-1; M150_169-1; M150_171-1; M150_174-1; M150_179-1; M150_192-1; M150_203-1; M150_2-1; M150_211-1; M150_220-1; M150_230-1; M150_238-1; M150_259-1; M150_269-1; M150_272-1; M150_274-1; M150_277-1; M150_281-1; M150_291-1; M150_308-1; M150_313-1; M150_315-1; M150_318-1; M150_323-1; M150_333-1; M150_347-1; M150_352-1; M150_355-1; M150_363-1; M150_380-1; M150_383-1; M150_386-1; M150_389-1; M150_39-1; M150_393-1; M150_404-1; M150_419-1; M150_423-1; M150_426-1; M150_429-1; M150_433-1; M150_443-1; M150_462-1; M150_465-1; M150_467-1; M150_470-1; M150_476-1; M150_486-1; M150_505-1; M150_508-1; M150_5-1; M150_51-1; M150_511-1; M150_522-1; M150_529-1; M150_531-1; M150_537-1; M150_539-1; M150_549-1; M150_560-1; M150_561-1; M150_563-1; M150_572-1; M150_584-1; M150_587-1; M150_597-1; M150_605-1; M150_615-1; M150_622-1; M150_639-1; M150_647-1; M150_654-1; M150_71-1; M150_72-1; M150_77-1; M150_87-1; M150_91-1; M150_94-1; Meteor (1986); Oxygen; Pressure, water; Radiation, photosynthetically active; Radiation, photosynthetically active, surface; Salinity; Sound velocity in water; Temperature, water
    Type: Dataset
    Format: text/tab-separated-values, 445770 data points
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  • 42
    Publication Date: 2024-06-13
    Description: These datasets provide data for the lowest part of a new composite profile GOS18 from Lake Gościąż in central Poland. The composite profile was established using sediment cores recovered in 2015 and 2018 with an UWITEC Piston Corer at 19.6-21.5 m water depth (Bonk et al., in press). Our data covers the time interval from the onset of lacustrine sedimentation in the late Allerød to the early Preboreal. Since Lake Gościąż comprises a continuous, seasonally resolved (varved) and exceptionally well-preserved archive of the Younger Dryas (YD) climate variation, it is highly suitable for detailed investigations of lake system responses during periods of rapid climate cooling (YD onset) and warming (YD termination), respectively. Our varve chronology is the lowest part of a new floating varve chronology established for Lake Gościąż (central Poland) that has been anchored to the absolute time scale through radiocarbon dating and age modelling (Bonk et al., in press). The here presented varve chronology reaches from the onset of lacustrine sedimentation in the late Allerød until the early Preboreal. Uncertainties for the absolute ages are derived from radiocarbon age modelling and varve counting. The internal varve counting uncertainty for the observed time interval is generally low (+14/-22) due to the mostly excellent varve preservation. Microfacies analyses, including varve counting and measurements of varve and sublayer thickness, have been performed on overlapping large-scale thin sections under an Axioplan 2 and Axiolab pol imaging microscope at magnifications of 50-400x. Thin sections have been prepared from 10 cm long freeze-dried and resin impregnated sediment slices (Brauer & Casanova 2001; doi:10.1023/A:1008136029735). The dataset incorporates the composite depth, age [BP] and age uncertainties [BP] for the varve bottom, the total varve thickness, selected sublayer thicknesses, detrital sublayer occurrence, the different varve types and the varve quality index (VQI).
    Keywords: AGE; Age, uncertainty maximum/old; Age, uncertainty minimum/young; Axioplan 2 and Axiolab pol imaging microscopes; chironomid-inferred temperature reconstructions; Depth, composite; GOS18_composite; Lake Gościąż; Lake Gościąż, Poland; microfacies analyses; PCUWI; Piston corer, UWITEC; Poland; varve chronology; Varve quality index; Varve sub-layer occurrence; Varve thickness; Varve thickness, amorphous organic matter sub-layer; Varve thickness, calcite sub-layer; Varve thickness, diatoms sub-layer; Varve type; δ13Corg; δ18Ocarb
    Type: Dataset
    Format: text/tab-separated-values, 13903 data points
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  • 43
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    Naturalis Biodiversity Center
    In:  Blumea: Biodiversity, Evolution and Biogeography of Plants vol. 65 no. 1, pp. 90-93
    Publication Date: 2024-06-13
    Description: Orchidantha anthracina (Lowiaceae), discovered at the south central coast of Vietnam, is described and illustrated, bringing the total number of species in the family to 26, of which four occur in Vietnam. The notes on distribution, habitat and etymology are given and a preliminary conservation assessment is provided. The species is compared with O. vietnamica, with which it shares flowers of similar size and colours, but from which it is readily distinguished by a narrow and strongly reflexed dorsal sepal and spreading lateral sepals, not supporting the labellum. Notes with additional comparisons to all species with a similar arrangement of lateral sepals are also provided.
    Keywords: Plant Science ; Ecology ; Evolution ; Behavior and Systematics ; Orchidantha grandiflora ; Orchidantha inouei ; Orchidantha vietnamica ; Phú Yên province ; south central coast of Vietnam ; vulnerable ; Zingiberales
    Repository Name: National Museum of Natural History, Netherlands
    Type: info:eu-repo/semantics/article
    Format: application/pdf
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  • 44
    facet.materialart.
    Unknown
    Naturalis Biodiversity Center
    In:  Blumea: Biodiversity, Evolution and Biogeography of Plants vol. 65 no. 1, pp. 86-89
    Publication Date: 2024-06-13
    Description: Three new species combinations are made under Villaria for the Philippine endemics Hypobathrum coriaceum, H. multibracteatum and H. purpureum. Morphological features of these three Hypobathrum species revealed a closer resemblance with Villaria than with Hypobathrum, as the three Philippine endemics possess a unilocular ovary with parietal placentation; a character that is not found in any genera of Octotropideae except in Villaria. Lectotypes and a neotype are selected.
    Keywords: Plant Science ; Ecology ; Evolution ; Behavior and Systematics ; Hypobathrum ; Ixoroideae ; Octotropideae ; Philippine endemics ; Rubiaceae ; Villaria
    Repository Name: National Museum of Natural History, Netherlands
    Type: info:eu-repo/semantics/article
    Format: application/pdf
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  • 45
    Publication Date: 2024-06-12
    Description: We present a continuous and well-resolved record of climatic variability for the past 100,000 yrs from a marine sediment core taken in Delagoa Bight, off southeastern Africa. In addition to providing a sea surface temperature reconstruction for the past ca. 100,000 yrs, this record also allows a high-resolution continental climatic reconstruction. Climate sensitive organic proxies, like the distribution and isotopic composition of plant-wax lipids as well as elemental indicators for fluvial input and weathering type provide information on climatic changes in the adjacent catchment areas (Incomati, Matola, and Lusutfu rivers). At the transition between glacials and interglacials, shifts in vegetation correlate with changes in sea surface temperature in the Agulhas current. The local hydrology, however, does not follow these orbital-paced shifts. Instead, precipitation patterns follow millennial scale variations with different forcing mechanisms in glacial versus interglacial climatic states. During glacials, southward displacement of the Intertropical Convergence Zone facilitates a transmission of northern hemispheric signals (e.g. Heinrich events) to the southern hemispheric subtropics. Furthermore, the southern hemispheric westerlies become a more direct source of precipitation as they shift northward over the study site, especially during Antarctic cold phases. During interglacials, the observed short-term hydrological variability is also a function of Antarctic climate variability, however, it is driven by the indirect influence of the southern hemispheric westerlies and the associated South African high-pressure cell blocking the South Indian Ocean Convergence Zone related precipitation. As a consequence of the interplay of these effects, small scale climatic zones exist. We propose a conceptual model describing latitudinal shifts of these zones along the southeastern African coast as tropical and temperate climate systems shift over glacial and interglacial cycles. The proposed model explains some of the apparent contradictions between several paleoclimate records in the region.
    Keywords: TRACES; Tracing Human and Climate impacts in South Africa
    Type: Dataset
    Format: application/zip, 5 datasets
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  • 46
    Publication Date: 2024-06-12
    Description: The data comprise sample locations and results of grain size measurements and optically stimulated luminescence dating of sediments from the Orog Nuur Basin (southern Mongolia). Samples were taken in order to gain a comprehensive sedimentological and geochronological overview over late Quaternary sediment cascades and respective archives. Grain size measurements were conducted in Aachen using a Beckmann Coulter Laser Particle Sizer. OSL data were obtained in the Luminescence lab of Cologne University. Samples were classified into 7 sediment archives according to the field description and grain size analysis (fluvial, beach ridge, lacustrine, littoral sand, dune sand, basin silty sands, and mountain silt). The grain size statistics is presented in the .xlsx-table according to this classification. The combination of sedimentological, geomorphologic and geochronological observations led to a late Quaternary landscape reconstruction, including alluvial fan evolution, lake level history and aeolian dynamics in this arid region of the northern Gobi Desert.
    Keywords: CAME-II_Q-TIP; Crossing Climatic Tipping Points - Consequences for Central Asia; MULT; Multiple investigations; Orog_Nuur
    Type: Dataset
    Format: application/zip, 10 datasets
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  • 47
    Publication Date: 2024-06-12
    Keywords: 2016/21/B/ST10/02334; Apatite; chaetognaths; chemical data; conodonts; Origin and early development stages of conodonts and chaetognaths; Oxygen isotopes
    Type: Dataset
    Format: application/zip, 4 datasets
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  • 48
    Publication Date: 2024-06-12
    Description: We performed laboratory friction experiments on simulated fault gouges, measuring both the velocity- and slip-dependence of friction in velocity-step tests. Here, we evaluate the relative importance of slip- and velocity-dependent friction in laboratory velocity-stepping experiments, and assess the impact of friction slip dependence on natural faults.As an analogue fault gouge, we used a mixture of silt-sized quartz and commercially obtained clay-rich sediment (Grüne Tonerde, Argiletz Laboratories) mixed with deionized water. All tests were conducted at an (effective) normal stress of 2 MPa, with total shear displacements of up to ~16 mm.
    Keywords: fault; friction; JSPS KAKENHI; KAKENHI; weakening
    Type: Dataset
    Format: application/zip, 4 datasets
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  • 49
    Publication Date: 2024-06-12
    Description: We present a multi-proxy dataset of two sediment cores (0.61 and 0.41 m long) from interconnected infilled depositional basins in the Kobbefjord area, southwestern Greenland. We performed analyses of magnetic susceptibility, grain size distribution, X-ray fluorescence (XRF) element composition , total content of carbon, nitrogen and sulfur, biogenic silica (at 0.5-cm resolution), and diatom stratigraphy (at 1 to 5-cm resolution). The sequences provide evidence of sedimentation in former shallow Arctic lakes or ponds in sparsely glacierized catchments.
    Keywords: Arctic Pond Sediments; biogenic silica; Diatom Stratigraphy; Grain Size; magnetic susceptibility; XRF
    Type: Dataset
    Format: application/zip, 4 datasets
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  • 50
    Publication Date: 2024-06-12
    Description: Surface ablation/accumulation was measured at 55 locations at the 79°N Glacier (Nioghalvfjerdsbraeen Glacier) in northeast Greenland in 2017 and 2018 (see links in "Further details"). Ablation/Accumulation are measured changes in height above ground level of bamboo poles installed in early July 2017 and changes were measured in late July 2017 or/and in July 2018.
    Keywords: 79°N Glacier; Ablation
/Accumulation; AWI Arctic Land Expedition; GL-Land_2017_iGRIFF; GL-Land_2018_iGRIFF; Greenland - Ice Sheet/Ocean Interaction: From process understanding to an analysis of the regional system; GROCE; ICEM; Ice measurement; iGRIFF_79N_glacier_2017; iGRIFF_79N_glacier_2018; iGRIFF 79°N Glacier Expedition; Nioghalvfjerdsbraeen Glacier; Northeast Greenland
    Type: Dataset
    Format: application/zip, 4 datasets
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  • 51
    Publication Date: 2024-06-12
    Description: Data presented here were collected during the two cruises SO248 and SO254 with RV SONNE in the Pacific Ocean at 25 stations along a transect closely following 180° longitude E/W between 52.1°S southeast of New Zealand and 58.9°N in the Bering Sea. The first cruise SO248 was conducted from Auckland, New Zealand, to Dutch Harbor, USA (May 1st, 2016 - June 3rd, 2016) and the second (SO254) took place from January 26th, 2017 - February 27th, 2017 and started and ended in Auckland, New Zealand. The data comprises hydrographical, chemical, biogeochemical and biological parameters.
    Keywords: Acetone extraction, fluorescence determination; Amino acid, total dissolved free; Amino acid, total dissolved free uptake; Amino acid, total hydrolysable dissolved; Amino acids, dissolved combined; BacGeoPac; Bacteria; Bacteria, heterotrophic with relatively low DNA content; BD FACS ARIA3 Flow Cytometer, autofluorescence (AF); Bering Sea; biogeochemistry; Biogeographical province; Biogeographical province after Longhurst (2006); biogeography; Breakdown of fluorescent substrate analoga (Obayashi and Suzuki, 2005, Limnol Oceanogr; Balmonte et al ., 2018, Environ Microbiol); Calculated; Calculated; DCAA = THDAA - DFAA; after Lunau et al. (2006); Calculated from downwelling photosynthetically active radiation PAR Ed, integrated from 400 - 700 nm; Carbohydrates, dissolved, neutral free; Carbohydrates, dissolved, neutral free, uptake; Carbohydrates, total hydrolyzable; Carbon, organic, particulate; Carbon, organic, particulate/Nitrogen, organic, particulate ratio; CARD-FISH; Catalyzed reporter deposition fluorescence in situ hybridisation (CARD-FISH); Catalyzed reporter deposition fluorescence in situ hybridisation (CARD-FISH), % of the DAPI positive stained cells; Chlorophyll a; Combustion by FlashEA 1112 CHN-analyzer; Conductivity; CTD, Sea-Bird, SBE 911plus [SN: 09-1266]; CTD, SEA-BIRD SBE 911plus, SN 5828 / SN 4529; CTD/Rosette; CTD-RO; cyanobacteria; Cyanobacteria; Cyanobacteria, cell size, forward scatter; Cyanobacteria, cell size, side scatter; Cytophaga-Flavobacteria; Cytophaga-Flavobacteria, cells; DATE/TIME; Density, sigma-theta (0); Depth, relative; DEPTH, water; Depth of Secchi Disk; ELEVATION; Equatorial Pacific; Eukaryotes; Eukaryotes, cell size, forward scatter; Eukaryotes, cell size, relative; Eukaryotes, cell size, side scatter; Event label; Flagellates+algae; Flagellates+algae, cell size, forward scatter; Flagellates+algae, cell size, side scatter; Flow Cytometer, BD Biosciences, C6 [autofluorescence, calibration of the forward scatter (FSC)]; Flow Cytometer, BD Biosciences, C6 [autofluorescence (AF)]; Flow Cytometer, BD Biosciences, C6 [calibration of the forward scatter (FSC), only relative cell size due to calibration after Giebel et al. (2019)]; Flow Cytometer, BD Biosciences, C6 [SybrGreenI staining]; flow cytometry; Fluorescence, chlorophyll; Fluorescence determination; Fluorometer, WET Labs ECO AFL/FL; Forel-Ule index; Gammaproteobacteria; Gammaproteobacteria, cells; Generation time; heterotrophic prokaryotic production; High nucleic acid bacteria; High nucleic acid bacteria, cell size, forward scatter; High nucleic acid bacteria, cell size, relative; High nucleic acid bacteria, cell size, side scatter; High performance liquid chromatography (HPLC) using an Agilent 1200 HPLC device after an ortho-phthaldialdehyde precolumn derivatization (Lindroth and Mopper, 1979) with slight modifications as described by Lunau et al. (2006); High Performance Liquid Chromatography (HPLC) using anion-exchange columns by pulsed amperometric detection according to Mopper et al. (1992); HNA; HPLC after Lindroth and Mopper (1979) with slight modifications as described by Lunau et al. (2006); Hydrolysis rate, beta-Glucose; Hydrolysis rate, Leucine; Incorporation of 14C-leucine (Simon and Azam, 1989, http://www.int-res.com/articles/meps/51/m051p201.pdf; Simon et al. 2004, doi:10.4319/lo.2004.49.4.1035); Incorporation of 3H-acetate (Simon et al. 2007, doi:10.4319/lo.2007.52.1.0085); Incorporation of 3H-Amino acid mix (Simon et al. 2004, doi:10.4319/lo.2004.49.4.1035; 2007, doi:10.4319/lo.2007.52.1.0085); Incorporation of 3H-Glucose (Simon et al. 2004, doi:10.4319/lo.2004.49.4.1035; 2007, doi:10.4319/lo.2007.52.1.0085); LATITUDE; LNA; LONGITUDE; Low nucleic acid bacteria; Low nucleic acid bacteria, cell size, forward scatter; Low nucleic acid bacteria, cell size, relative; Low nucleic acid bacteria, cell size, side scatter; Microplankton; Microplankton, cell size, forward scatter; Microplankton, cell size, relative; Microplankton, cell size, side scatter; Mixed layer depth; Nanoplankton; Nanoplankton, cell size, forward scatter; Nanoplankton, cell size, relative; Nanoplankton, cell size, side scatter; Nitrate; Nitrite; Nitrogen, organic, particulate; Nitrogen oxide; North Pacific Ocean; Ökologie, Physiologie und Molekularbiologie der Roseobacter-Gruppe: Aufbruch zu einem systembiologischen Verständnis einer global wichtigen Gruppe mariner Bakterien; Oxygen; Oxygen optode, Aanderaa, type 4831F; Pacific Ocean; Phosphate; Picoplankton; Picoplankton, cell size, forward scatter; Picoplankton, cell size, relative; Picoplankton, cell size, side scatter; Polaribacter; Polaribacter, cells; Pori Bac NewZ; Pressure, water; Prochlorococcus; Prochlorococcus, cell size, forward scatter; Prochlorococcus, cell size, side scatter; Prokaryotes, cell size, forward scatter; Prokaryotes, cell size, relative; Prokaryotes, growth rate; Prokaryotes, heterotroph; Prokaryotes, heterotroph, biomass production in mass protein; Prokaryotes, heterotroph, carbon production; Prokaryotes, heterotroph, cell size, side scatter; Prokaryotes, heterotroph, nitrogen production; Prokaryotes, heterotroph, protein production; Roseobacter; Roseobacter, cells; Roseobacter clade affiliated cluster, Planktomarina temperata; Roseobacter clade affiliated cluster, Planktomarina temperata, cells; RV Sonne; Salinity; SAR11; SAR11, cells; Silicate; SO248; SO248_10-2a; SO248_1-1; SO248_11-1; SO248_12-1; SO248_13-3; SO248_14-3; SO248_15-1; SO248_16-2; SO248_17-4; SO248_18-3; SO248_19-1; SO248_2-1; SO248_3-1; SO248_4-3; SO248_5-1; SO248_6-2; SO248_7-1; SO248_8-4; SO248_9-6; SO254; SO254_11-1; SO254_32-1; SO254_38-1; SO254_47-1; SO254_61-1; SO254_65-1; Sonne_2; Sound velocity in water; South Pacific Ocean; Station label; Synechococcus; Synechococcus, cell size, forward scatter; Synechococcus, cell size, side scatter; Temperature, water; Temperature, water, potential; TRR51; Turbidity (Nephelometric turbidity unit); Turnover rate, acetate; Turnover rate, amino acids, dissolved, free; Turnover rate, glucose
    Type: Dataset
    Format: text/tab-separated-values, 19990 data points
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  • 52
    Publication Date: 2024-06-12
    Keywords: Age, 14C AMS; Age, dated; Age, dated standard deviation; Calendar age, maximum/old; Calendar age, minimum/young; DEPTH, sediment/rock; Laboratory code/label; MKD1; Mkhuze, KwaZulu-Natal, South Africa; Mkhuze swamp; PCUWI; Piston corer, UWITEC; Probability; TRACES; Tracing Human and Climate impacts in South Africa
    Type: Dataset
    Format: text/tab-separated-values, 84 data points
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  • 53
    Publication Date: 2024-06-12
    Keywords: Calculated from Mg/Ca ratios (Lea et al. 2003); DEPTH, sediment/rock; GC; GeoB20616-1; Gravity corer; ICP-OES; M123; M123_175-1; Magnesium/Calcium ratio; Meteor (1986); Sea surface temperature, annual mean; TRACES; Tracing Human and Climate impacts in South Africa
    Type: Dataset
    Format: text/tab-separated-values, 96 data points
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  • 54
    facet.materialart.
    Unknown
    PANGAEA
    In:  Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven
    Publication Date: 2024-06-12
    Description: A total of four moorings ("1893", "Taymyr", "Kotelny", "Vilkitsky") was deployed in September 2013 during the Transdrift 21 - expedition and recovered in September 2014 during Transdrift 22 aboard the Viktor Buinitsky. The expeditions were carried out in the framework of the German-Russian "Laptev Sea Systems" partnership, and within the BMBF-funded "Transdrift"-project. The moorings were equipped with RDI-Workhorse ADCPs for current measurements and Seabird SBE37 for temperature and salinity measurements. Sampling intervals were 1 hour for ADCP, and 30 minutes for SBE37. Currents were corrected for misalignment based on angles extracted from: https://geomag.nrcan.gc.ca/calc/mdcal-en.php Not all SBE37 models included a pressure sensor. If pressure was recorded, the data files provide pressure and the converted water depth. For models without a pressure sensor, the data file lists only a constant value indicating the targeted instrument depth. Temperature and salinity data were despiked, and outliers exceeding three times the standard deviation were removed and interpolated.
    Keywords: 1893-T1-13; Arctic Ocean; AWI_PhyOce; CTD, SEA-BIRD SBE 37; DATE/TIME; Density, sigma-theta (0); DEPTH, water; Gear identification number; Laptev Sea; Laptev Sea System; LSS; Mooring (long time); MOORY; oceanographic moorings; Physical Oceanography @ AWI; Pressure, water; Salinity; System Laptev-Sea: Transdrift; Temperature, water; TRANSDRIFT; Transdrift-XXI; VB13; VB13_16-5a; Viktor Buynitskiy
    Type: Dataset
    Format: text/tab-separated-values, 441575 data points
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  • 55
    Publication Date: 2024-06-12
    Keywords: ADCP; AWI_SeaIce; DATE/TIME; Ivan Petrov; Laptev Sea; Laptev Sea System; Latitude of event; Longitude of event; LSS; Mooring (long time); MOORY; OSL-08; OuterShelf-0809; sea ice draft; Sea ice draft; Sea Ice Physics @ AWI; System Laptev-Sea: Transdrift; TRANSDRIFT; Transdrift-XIV; Upward looking Acoustic Doppler Current Profiler
    Type: Dataset
    Format: text/tab-separated-values, 340 data points
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  • 56
    Publication Date: 2024-06-12
    Description: Soil surface temperatures were collected with help of iButtons along different transects and clusters in the region of Illirney (Russia). The interval was set to 4 hours resp. 4.25 hours. Different models of iButtons were used (with a resolution of 0.0625 °C and 0.5°C resp.), see Comment.
    Keywords: AWI_Envi; AWI_Perma; AWI Arctic Land Expedition; Chukotka, Russia; DATE/TIME; DEPTH, soil; ibuttons; iButton sensor; Illirney-iButton005; MULT; Multiple investigations; Nyurba 2019; Permafrost Research; PermaRisk; Polar Terrestrial Environmental Systems @ AWI; RU-Land_2019_Nyurba; Simulating erosion processes in permafrost landscapes under a warming climate – a risk assessment for ecosystems and infrastructure within the Arctic; soil surface temperature; Temperature, soil
    Type: Dataset
    Format: text/tab-separated-values, 3280 data points
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  • 57
    Publication Date: 2024-06-12
    Keywords: Age, dated; Age, dated material; Age, dated standard deviation; Calendar age; Calendar age, maximum/old; Calendar age, minimum/young; DEPTH, sediment/rock; GC; GeoB20616-1; Gravity corer; Laboratory code/label; M123; M123_175-1; Meteor (1986); TRACES; Tracing Human and Climate impacts in South Africa
    Type: Dataset
    Format: text/tab-separated-values, 76 data points
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  • 58
    Publication Date: 2024-06-12
    Keywords: ADCP; Anabar-07; AWI_SeaIce; DATE/TIME; IP07-2_1-1M, Anabar-0708; Ivan Petrov; Laptev Sea; Laptev Sea System; Latitude of event; Longitude of event; LSS; Mooring (long time); MOORY; sea ice draft; Sea ice draft; Sea Ice Physics @ AWI; System Laptev-Sea: Transdrift; TD07; TRANSDRIFT; Transdrift-XII; Upward looking Acoustic Doppler Current Profiler
    Type: Dataset
    Format: text/tab-separated-values, 359 data points
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  • 59
    Publication Date: 2024-06-12
    Keywords: ADCP; AWI_SeaIce; DATE/TIME; Ivan Petrov; Khatanga-08; Khatanga-0809; Laptev Sea; Laptev Sea System; Latitude of event; Longitude of event; LSS; Mooring (long time); MOORY; sea ice draft; Sea ice draft; Sea Ice Physics @ AWI; System Laptev-Sea: Transdrift; TRANSDRIFT; Transdrift-XIV; Upward looking Acoustic Doppler Current Profiler
    Type: Dataset
    Format: text/tab-separated-values, 194 data points
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  • 60
    Publication Date: 2024-06-12
    Keywords: ADCP; AWI_SeaIce; DATE/TIME; Laptev Sea; Laptev Sea System; Latitude of event; Longitude of event; LSS; Mooring (long time); MOORY; Nikolay Evgenov; OSL-10; OuterShelf-1011; sea ice draft; Sea ice draft; Sea Ice Physics @ AWI; System Laptev-Sea: Transdrift; TD10; TRANSDRIFT; Transdrift-XVII; Upward looking Acoustic Doppler Current Profiler
    Type: Dataset
    Format: text/tab-separated-values, 261 data points
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  • 61
    facet.materialart.
    Unknown
    PANGAEA
    In:  Universität Bern
    Publication Date: 2024-06-12
    Keywords: AGE; anoxia; Aquatic productivity; Calculated from mass/volume; Density; DEPTH, sediment/rock; High resolution record; Holocene; Laz-17; Magnetic susceptibility; Poland; SEDCO; Sediment corer
    Type: Dataset
    Format: text/tab-separated-values, 2660 data points
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  • 62
    facet.materialart.
    Unknown
    PANGAEA
    In:  Universität Bern
    Publication Date: 2024-06-12
    Keywords: Alloxanthin; alpha-Carotene, beta,epsilon-Carotene; anoxia; Aquatic productivity; beta-Carotene, beta,beta-Carotene; Chlorophyll a; Chlorophyll b; Crocoxanthin; DEPTH, sediment/rock; Diadinoxanthin; Diatoxanthin; Echinenone; Fucoxanthin; High resolution record; Holocene; Laz-17; Neoxanthin; Phaeophytin; Pheophytin a; Pheophytin b; Poland; Pyropheophorbide a; Pyropheophytin a; Sample ID; SEDCO; Sediment corer; Violaxanthin; Zeaxanthin + Lutein
    Type: Dataset
    Format: text/tab-separated-values, 726 data points
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  • 63
    Publication Date: 2024-06-12
    Description: Soil surface temperatures were collected with help of iButtons along different transects and clusters in the North Slope of Alaska. The interval was set to 4 hours resp. 4.25 hours. Different models of iButtons were used (with a resolution of 0.0625 °C and 0.5°C resp.), see Comment.
    Keywords: AK-Land_2019_Deadhorse; AWI_Envi; AWI_Perma; AWI Arctic Land Expedition; DATE/TIME; Deadhorse_2019; Deadhorse, Alaska; Deadhorse-iButton254; DEPTH, soil; ibuttons; iButton sensor; MULT; Multiple investigations; Permafrost Research; PermaRisk; Polar Terrestrial Environmental Systems @ AWI; Simulating erosion processes in permafrost landscapes under a warming climate – a risk assessment for ecosystems and infrastructure within the Arctic; soil surface temperature; Temperature, soil
    Type: Dataset
    Format: text/tab-separated-values, 1970 data points
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  • 64
    Publication Date: 2024-06-12
    Description: Soil surface temperatures were collected with help of iButtons along different transects and clusters in the North Slope of Alaska. The interval was set to 4 hours resp. 4.25 hours. Different models of iButtons were used (with a resolution of 0.0625 °C and 0.5°C resp.), see Comment.
    Keywords: AK-Land_2019_Deadhorse; AWI_Envi; AWI_Perma; AWI Arctic Land Expedition; DATE/TIME; Deadhorse_2019; Deadhorse, Alaska; Deadhorse-iButton257; DEPTH, soil; ibuttons; iButton sensor; MULT; Multiple investigations; Permafrost Research; PermaRisk; Polar Terrestrial Environmental Systems @ AWI; Simulating erosion processes in permafrost landscapes under a warming climate – a risk assessment for ecosystems and infrastructure within the Arctic; soil surface temperature; Temperature, soil
    Type: Dataset
    Format: text/tab-separated-values, 1970 data points
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  • 65
    Publication Date: 2024-06-12
    Description: Soil surface temperatures were collected with help of iButtons along different transects and clusters in the North Slope of Alaska. The interval was set to 4 hours resp. 4.25 hours. Different models of iButtons were used (with a resolution of 0.0625 °C and 0.5°C resp.), see Comment.
    Keywords: AK-Land_2019_Deadhorse; AWI_Envi; AWI_Perma; AWI Arctic Land Expedition; DATE/TIME; Deadhorse_2019; Deadhorse, Alaska; Deadhorse-iButton262; DEPTH, soil; ibuttons; iButton sensor; MULT; Multiple investigations; Permafrost Research; PermaRisk; Polar Terrestrial Environmental Systems @ AWI; Simulating erosion processes in permafrost landscapes under a warming climate – a risk assessment for ecosystems and infrastructure within the Arctic; soil surface temperature; Temperature, soil
    Type: Dataset
    Format: text/tab-separated-values, 1954 data points
    Location Call Number Expected Availability
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  • 66
    Publication Date: 2024-06-12
    Description: Soil surface temperatures were collected with help of iButtons along different transects and clusters in the North Slope of Alaska. The interval was set to 4 hours resp. 4.25 hours. Different models of iButtons were used (with a resolution of 0.0625 °C and 0.5°C resp.), see Comment.
    Keywords: AK-Land_2019_Deadhorse; AWI_Envi; AWI_Perma; AWI Arctic Land Expedition; DATE/TIME; Deadhorse_2019; Deadhorse, Alaska; Deadhorse-iButton259; DEPTH, soil; ibuttons; iButton sensor; MULT; Multiple investigations; Permafrost Research; PermaRisk; Polar Terrestrial Environmental Systems @ AWI; Simulating erosion processes in permafrost landscapes under a warming climate – a risk assessment for ecosystems and infrastructure within the Arctic; soil surface temperature; Temperature, soil
    Type: Dataset
    Format: text/tab-separated-values, 1970 data points
    Location Call Number Expected Availability
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  • 67
    Publication Date: 2024-06-12
    Description: Soil surface temperatures were collected with help of iButtons along different transects and clusters in the North Slope of Alaska. The interval was set to 4 hours resp. 4.25 hours. Different models of iButtons were used (with a resolution of 0.0625 °C and 0.5°C resp.), see Comment.
    Keywords: AK-Land_2019_Deadhorse; AWI_Envi; AWI_Perma; AWI Arctic Land Expedition; DATE/TIME; Deadhorse_2019; Deadhorse, Alaska; Deadhorse-iButton268; DEPTH, soil; ibuttons; iButton sensor; MULT; Multiple investigations; Permafrost Research; PermaRisk; Polar Terrestrial Environmental Systems @ AWI; Simulating erosion processes in permafrost landscapes under a warming climate – a risk assessment for ecosystems and infrastructure within the Arctic; soil surface temperature; Temperature, soil
    Type: Dataset
    Format: text/tab-separated-values, 1954 data points
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  • 68
    Publication Date: 2024-06-12
    Description: Soil surface temperatures were collected with help of iButtons along different transects and clusters in the North Slope of Alaska. The interval was set to 4 hours resp. 4.25 hours. Different models of iButtons were used (with a resolution of 0.0625 °C and 0.5°C resp.), see Comment.
    Keywords: AK-Land_2019_Deadhorse; AWI_Envi; AWI_Perma; AWI Arctic Land Expedition; DATE/TIME; Deadhorse_2019; Deadhorse, Alaska; Deadhorse-iButton229; DEPTH, soil; ibuttons; iButton sensor; MULT; Multiple investigations; Permafrost Research; PermaRisk; Polar Terrestrial Environmental Systems @ AWI; Simulating erosion processes in permafrost landscapes under a warming climate – a risk assessment for ecosystems and infrastructure within the Arctic; soil surface temperature; Temperature, soil
    Type: Dataset
    Format: text/tab-separated-values, 1970 data points
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  • 69
    Publication Date: 2024-06-12
    Description: Soil surface temperatures were collected with help of iButtons along different transects and clusters in the North Slope of Alaska. The interval was set to 4 hours resp. 4.25 hours. Different models of iButtons were used (with a resolution of 0.0625 °C and 0.5°C resp.), see Comment.
    Keywords: AK-Land_2019_Deadhorse; AWI_Envi; AWI_Perma; AWI Arctic Land Expedition; DATE/TIME; Deadhorse_2019; Deadhorse, Alaska; Deadhorse-iButton269; DEPTH, soil; ibuttons; iButton sensor; MULT; Multiple investigations; Permafrost Research; PermaRisk; Polar Terrestrial Environmental Systems @ AWI; Simulating erosion processes in permafrost landscapes under a warming climate – a risk assessment for ecosystems and infrastructure within the Arctic; soil surface temperature; Temperature, soil
    Type: Dataset
    Format: text/tab-separated-values, 1954 data points
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  • 70
    Publication Date: 2024-06-12
    Description: Soil surface temperatures were collected with help of iButtons along different transects and clusters in the North Slope of Alaska. The interval was set to 4 hours resp. 4.25 hours. Different models of iButtons were used (with a resolution of 0.0625 °C and 0.5°C resp.), see Comment.
    Keywords: AK-Land_2019_Deadhorse; AWI_Envi; AWI_Perma; AWI Arctic Land Expedition; DATE/TIME; Deadhorse_2019; Deadhorse, Alaska; Deadhorse-iButton237; DEPTH, soil; ibuttons; iButton sensor; MULT; Multiple investigations; Permafrost Research; PermaRisk; Polar Terrestrial Environmental Systems @ AWI; Simulating erosion processes in permafrost landscapes under a warming climate – a risk assessment for ecosystems and infrastructure within the Arctic; soil surface temperature; Temperature, soil
    Type: Dataset
    Format: text/tab-separated-values, 1970 data points
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  • 71
    Publication Date: 2024-06-12
    Description: Soil surface temperatures were collected with help of iButtons along different transects and clusters in the North Slope of Alaska. The interval was set to 4 hours resp. 4.25 hours. Different models of iButtons were used (with a resolution of 0.0625 °C and 0.5°C resp.), see Comment.
    Keywords: AK-Land_2019_Deadhorse; AWI_Envi; AWI_Perma; AWI Arctic Land Expedition; DATE/TIME; Deadhorse_2019; Deadhorse, Alaska; Deadhorse-iButton240; DEPTH, soil; ibuttons; iButton sensor; MULT; Multiple investigations; Permafrost Research; PermaRisk; Polar Terrestrial Environmental Systems @ AWI; Simulating erosion processes in permafrost landscapes under a warming climate – a risk assessment for ecosystems and infrastructure within the Arctic; soil surface temperature; Temperature, soil
    Type: Dataset
    Format: text/tab-separated-values, 1970 data points
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  • 72
    Publication Date: 2024-06-12
    Description: Soil surface temperatures were collected with help of iButtons along different transects and clusters in the North Slope of Alaska. The interval was set to 4 hours resp. 4.25 hours. Different models of iButtons were used (with a resolution of 0.0625 °C and 0.5°C resp.), see Comment.
    Keywords: AK-Land_2019_Deadhorse; AWI_Envi; AWI_Perma; AWI Arctic Land Expedition; DATE/TIME; Deadhorse_2019; Deadhorse, Alaska; Deadhorse-iButton200; DEPTH, soil; ibuttons; iButton sensor; MULT; Multiple investigations; Permafrost Research; PermaRisk; Polar Terrestrial Environmental Systems @ AWI; Simulating erosion processes in permafrost landscapes under a warming climate – a risk assessment for ecosystems and infrastructure within the Arctic; soil surface temperature; Temperature, soil
    Type: Dataset
    Format: text/tab-separated-values, 1976 data points
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  • 73
    Publication Date: 2024-06-12
    Description: Soil surface temperatures were collected with help of iButtons along different transects and clusters in the North Slope of Alaska. The interval was set to 4 hours resp. 4.25 hours. Different models of iButtons were used (with a resolution of 0.0625 °C and 0.5°C resp.), see Comment.
    Keywords: AK-Land_2019_Deadhorse; AWI_Envi; AWI_Perma; AWI Arctic Land Expedition; DATE/TIME; Deadhorse_2019; Deadhorse, Alaska; Deadhorse-iButton202; DEPTH, soil; ibuttons; iButton sensor; MULT; Multiple investigations; Permafrost Research; PermaRisk; Polar Terrestrial Environmental Systems @ AWI; Simulating erosion processes in permafrost landscapes under a warming climate – a risk assessment for ecosystems and infrastructure within the Arctic; soil surface temperature; Temperature, soil
    Type: Dataset
    Format: text/tab-separated-values, 1976 data points
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  • 74
    Publication Date: 2024-06-12
    Description: Soil surface temperatures were collected with help of iButtons along different transects and clusters in the North Slope of Alaska. The interval was set to 4 hours resp. 4.25 hours. Different models of iButtons were used (with a resolution of 0.0625 °C and 0.5°C resp.), see Comment.
    Keywords: AK-Land_2019_Deadhorse; AWI_Envi; AWI_Perma; AWI Arctic Land Expedition; DATE/TIME; Deadhorse_2019; Deadhorse, Alaska; Deadhorse-iButton201; DEPTH, soil; ibuttons; iButton sensor; MULT; Multiple investigations; Permafrost Research; PermaRisk; Polar Terrestrial Environmental Systems @ AWI; Simulating erosion processes in permafrost landscapes under a warming climate – a risk assessment for ecosystems and infrastructure within the Arctic; soil surface temperature; Temperature, soil
    Type: Dataset
    Format: text/tab-separated-values, 1976 data points
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  • 75
    Publication Date: 2024-06-12
    Description: Soil surface temperatures were collected with help of iButtons along different transects and clusters around Churchill (Canada). The interval was set to 4 hours resp. 4.25 hours. Different models of iButtons were used (with a resolution of 0.0625 °C and 0.5°C resp.), see Comment.
    Keywords: AWI_Envi; AWI_Perma; AWI Arctic Land Expedition; CA-Land_2019_Churchill; Churchill_2019; Churchill, Canada; Churchill-iButton106; DATE/TIME; DEPTH, soil; ibuttons; iButton sensor; MULT; Multiple investigations; Permafrost Research; PermaRisk; Polar Terrestrial Environmental Systems @ AWI; Simulating erosion processes in permafrost landscapes under a warming climate – a risk assessment for ecosystems and infrastructure within the Arctic; soil surface temperature; Temperature, soil
    Type: Dataset
    Format: text/tab-separated-values, 2028 data points
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  • 76
    Publication Date: 2024-06-12
    Description: Soil surface temperatures were collected with help of iButtons along different transects and clusters around Churchill (Canada). The interval was set to 4 hours resp. 4.25 hours. Different models of iButtons were used (with a resolution of 0.0625 °C and 0.5°C resp.), see Comment.
    Keywords: AWI_Envi; AWI_Perma; AWI Arctic Land Expedition; CA-Land_2019_Churchill; Churchill_2019; Churchill, Canada; Churchill-iButton112; DATE/TIME; DEPTH, soil; ibuttons; iButton sensor; MULT; Multiple investigations; Permafrost Research; PermaRisk; Polar Terrestrial Environmental Systems @ AWI; Simulating erosion processes in permafrost landscapes under a warming climate – a risk assessment for ecosystems and infrastructure within the Arctic; soil surface temperature; Temperature, soil
    Type: Dataset
    Format: text/tab-separated-values, 2028 data points
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  • 77
    Publication Date: 2024-06-12
    Description: Soil surface temperatures were collected with help of iButtons along different transects and clusters around Churchill (Canada). The interval was set to 4 hours resp. 4.25 hours. Different models of iButtons were used (with a resolution of 0.0625 °C and 0.5°C resp.), see Comment.
    Keywords: AWI_Envi; AWI_Perma; AWI Arctic Land Expedition; CA-Land_2019_Churchill; Churchill_2019; Churchill, Canada; Churchill-iButton113; DATE/TIME; DEPTH, soil; ibuttons; iButton sensor; MULT; Multiple investigations; Permafrost Research; PermaRisk; Polar Terrestrial Environmental Systems @ AWI; Simulating erosion processes in permafrost landscapes under a warming climate – a risk assessment for ecosystems and infrastructure within the Arctic; soil surface temperature; Temperature, soil
    Type: Dataset
    Format: text/tab-separated-values, 2028 data points
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  • 78
    Publication Date: 2024-06-12
    Description: Soil surface temperatures were collected with help of iButtons along different transects and clusters around Churchill (Canada). The interval was set to 4 hours resp. 4.25 hours. Different models of iButtons were used (with a resolution of 0.0625 °C and 0.5°C resp.), see Comment.
    Keywords: AWI_Envi; AWI_Perma; AWI Arctic Land Expedition; CA-Land_2019_Churchill; Churchill_2019; Churchill, Canada; Churchill-iButton114; DATE/TIME; DEPTH, soil; ibuttons; iButton sensor; MULT; Multiple investigations; Permafrost Research; PermaRisk; Polar Terrestrial Environmental Systems @ AWI; Simulating erosion processes in permafrost landscapes under a warming climate – a risk assessment for ecosystems and infrastructure within the Arctic; soil surface temperature; Temperature, soil
    Type: Dataset
    Format: text/tab-separated-values, 2028 data points
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  • 79
    Publication Date: 2024-06-12
    Description: Soil surface temperatures were collected with help of iButtons along different transects and clusters around Churchill (Canada). The interval was set to 4 hours resp. 4.25 hours. Different models of iButtons were used (with a resolution of 0.0625 °C and 0.5°C resp.), see Comment.
    Keywords: AWI_Envi; AWI_Perma; AWI Arctic Land Expedition; CA-Land_2019_Churchill; Churchill_2019; Churchill, Canada; Churchill-iButton116; DATE/TIME; DEPTH, soil; ibuttons; iButton sensor; MULT; Multiple investigations; Permafrost Research; PermaRisk; Polar Terrestrial Environmental Systems @ AWI; Simulating erosion processes in permafrost landscapes under a warming climate – a risk assessment for ecosystems and infrastructure within the Arctic; soil surface temperature; Temperature, soil
    Type: Dataset
    Format: text/tab-separated-values, 2028 data points
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  • 80
    Publication Date: 2024-06-12
    Description: Soil surface temperatures were collected with help of iButtons along different transects and clusters around Churchill (Canada). The interval was set to 4 hours resp. 4.25 hours. Different models of iButtons were used (with a resolution of 0.0625 °C and 0.5°C resp.), see Comment.
    Keywords: AWI_Envi; AWI_Perma; AWI Arctic Land Expedition; CA-Land_2019_Churchill; Churchill_2019; Churchill, Canada; Churchill-iButton118; DATE/TIME; DEPTH, soil; ibuttons; iButton sensor; MULT; Multiple investigations; Permafrost Research; PermaRisk; Polar Terrestrial Environmental Systems @ AWI; Simulating erosion processes in permafrost landscapes under a warming climate – a risk assessment for ecosystems and infrastructure within the Arctic; soil surface temperature; Temperature, soil
    Type: Dataset
    Format: text/tab-separated-values, 2028 data points
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  • 81
    Publication Date: 2024-06-12
    Description: Soil surface temperatures were collected with help of iButtons along different transects and clusters around Churchill (Canada). The interval was set to 4 hours resp. 4.25 hours. Different models of iButtons were used (with a resolution of 0.0625 °C and 0.5°C resp.), see Comment.
    Keywords: AWI_Envi; AWI_Perma; AWI Arctic Land Expedition; CA-Land_2019_Churchill; Churchill_2019; Churchill, Canada; Churchill-iButton117; DATE/TIME; DEPTH, soil; ibuttons; iButton sensor; MULT; Multiple investigations; Permafrost Research; PermaRisk; Polar Terrestrial Environmental Systems @ AWI; Simulating erosion processes in permafrost landscapes under a warming climate – a risk assessment for ecosystems and infrastructure within the Arctic; soil surface temperature; Temperature, soil
    Type: Dataset
    Format: text/tab-separated-values, 2028 data points
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  • 82
    Publication Date: 2024-06-12
    Description: Soil surface temperatures were collected with help of iButtons along different transects and clusters around Churchill (Canada). The interval was set to 4 hours resp. 4.25 hours. Different models of iButtons were used (with a resolution of 0.0625 °C and 0.5°C resp.), see Comment.
    Keywords: AWI_Envi; AWI_Perma; AWI Arctic Land Expedition; CA-Land_2019_Churchill; Churchill_2019; Churchill, Canada; Churchill-iButton115; DATE/TIME; DEPTH, soil; ibuttons; iButton sensor; MULT; Multiple investigations; Permafrost Research; PermaRisk; Polar Terrestrial Environmental Systems @ AWI; Simulating erosion processes in permafrost landscapes under a warming climate – a risk assessment for ecosystems and infrastructure within the Arctic; soil surface temperature; Temperature, soil
    Type: Dataset
    Format: text/tab-separated-values, 2028 data points
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  • 83
    Publication Date: 2024-06-12
    Description: Soil surface temperatures were collected with help of iButtons along different transects and clusters around Churchill (Canada). The interval was set to 4 hours resp. 4.25 hours. Different models of iButtons were used (with a resolution of 0.0625 °C and 0.5°C resp.), see Comment.
    Keywords: AWI_Envi; AWI_Perma; AWI Arctic Land Expedition; CA-Land_2019_Churchill; Churchill_2019; Churchill, Canada; Churchill-iButton119; DATE/TIME; DEPTH, soil; ibuttons; iButton sensor; MULT; Multiple investigations; Permafrost Research; PermaRisk; Polar Terrestrial Environmental Systems @ AWI; Simulating erosion processes in permafrost landscapes under a warming climate – a risk assessment for ecosystems and infrastructure within the Arctic; soil surface temperature; Temperature, soil
    Type: Dataset
    Format: text/tab-separated-values, 2028 data points
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  • 84
    Publication Date: 2024-06-12
    Description: Soil surface temperatures were collected with help of iButtons along different transects and clusters around Churchill (Canada). The interval was set to 4 hours resp. 4.25 hours. Different models of iButtons were used (with a resolution of 0.0625 °C and 0.5°C resp.), see Comment.
    Keywords: AWI_Envi; AWI_Perma; AWI Arctic Land Expedition; CA-Land_2019_Churchill; Churchill_2019; Churchill, Canada; Churchill-iButton120; DATE/TIME; DEPTH, soil; ibuttons; iButton sensor; MULT; Multiple investigations; Permafrost Research; PermaRisk; Polar Terrestrial Environmental Systems @ AWI; Simulating erosion processes in permafrost landscapes under a warming climate – a risk assessment for ecosystems and infrastructure within the Arctic; soil surface temperature; Temperature, soil
    Type: Dataset
    Format: text/tab-separated-values, 2028 data points
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  • 85
    Publication Date: 2024-06-12
    Description: Permafrost thaw and ice wedge degradation lead to drastic landscape changes in the permafrost region. With this data set we investigated the cliff retreat of the Sobo-Sise Cliff (SSC), a high ice-bearing yedoma cliff in the Lena River Delta. The 1,660 m long cliff SSC extends from 72°32'34 N / 128°15'59 E to 72°32'06 N / 128°18'21 E and is located on the Sardakhskaya channel, which is one of the main Lena river branches in the Lena River Delta. Erosion rates for the SSC were determined based on satellite images from different sensors (Corona, Hexagon, Landsat, Planet cube-sat) for the period 1965-2018. Cliff front lines were manually digitized and erosion rates were calculated with the Digital Shoreline Analysis System (DSAS) tool (Himmelstoos et al. 2018). The study Fuchs et al. (2020) (DOI:10.3389/feart.2020.00336) shows that the up to 27.7 m high SSC erodes in average 15.7 m yr-1 (2015-2018). During the entire observed time period from 1965-2018, the SSC retreated in average 484 m (ranging from 322 - 680 m). This dataset includes the mean annual erosion rates of the yedoma SSC for the time periods 1965-1975, 1975-2000, 2000-2005, 2005-2010, 2010-2015, and 2015-2018, as well as the absolute cliff retreat rates over the entire period 1965-2018, which are derived from remote sensing imagery analyzed with the DSAS tool (doi:10.1594/PANGAEA.918505). Related trend data for this region, based on Landsat trend analysis are available at doi:10.1594/PANGAEA.884136 (Nitze, 2018).
    Keywords: AWI_Envi; AWI_Perma; Azimuth; CACOON; Carbon in Permafrost / Kohlenstoff im Permafrost; Changing Arctic Carbon cycle in the cOastal Ocean Near-shore; cliff erosion; Coastal retreat; Coastal retreat rate; derived from remote sensing data; digital shoreline analysis system; erosion rates; KoPF; Lena Delta; Lena Delta, Siberia, Russia; MULT; Multiple investigations; NUNATARYUK; NUNATARYUK, Permafrost thaw and the changing Arctic coast, science for socioeconomic adaptation; ORDINAL NUMBER; Permafrost; Permafrost Research; PETA-CARB; POINT DISTANCE from start; Polar Terrestrial Environmental Systems @ AWI; Rapid Permafrost Thaw in a Warming Arctic and Impacts on the Soil Organic Carbon Pool; remote sensing; river delta; Sobo-Sise_Cliff; SSC; Time series
    Type: Dataset
    Format: text/tab-separated-values, 256 data points
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  • 86
    Publication Date: 2024-06-12
    Keywords: AK-Land_2019_Deadhorse; Alaska North Slope; AWI_Perma; AWI Arctic Land Expedition; Bathymetry; DATE/TIME; Deadhorse_2019; Depth, bathymetric; LAKE; Lake_Lat_69_92_Lon_-148_78; LATITUDE; LONGITUDE; Permafrost Research; PermaRisk; Sampling lake; Simple Scan II; Simulating erosion processes in permafrost landscapes under a warming climate – a risk assessment for ecosystems and infrastructure within the Arctic; Temperature, water; thermokarst lakes
    Type: Dataset
    Format: text/tab-separated-values, 3234 data points
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  • 87
    Publication Date: 2024-06-12
    Keywords: AK-Land_2019_Deadhorse; Alaska North Slope; AWI_Perma; AWI Arctic Land Expedition; Bathymetry; DATE/TIME; Deadhorse_2019; Depth, bathymetric; LAKE; Lake_Lat_69_96_Lon_-148_73; LATITUDE; LONGITUDE; Permafrost Research; PermaRisk; Sampling lake; Simple Scan II; Simulating erosion processes in permafrost landscapes under a warming climate – a risk assessment for ecosystems and infrastructure within the Arctic; Temperature, water; thermokarst lakes
    Type: Dataset
    Format: text/tab-separated-values, 2624 data points
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  • 88
    Publication Date: 2024-06-12
    Keywords: AK-Land_2019_Deadhorse; Alaska North Slope; AWI_Perma; AWI Arctic Land Expedition; Bathymetry; DATE/TIME; Deadhorse_2019; Depth, bathymetric; LAKE; Lake_Lat_70_012_Lon_-148_662; LATITUDE; LONGITUDE; Permafrost Research; PermaRisk; Sampling lake; Simple Scan II; Simulating erosion processes in permafrost landscapes under a warming climate – a risk assessment for ecosystems and infrastructure within the Arctic; Temperature, water; thermokarst lakes
    Type: Dataset
    Format: text/tab-separated-values, 2656 data points
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  • 89
    Publication Date: 2024-06-12
    Description: This data set includes meteorological and soil temperature data obtained from two study areas in Eastern Siberia. The first study area is located at Lake Illirney in Chukotka, on a plateau above the treeline. The study site is located in a high-latitude boreal forest zone with alpine tundra above the treeline where the automatic weather station (AWS) is located. The annual average temperature is below zero degrees and results in continuous permafrost. One stand-alone Hobo logger for soil temperature measurements was installed in the soil pit next to the AWS. A second one at the subsite in a sparse larch-dominated forest with an average larch tree height of 12.5 m and 1 % cover of Salix shrubs with an average height of 0.9 m. The second study area is located in a typical boreal forest zone intermixed with some grassland for cattle grazing and shallow lakes. These boreal forest environments experience 6 to 8 months of freezing temperatures reaching extremes of -62 °C in winter and up to 35 °C between May and September. The annual average temperature is below zero degrees and results in continuous permafrost. The AWS is installed on a meadow surrounded by mixed boreal forest. The grassland is grazed by horses in summer and deforestation occurred more than 50 years ago. In addition, one stand-alone hobo logger was installed in the soil pit next to the AWS. In the forest, south of the AWS, a standalone Hobo logger was installed to record a vertical temperature profile. The forest is rather dense and mixed, with deciduous Larix gmelinii and evergreen Picea obovata. The average tree height is 12 m for larch and 5.5 m for spruce.
    Keywords: air pressure; air temperature; automatic weather station; AWI_Envi; AWI_Perma; boreal forest; hobo logger; humidity; Modular Observation Solutions for Earth Systems; MOSES; Permafrost; Permafrost Research; PermaRisk; Polar Terrestrial Environmental Systems @ AWI; precipitation; radiation data; Siberia; Simulating erosion processes in permafrost landscapes under a warming climate – a risk assessment for ecosystems and infrastructure within the Arctic; snow depth; soil temperature; wind
    Type: Dataset
    Format: application/zip, 7 datasets
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  • 90
    Publication Date: 2024-06-12
    Description: This data set contains the benthic foraminifera d18O and sediment elemental compositions of core MD10-3340 (00°30.98'S, 128°43.47'E, water depth 1094 m) with a total core length of 34.10 m and covering the last 235,000 years, retrieved from the Halmahera Sea, eastern Indonesia. The elemental compositions were measured by X-ray fluorescence (XRF) core-scanning and analyses of XRF and Inductively Coupled Plasma Mass Spectrometry (ICP-MS) on discrete samples. The original XRF core-scanned results of calcium and titanium are corrected for water content (indicated by the scanning intensity of chlorine) following the method described in the original publication.
    Keywords: benthic d18O; Halmahera Sea; Late Quaternary; Sediment Geochemistry
    Type: Dataset
    Format: application/zip, 10 datasets
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  • 91
    facet.materialart.
    Unknown
    PANGAEA
    In:  Supplement to: Yang, Xueping; Groeneveld, Jeroen; Jian, Zhimin; Steinke, Stephan; Giosan, Liviu (2020): Middle Miocene Intensification of South Asian Monsoonal Rainfall. Paleoceanography and Paleoclimatology, 35(12), e2020PA003853, https://doi.org/10.1029/2020PA003853
    Publication Date: 2024-06-12
    Description: During the middle Miocene, Earth's climate changed from a global warm period (Miocene Climatic Optimum) into a colder one with the expansion of the Antarctic ice sheet. This prominent climate transition was also a period of drastic changes in global atmospheric circulation. The development of the South Asian Monsoon (SAM) is not well understood and mainly derived from proxy records of wind strength. Proxy records for middle Miocene changes in rainfall are virtually non-existent for India and the Arabian Sea prior to 11 Ma. This study presents planktic foraminiferal trace element (Mg/Ca and Ba/Ca) and stable oxygen isotope records from NGHP-01 Site 01A off the coast of West India in the Eastern Arabian Sea (EAS) to reconstruct the regional surface hydrography and hydroclimate in the SAM region during the middle Miocene. The Ba/Ca and local seawater d18O (d18Osw) changes reveal a notable gradual increase in SAM rainfall intensity during the middle Miocene. Additionally to this long term increase in precipitation, the seawater δ18O is punctuated by a prominent decrease, i.e. freshening, at ~14 Ma contemporary with Antarctic glaciation. This suggests that Southern Ocean Intermediate Waters (SOIW) transmitted Antarctic salinity changes into the Arabian Sea via an “oceanic tunnel” mechanism. The middle Miocene increase in SAM rainfall is consistent with climate model simulations of an overall strengthening Asian monsoon from the Eocene to the middle/late Miocene with a further acceleration after the Middle Miocene climate transition.
    Keywords: adjusted; AGE; Calculated from Mg/Ca ratios (Anand et al., 2003); CDRILL; Core drilling; DEPTH, sediment/rock; Foraminifera, benthic; Foraminifera, benthic δ18O; Fragmentation index, planktic foraminifera; ICP-MS (Thermo X7); Mass spectrometer, Finnigan, MAT253; connected with Automatic carbonate preparation line, Finnigan, Kiel III; NGHP-01-01A; Sea surface temperature; Trilobatus sacculifer, Barium/Calcium ratio; Trilobatus sacculifer, Manganese/Calcium ratio; Trilobatus sacculifer, δ18O; δ18O, seawater, reconstructed
    Type: Dataset
    Format: text/tab-separated-values, 1310 data points
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  • 92
    facet.materialart.
    Unknown
    PANGAEA
    In:  Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven
    Publication Date: 2024-06-12
    Keywords: AWI_PhyOce; Bottle number; Calculated; Conductivity; CTD, SEA-BIRD SBE 911plus, SN T1526-C1222; CTD/Rosette; CTD-RO; Date/Time of event; Density, sigma-theta (0); DEPTH, water; Der Nordatlantik als Teil des Erdsystems; Elevation of event; Event label; FRAM; Fram Strait; FRontiers in Arctic marine Monitoring; Greenland - Ice Sheet/Ocean Interaction: From process understanding to an analysis of the regional system; GROCE; Latitude of event; Longitude of event; Maria S. Merian; MSM76; MSM76_100-1; MSM76_101-1; MSM76_102-1; MSM76_104-1; MSM76_105-1; MSM76_106-1; MSM76_107-1; MSM76_108-1; MSM76_109-1; MSM76_1-1; MSM76_110-1; MSM76_11-1; MSM76_111-1; MSM76_112-1; MSM76_113-1; MSM76_114-1; MSM76_115-1; MSM76_116-1; MSM76_118-1; MSM76_119-1; MSM76_120-1; MSM76_121-1; MSM76_122-1; MSM76_123-1; MSM76_124-1; MSM76_125-1; MSM76_126-1; MSM76_129-1; MSM76_130-1; MSM76_13-1; MSM76_131-1; MSM76_133-1; MSM76_134-1; MSM76_135-1; MSM76_136-1; MSM76_137-1; MSM76_138-1; MSM76_14-1; MSM76_141-1; MSM76_142-1; MSM76_143-1; MSM76_144-1; MSM76_145-1; MSM76_146-1; MSM76_147-1; MSM76_148-1; MSM76_149-1; MSM76_15-1; MSM76_16-1; MSM76_162-1; MSM76_163-1; MSM76_164-1; MSM76_165-1; MSM76_166-1; MSM76_167-1; MSM76_168-1; MSM76_169-1; MSM76_170-1; MSM76_17-1; MSM76_171-1; MSM76_172-1; MSM76_173-1; MSM76_174-1; MSM76_175-1; MSM76_176-1; MSM76_177-1; MSM76_180-1; MSM76_181-1; MSM76_182-1; MSM76_183-1; MSM76_184-1; MSM76_185-1; MSM76_186-1; MSM76_187-1; MSM76_188-1; MSM76_189-1; MSM76_190-1; MSM76_19-1; MSM76_191-1; MSM76_192-1; MSM76_193-1; MSM76_194-1; MSM76_195-1; MSM76_196-1; MSM76_197-1; MSM76_200-1; MSM76_201-1; MSM76_207-1; MSM76_208-1; MSM76_209-1; MSM76_2-1; MSM76_210-1; MSM76_211-1; MSM76_212-1; MSM76_215-1; MSM76_216-1; MSM76_218-1; MSM76_220-1; MSM76_222-1; MSM76_224-1; MSM76_24-1; MSM76_26-1; MSM76_27-1; MSM76_28-1; MSM76_29-1; MSM76_30-1; MSM76_3-1; MSM76_31-1; MSM76_32-1; MSM76_33-1; MSM76_34-1; MSM76_35-1; MSM76_36-1; MSM76_37-1; MSM76_38-1; MSM76_39-1; MSM76_40-1; MSM76_4-1; MSM76_41-1; MSM76_42-1; MSM76_43-1; MSM76_44-1; MSM76_45-1; MSM76_46-1; MSM76_47-1; MSM76_48-1; MSM76_49-1; MSM76_50-1; MSM76_5-1; MSM76_53-1; MSM76_55-1; MSM76_56-1; MSM76_57-1; MSM76_58-1; MSM76_59-1; MSM76_60-1; MSM76_6-1; MSM76_61-1; MSM76_62-1; MSM76_63-1; MSM76_64-1; MSM76_65-1; MSM76_66-1; MSM76_67-1; MSM76_68-1; MSM76_69-1; MSM76_70-1; MSM76_7-1; MSM76_71-1; MSM76_72-1; MSM76_73-1; MSM76_74-1; MSM76_75-1; MSM76_76-1; MSM76_77-1; MSM76_78-1; MSM76_79-1; MSM76_80-1; MSM76_8-1; MSM76_81-1; MSM76_82-1; MSM76_83-1; MSM76_84-1; MSM76_85-1; MSM76_86-1; MSM76_87-1; MSM76_88-1; MSM76_89-1; MSM76_90-1; MSM76_91-1; MSM76_92-1; MSM76_93-1; MSM76_94-1; MSM76_95-1; MSM76_96-1; MSM76_97-1; MSM76_98-1; MSM76_99-1; NACLIM; Nordatlantik; North Atlantic; North Atlantic Climate; Oxygen; Oxygen saturation; Oxygen sensor, SBE 43; Physical Oceanography @ AWI; Pressure, water; Priority Programme 1889 Regional Sea Level Change and Society; RACE; Regional Atlantic Circulation and global Change; Salinity; SPP1889; Temperature, water; Temperature, water, potential; TRR181; TRR181 Energy transfers in Atmosphere and Ocean
    Type: Dataset
    Format: text/tab-separated-values, 4671 data points
    Location Call Number Expected Availability
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  • 93
    facet.materialart.
    Unknown
    PANGAEA
    In:  Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven
    Publication Date: 2024-06-12
    Keywords: AWI_PhyOce; Calculated; Conductivity; CTD, SEA-BIRD SBE 911plus, SN T1526-C1222; CTD, towed system; CTD/Rosette; CTD-RO; CTD-twoyo; CTD-yoyo; Date/Time of event; Density, sigma-theta (0); DEPTH, water; Der Nordatlantik als Teil des Erdsystems; Elevation of event; Event label; FRAM; Fram Strait; FRontiers in Arctic marine Monitoring; Greenland - Ice Sheet/Ocean Interaction: From process understanding to an analysis of the regional system; GROCE; Latitude of event; Longitude of event; Maria S. Merian; MSM76; MSM76_100-1; MSM76_101-1; MSM76_102-1; MSM76_103-1; MSM76_103-10; MSM76_103-11; MSM76_103-12; MSM76_103-13; MSM76_103-14; MSM76_103-15; MSM76_103-16; MSM76_103-17; MSM76_103-18; MSM76_103-19; MSM76_103-2; MSM76_103-20; MSM76_103-21; MSM76_103-22; MSM76_103-23; MSM76_103-24; MSM76_103-25; MSM76_103-26; MSM76_103-3; MSM76_103-4; MSM76_103-5; MSM76_103-6; MSM76_103-7; MSM76_103-8; MSM76_103-9; MSM76_104-1; MSM76_105-1; MSM76_106-1; MSM76_107-1; MSM76_108-1; MSM76_109-1; MSM76_1-1; MSM76_110-1; MSM76_11-1; MSM76_111-1; MSM76_112-1; MSM76_113-1; MSM76_114-1; MSM76_115-1; MSM76_116-1; MSM76_118-1; MSM76_119-1; MSM76_120-1; MSM76_121-1; MSM76_122-1; MSM76_123-1; MSM76_124-1; MSM76_125-1; MSM76_126-1; MSM76_129-1; MSM76_130-1; MSM76_13-1; MSM76_131-1; MSM76_133-1; MSM76_134-1; MSM76_135-1; MSM76_136-1; MSM76_137-1; MSM76_138-1; MSM76_14-1; MSM76_141-1; MSM76_142-1; MSM76_143-1; MSM76_144-1; MSM76_145-1; MSM76_146-1; MSM76_147-1; MSM76_148-1; MSM76_149-1; MSM76_15-1; MSM76_154-1; MSM76_154-10; MSM76_154-11; MSM76_154-12; MSM76_154-13; MSM76_154-14; MSM76_154-15; MSM76_154-16; MSM76_154-17; MSM76_154-18; MSM76_154-19; MSM76_154-2; MSM76_154-20; MSM76_154-21; MSM76_154-22; MSM76_154-23; MSM76_154-24; MSM76_154-25; MSM76_154-26; MSM76_154-27; MSM76_154-28; MSM76_154-29; MSM76_154-3; MSM76_154-30; MSM76_154-31; MSM76_154-4; MSM76_154-5; MSM76_154-6; MSM76_154-7; MSM76_154-8; MSM76_154-9; MSM76_158-1; MSM76_158-10; MSM76_158-11; MSM76_158-12; MSM76_158-13; MSM76_158-14; MSM76_158-15; MSM76_158-16; MSM76_158-17; MSM76_158-18; MSM76_158-19; MSM76_158-2; MSM76_158-20; MSM76_158-3; MSM76_158-4; MSM76_158-5; MSM76_158-6; MSM76_158-7; MSM76_158-8; MSM76_158-9; MSM76_159-1; MSM76_159-10; MSM76_159-11; MSM76_159-12; MSM76_159-13; MSM76_159-2; MSM76_159-3; MSM76_159-4; MSM76_159-5; MSM76_159-6; MSM76_159-7; MSM76_159-8; MSM76_159-9; MSM76_16-1; MSM76_162-1; MSM76_163-1; MSM76_164-1; MSM76_165-1; MSM76_166-1; MSM76_167-1; MSM76_168-1; MSM76_169-1; MSM76_170-1; MSM76_17-1; MSM76_171-1; MSM76_172-1; MSM76_173-1; MSM76_174-1; MSM76_175-1; MSM76_176-1; MSM76_177-1; MSM76_180-1; MSM76_18-1; MSM76_181-1; MSM76_182-1; MSM76_183-1; MSM76_184-1; MSM76_185-1; MSM76_186-1; MSM76_187-1; MSM76_188-1; MSM76_189-1; MSM76_190-1; MSM76_19-1; MSM76_191-1; MSM76_192-1; MSM76_193-1; MSM76_194-1; MSM76_195-1; MSM76_196-1; MSM76_197-1; MSM76_200-1; MSM76_20-1; MSM76_201-1; MSM76_207-1; MSM76_208-1; MSM76_209-1; MSM76_2-1; MSM76_210-1; MSM76_211-1; MSM76_212-1; MSM76_215-1; MSM76_216-1; MSM76_217-1; MSM76_218-1; MSM76_219-1; MSM76_220-1; MSM76_221-1; MSM76_222-1; MSM76_223-1; MSM76_224-1; MSM76_227-1; MSM76_228-1; MSM76_229-1; MSM76_230-1; MSM76_231-1; MSM76_232-1; MSM76_233-1; MSM76_234-1; MSM76_235-1; MSM76_236-1; MSM76_237-1; MSM76_238-1; MSM76_239-1; MSM76_24-1; MSM76_25-1; MSM76_26-1; MSM76_27-1; MSM76_28-1; MSM76_29-1; MSM76_30-1; MSM76_3-1; MSM76_31-1; MSM76_32-1; MSM76_33-1; MSM76_34-1; MSM76_35-1; MSM76_36-1; MSM76_37-1; MSM76_38-1; MSM76_39-1; MSM76_40-1; MSM76_4-1; MSM76_41-1; MSM76_42-1; MSM76_43-1; MSM76_44-1; MSM76_45-1; MSM76_46-1; MSM76_47-1; MSM76_48-1; MSM76_49-1; MSM76_50-1; MSM76_5-1; MSM76_53-1; MSM76_55-1; MSM76_56-1; MSM76_57-1; MSM76_58-1; MSM76_59-1; MSM76_60-1; MSM76_6-1; MSM76_61-1; MSM76_62-1; MSM76_63-1; MSM76_64-1; MSM76_65-1; MSM76_66-1; MSM76_67-1; MSM76_68-1; MSM76_69-1; MSM76_70-1; MSM76_7-1; MSM76_71-1; MSM76_72-1; MSM76_73-1; MSM76_74-1; MSM76_75-1; MSM76_76-1; MSM76_77-1; MSM76_78-1; MSM76_79-1; MSM76_80-1; MSM76_8-1; MSM76_81-1; MSM76_82-1; MSM76_83-1; MSM76_84-1; MSM76_85-1; MSM76_86-1; MSM76_87-1; MSM76_88-1; MSM76_89-1; MSM76_90-1; MSM76_91-1; MSM76_92-1; MSM76_93-1; MSM76_94-1; MSM76_95-1; MSM76_96-1; MSM76_97-1; MSM76_98-1; MSM76_99-1; NACLIM; Nordatlantik; North Atlantic; North Atlantic Climate; Number of observations; Oxygen; Oxygen saturation; Physical Oceanography @ AWI; Pressure, water; Priority Programme 1889 Regional Sea Level Change and Society; RACE; Regional Atlantic Circulation and global Change; Salinity; SPP1889; Temperature, water; Temperature, water, potential; TRR181; TRR181 Energy transfers in Atmosphere and Ocean; Yoyo-CTD
    Type: Dataset
    Format: text/tab-separated-values, 1762191 data points
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  • 94
    Publication Date: 2024-06-12
    Description: These data represent continuous measurements of tropospheric nitryl chloride (ClNO2), dinitrogen pentoxide (N2O5), and nitric acid (HNO3) using chemical ionization mass spectrometry, and ozone (O3) using a chemiluminescence O3 monitor. The study was conducted from February 1 to March 10, 2016, at the University of Michigan in Ann Arbor, MI, USA. All measurements were conducted at 12 m above ground level.
    Keywords: Ann_Arbor_UMICH_campus_troposphere; atmospheric halogens; Chemical Ionization mass spectrometer (CIMS), THS Instruments, reagent ion I(H2O)n-; Chemiluminescence O3 monitor, 2B Technologies model 205 dual-beam; ClNO2; DATE/TIME; Dinitrogen pentoxide; Dinitrogen pentoxide, uncertainty; MULT; Multiple investigations; N2O5; Nitric acid; Nitric acid, uncertainty; Nitryl chloride; Nitryl chloride, uncertainty; Ozone mixing ratio; wintertime air quality
    Type: Dataset
    Format: text/tab-separated-values, 38355 data points
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  • 95
    Publication Date: 2024-06-12
    Description: The data show the long-term relative sea ice lead frequencies for the Arctic (November – April 2002/03 – 2018/19) and Antarctic (April – September 2003 – 2019), respectively. The data are projected onto the coordinate grid EPSG:3413 (ARC) and ESPG:3412 (ANT) at a spatial resolution of 1 km² and are stored as NetCDF4 files. Ice surface temperature data (MYD/MOD29 col. 6 [Hall and Riggers, 2015]) from the Moderate-Resolution Imaging Spectroradiometer (MODIS) are used to derive daily observations of sea ice leads in both polar regions. Sea ice leads are defined as significant local surface temperature anomalies and they are automatically identified during a two-stage process, including 1) the tile-based retrieval of potential sea ice leads and 2) the identification of cloud artefacts using fuzzy logic (see Reiser et al., 2020 for further details [Reiser et al., 2020]). Subsequently, all daily sea ice lead maps are combined to long-term averages showing the climatological distribution of leads in the Arctic and Antarctic, respectively. The dataset represents an update for the Arctic (Willmes & Heinemann, 2016 [Willmes and Heinemann, 2016]) and is the first for the Antarctic. These maps reveal, that multiple distinct features with increased lead frequencies are present that are related to bathymetric structures, e.g. the continental shelf break or ridges and troughs.
    Keywords: Arctic; CATS; CATS - The Changing Arctic Transpolar System; Event label; File format; File name; File size; leads; pan-Antarctica; pan-Arctic; Priority Programme 1158 Antarctic Research with Comparable Investigations in Arctic Sea Ice Areas; satellite data; Sea ice; SPP1158; Uniform resource locator/link to file
    Type: Dataset
    Format: text/tab-separated-values, 8 data points
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  • 96
    Publication Date: 2024-06-12
    Description: We investigated effects of temperature during ontogeny of the kelp Laminaria digitata across haploid gametophyte and diploid sporophyte life cycle stages in 5 distinct genetic lines. We sampled meristematic discs from wild sporophytes on the island of Helgoland (North Sea; 54.1779 N, 7.8926 E) in May 2017, July 2017 and February 2018 and conducted a seasonal growth experiment at 5°C and 15°C over 14 days (experiment 1). Based on meiospores from five individuals (genetic lines) sampled in July 2017, we applied a full-factorial experimental design to generate different temperature histories by applying 5°C and 15°C during meiospore germination, gametogenesis of parental gametophytes and recruitment of offspring sporophytes (19-26 days; recruitment), and juvenile sporophyte rearing (91-122 days). We then tested for thermal plasticity among temperature history treatments at 5°C and 15°C in a final 12-day experiment assessing growth, the storage compound mannitol, carbon and nitrogen contents, and fluorometric responses in 3-4 month old sporophytes (experiment 2).
    Keywords: BiodivERsA; Biological sample; BIOS; biphasic life cycle; carry-over effect; developmental plasticity; gametogenesis; genetic variation; Helgoland_L_digitata; ontogeny; phenotypic plasticity; temperature acclimation
    Type: Dataset
    Format: application/zip, 20.2 kBytes
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  • 97
    Publication Date: 2024-06-12
    Description: Assessments of aquatic paleoproduction and pigment preservation require accurate identification and quantification of sedimentary chlorophylls. Using chromatographic techniques to analyze long records at high-resolution is impractical because they are expensive and labor intensive. We have developed a new rapid and low-cost approach to infer the concentrations of chlorophyll-a, chlorophyll-b and related chlorophyll derivatives (pheopigments-a) from the mathematical decomposition of UV-VIS measured bulk spectrophotometer absorption spectra of standards and sediment extracts. We validated our method against high-performance liquid chromatography (HPLC) measurements on standard solutions and on varved, anoxic sediment from eutrophic Lake Lugano (Ponte Tresa sub-basin, southern Switzerland), where the history of productivity is relatively well known for the 20th century. Our mathematical approach quantifies the concentration of chlorophyll-b (R_(ad_J)^2=0.99; RMSEP~5.9%), chlorophyll-a (R_(ad_J)^2=0.98; RMSEP~5.0%), and pyropheophorbide-a (R_(ad_J)^2=0.99; RMSEP~7.8%) in standard solutions. We obtain comparable results for total chloropigment-a (chlorophyll-a + pheopigments-a), chlorophyll-a and diagenetic products (pheopigments-a) in the sediment samples of our case study (Ponte Tresa). Here, concentrations of chl-b were too low. The pigment stratigraphy of the Ponte Tresa sediments correspond very well with the paleoproduction and eutrophication history of the 20th century. The ratio between chlorophyll-a and pheopigments-a used as a qualitative indicator of sedimentary chlorophyll preservation (chlorophyll-a / {chlorophyll-a + pheopigments-a}) is only weakly correlated with aquatic paleoproduction (radj= 0.35, p-value=0.045) and remained remarkably constant in the recent century despite strong anthropogenic eutrophication. The new method is useful for obtaining, in a cost- and time-efficient way, information about major sedimentary pigment groups which are relevant to infer paleoproduction, potentially green algae biomass, pigment preservation and early diagenetic effects.
    Keywords: aquatic paleoproduction; Chlorophylls Preservation Index; deconvolution; File format; File name; File size; Lake_Lugano; Sedimentary pigments; Switzerland; Uniform resource locator/link to file; UV-VIS absorption spectra
    Type: Dataset
    Format: text/tab-separated-values, 28 data points
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  • 98
    Publication Date: 2024-06-12
    Description: Active layer thickness (ALT) on permafrost soils were measured with a metal rod in July/August 2018 and a year later at the same spots. The spots were nearby the Dalton Highway on the Northslope of Alaska and in the surroundings of Churchill (Manitoba, Canada).
    Keywords: Active layer depth; Active Layer Thickness; AK-Land_2019_Deadhorse; ALT; Area/locality; AWI_PerDyn; AWI Arctic Land Expedition; CA-Land_2019_Churchill; Churchill_2019; Churchill, Canada; Churchill-iButton101; Churchill-iButton102; Churchill-iButton103; Churchill-iButton104; Churchill-iButton105; Churchill-iButton106; Churchill-iButton107; Churchill-iButton108; Churchill-iButton109; Churchill-iButton110; Churchill-iButton111; Churchill-iButton112; Churchill-iButton113; Churchill-iButton114; Churchill-iButton115; Churchill-iButton116; Churchill-iButton117; Churchill-iButton118; Churchill-iButton119; Churchill-iButton120; Churchill-iButton121; Churchill-iButton122; Churchill-iButton123; Churchill-iButton124; Churchill-iButton125; Churchill-iButton126; Churchill-iButton127; Churchill-iButton128; Churchill-iButton129; Churchill-iButton130; Churchill-iButton131; Churchill-iButton132; Churchill-iButton133; Churchill-iButton134; Churchill-iButton135; Churchill-iButton136; Churchill-iButton137; Churchill-iButton138; Churchill-iButton139; Churchill-iButton140; Churchill-iButton141; Churchill-iButton142; Churchill-iButton143; Churchill-iButton144; Churchill-iButton145; Churchill-iButton146; Churchill-iButton147; Churchill-iButton148; Churchill-iButton149; Churchill-iButton150; Churchill-iButton151; Churchill-iButton152; Churchill-iButton153; Churchill-iButton154; Churchill-iButton155; Churchill-iButton156; Churchill-iButton157; Churchill-iButton158; Churchill-iButton159; Churchill-iButton160; Churchill-iButton161; Churchill-iButton162; Churchill-iButton163; Churchill-iButton164; Churchill-iButton165; Churchill-iButton166; Churchill-iButton167; Churchill-iButton168; Churchill-iButton169; Churchill-iButton170; Comment; DATE/TIME; Deadhorse_2019; Deadhorse, Alaska; Deadhorse-iButton171; Deadhorse-iButton172; Deadhorse-iButton173; Deadhorse-iButton174; Deadhorse-iButton175; Deadhorse-iButton176; Deadhorse-iButton177; Deadhorse-iButton178; Deadhorse-iButton179; Deadhorse-iButton180; Deadhorse-iButton181; Deadhorse-iButton182; Deadhorse-iButton183; Deadhorse-iButton184; Deadhorse-iButton185; Deadhorse-iButton186; Deadhorse-iButton187; Deadhorse-iButton188; Deadhorse-iButton189; Deadhorse-iButton199; Deadhorse-iButton200; Deadhorse-iButton201; Deadhorse-iButton202; Deadhorse-iButton203; Deadhorse-iButton204; Deadhorse-iButton205; Deadhorse-iButton206; Deadhorse-iButton207; Deadhorse-iButton208; Deadhorse-iButton209; Deadhorse-iButton210; Deadhorse-iButton211; Deadhorse-iButton212; Deadhorse-iButton213; Deadhorse-iButton214; Deadhorse-iButton215; Deadhorse-iButton216; Deadhorse-iButton217; Deadhorse-iButton218; Deadhorse-iButton219; Deadhorse-iButton220; Deadhorse-iButton221; Deadhorse-iButton222; Deadhorse-iButton223; Deadhorse-iButton224; Deadhorse-iButton225; Deadhorse-iButton226; Deadhorse-iButton227; Deadhorse-iButton228; Deadhorse-iButton229; Deadhorse-iButton230; Deadhorse-iButton231; Deadhorse-iButton232; Deadhorse-iButton233; Deadhorse-iButton234; Deadhorse-iButton235; Deadhorse-iButton236; Deadhorse-iButton237; Deadhorse-iButton238; Deadhorse-iButton239; Deadhorse-iButton240; Deadhorse-iButton241; Deadhorse-iButton242; Deadhorse-iButton243; Deadhorse-iButton244; Deadhorse-iButton245; Deadhorse-iButton246; Deadhorse-iButton247; Deadhorse-iButton248; Deadhorse-iButton249; Deadhorse-iButton250; Deadhorse-iButton251; Deadhorse-iButton252; Deadhorse-iButton253; Deadhorse-iButton254; Deadhorse-iButton255; Deadhorse-iButton256; Deadhorse-iButton257; Deadhorse-iButton258; Deadhorse-iButton259; Deadhorse-iButton260; Deadhorse-iButton261; Deadhorse-iButton262; Deadhorse-iButton263; Deadhorse-iButton264; Deadhorse-iButton265; Deadhorse-iButton266; Deadhorse-iButton267; Deadhorse-iButton268; Deadhorse-iButton269; Deadhorse-iButton270; Deadhorse-iButton271; Deadhorse-iButton272; Deadhorse-iButton273; Deadhorse-iButton274; Deadhorse-iButton275; Deadhorse-iButton276; Deadhorse-iButton277; Deadhorse-iButton278; Deadhorse-iButton279; Deadhorse-iButton280; Deadhorse-iButton281; Deadhorse-iButton282; Deadhorse-iButton283; Deadhorse-iButton284; Deadhorse-iButton285; Deadhorse-iButton286; Deadhorse-iButton287; Deadhorse-iButton288; Deadhorse-iButton289; Deadhorse-iButton290; Event label; Identification; LATITUDE; LONGITUDE; Metal rod; MULT; Multiple investigations; Permafrost; Permafrost Research (Periglacial Dynamics) @ AWI; PermaRisk; Simulating erosion processes in permafrost landscapes under a warming climate – a risk assessment for ecosystems and infrastructure within the Arctic
    Type: Dataset
    Format: text/tab-separated-values, 1068 data points
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  • 99
    Publication Date: 2024-06-12
    Description: This dataset represents the first ice thickness measurements at Glacier Schiaparelli in Cordillera Darwin, Southern Chile. Data were collected in April 2016 using a ground-penetrating radar (http://www.unmannedindustrial.com/sites/default/files/GPR.pdf) in the ablation area of the glacier. The ASCII file contains 5 columns with the geographical position, elevation and ice thickness interpreted from the radar data. The coordinates (WGS84/UTM 19S) were recorded using a navigator which is integrated to the radar system. The field campaign and the measurements were part of CONICYT-BMBF project GABY-VASA "Responses of Glaciers, Biosphere and Hydrology to Climate Variability across the Southern Andes".
    Keywords: DATE/TIME; ELEVATION; GABY-VASA; glaciers; GPR; GPR data; Ground-penetrating radar; ICEM; Ice measurement; ice thickness; Ice thickness, glacier; Identification; LATITUDE; LONGITUDE; Responses of Glaciers, Biosphere and Hydrology to Climate Variability and Climate Change Across the Southern Andes; Schiaparelli_Glacier; Southern Patagonia, Chile; UTM Easting, Universal Transverse Mercator; UTM Northing, Universal Transverse Mercator; UTM Zone, Universal Transverse Mercator
    Type: Dataset
    Format: text/tab-separated-values, 15870 data points
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  • 100
    Publication Date: 2024-06-12
    Keywords: DEPTH, sediment/rock; Foraminifera, planktic δ13C; Foraminifera, planktic δ18O; GC; GeoB20616-1; Gravity corer; M123; M123_175-1; Meteor (1986); TRACES; Tracing Human and Climate impacts in South Africa
    Type: Dataset
    Format: text/tab-separated-values, 56 data points
    Location Call Number Expected Availability
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