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  • 1; 10; 11; 12; 13; 14; 15; 16; 17; 18; 2; 3; 4; 5; 6; 7; 8; 9; AC3; Arctic; Arctic Amplification; CFC12; Date/Time of event; DEPTH, ice/snow; Event label; Helium; Latitude of event; Longitude of event; MOSAiC; MOSAIC_PO; MOSAiC20192020; MOSAiC expedition; Multidisciplinary drifting Observatory for the Study of Arctic Climate; NEON; Polarstern; PS122/3; PS122/3_99-100; PS122/3_99-101; PS122/3_99-102; PS122/3_99-103; PS122/3_99-104; PS122/3_99-105; PS122/3_99-106; PS122/3_99-107; PS122/3_99-108; PS122/3_99-109; PS122/3_99-110; PS122/3_99-111; PS122/3_99-112; PS122/3_99-95; PS122/3_99-96; PS122/3_99-97; PS122/3_99-98; PS122/3_99-99; Quality flag; Sample ID; SF6; SNOW; Snow/ice sample; tracer; tritium; Tritium; Ultra high vacuum (UHV) mass spectrometry; World Oceans Circulation Experiment (WOCE) quality flags according to Jiang et al. (2022)  (1)
  • 551.46  (1)
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  • 1
    Publication Date: 2021-10-01
    Description: Low-mode internal waves propagate over large distances and provide energy for turbulent mixing when they break far from their generation sites. A realistic representation of the oceanic energy cycle in ocean and climate models requires a consistent implementation of their generation, propagation, and dissipation. Here we combine the long-term mean energy flux from satellite altimetry with results from a 1/10° global ocean general circulation model that resolves the low modes of internal waves and in situ observations of stratification and horizontal currents to study energy flux and dissipation along a 1000 km internal tide beam in the eastern North Atlantic. Internal wave fluxes were estimated from twelve 36- to 48-hr stations in along- and across-beam direction to resolve both the inertial period and tidal cycle. The observed internal tide energy fluxes range from 5.9 kW m−1 near the generation sites to 0.5 kW m−1 at distant stations. Estimates of energy dissipation come from both finestructure and upper ocean microstructure profiles and range, vertically integrated, from 0.5 to 3.3 mW m−2 along the beam. Overall, the in situ observations confirm the internal tide pattern derived from satellite altimetry, but the in situ energy fluxes are more variable and decrease less monotonically along the beam. Internal tides in the model propagate over shorter distances compared to results from altimetry and in situ measurements, but more spatial details close the main generation sites are resolved.
    Keywords: 551.46 ; internal tide ; energy flux ; energy dissipation
    Language: English
    Type: map
    Location Call Number Limitation Availability
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  • 2
    Publication Date: 2024-04-13
    Description: We present a data set of tritium in snow collected during the Multidisciplinary drifting Observatory for the Study of Arctic Climate (MOSAiC, PS122) expedition, during which the R/V Polarstern drifted along with the Arctic sea ice from the Laptev Sea to Fram Strait, from October 2019 to September 2020. During the expedition, tritium data were collected occasionally in the snow, from the ship and from the ice. We took 9 samples from snow into 2x500 ml plastic bottles during leg 3. In the IUP Bremen noble gas lab the water samples were pre-processed with a gas extraction system for complete degassing and were then stored for several months. During that time, part of the tritium (3H) decayed by beta-decay to helium 3 (3He). The new produced 3He was then analysed by the same mass spectrometer system as for the noble gases. Tritium concentrations reported here are scaled to the 1st January 2020 and referred to as TU2020. Concentrations are given in TU (tritium unit), where 1 TU is the ratio of 1 tritium atom to 10^18 hydrogen atoms. Typical errors for this data set is 0.04TU or 3% whatever is larger. Acknowledgment These data were produced as part of the international Multidisciplinary drifting Observatory for the Study of the Arctic Climate (MOSAiC) with the tag MOSAiC20192020 (AWI_PS122_00). We thank all those who contributed to MOSAiC and made this endeavor possible, as listed in Nixdorf et al. (2021). CH was funded by Vetenskapsrådet grant number 2018-03859 awarded to CH, project Why is the deep Arctic Ocean Warming? (WAOW), and acknowledge support from the Swedish Polar Research Secretariat for berth fees onboard MOSAiC. MW gratefully acknowledge the funding by the Deutsche Forschungsgemeinschaft (DFG, German Research Foundation) – Project Number 268020496–TRR 172, within the Transregional Collaborative Research Center "ArctiC Amplification: Climate Relevant Atmospheric and SurfaCe Processes, and Feedback Mechanisms (AC)3.
    Keywords: 1; 10; 11; 12; 13; 14; 15; 16; 17; 18; 2; 3; 4; 5; 6; 7; 8; 9; AC3; Arctic; Arctic Amplification; CFC12; Date/Time of event; DEPTH, ice/snow; Event label; Helium; Latitude of event; Longitude of event; MOSAiC; MOSAIC_PO; MOSAiC20192020; MOSAiC expedition; Multidisciplinary drifting Observatory for the Study of Arctic Climate; NEON; Polarstern; PS122/3; PS122/3_99-100; PS122/3_99-101; PS122/3_99-102; PS122/3_99-103; PS122/3_99-104; PS122/3_99-105; PS122/3_99-106; PS122/3_99-107; PS122/3_99-108; PS122/3_99-109; PS122/3_99-110; PS122/3_99-111; PS122/3_99-112; PS122/3_99-95; PS122/3_99-96; PS122/3_99-97; PS122/3_99-98; PS122/3_99-99; Quality flag; Sample ID; SF6; SNOW; Snow/ice sample; tracer; tritium; Tritium; Ultra high vacuum (UHV) mass spectrometry; World Oceans Circulation Experiment (WOCE) quality flags according to Jiang et al. (2022)
    Type: Dataset
    Format: text/tab-separated-values, 54 data points
    Location Call Number Limitation Availability
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