Origin and fate of the Chukchi Slope Current using a numerical model and in-situ data
Author Posting. © American Geophysical Union, 2021. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Journal of Geophysical Research: Oceans 126(5), (2021): e2021JC017291, https://doi.org/10.1029...
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ftwhoas:oai:darchive.mblwhoilibrary.org:1912/27527 2023-05-15T15:40:39+02:00 Origin and fate of the Chukchi Slope Current using a numerical model and in-situ data Leng, Hengling Spall, Michael A. Pickart, Robert S. Lin, Peigen Bai, Xuezhi 2021-04-29 https://hdl.handle.net/1912/27527 unknown American Geophysical Union https://doi.org/10.1029/2021JC017291 Leng, H., Spall, M. A., Pickart, R. S., Lin, P., & Bai, X. (2021). Origin and fate of the Chukchi Slope Current using a numerical model and in-situ data. Journal of Geophysical Research: Oceans, 126(5), e2021JC017291. https://hdl.handle.net/1912/27527 doi:10.1029/2021JC017291 Leng, H., Spall, M. A., Pickart, R. S., Lin, P., & Bai, X. (2021). Origin and fate of the Chukchi Slope Current using a numerical model and in-situ data. Journal of Geophysical Research: Oceans, 126(5), e2021JC017291. doi:10.1029/2021JC017291 Article 2021 ftwhoas https://doi.org/10.1029/2021JC017291 2022-05-28T23:04:17Z Author Posting. © American Geophysical Union, 2021. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Journal of Geophysical Research: Oceans 126(5), (2021): e2021JC017291, https://doi.org/10.1029/2021JC017291. A regional coupled sea ice-ocean model and mooring/shipboard measurements are used to investigate the origins, seasonality, and downstream fate of the Chukchi Slope Current (CSC). Three years (2013–2015) of model integration indicates that, in the mean, the model slope current transports ∼0.45 Sv of Pacific water northwestward along the Chukchi continental slope. Only 62% of this water emanates from Barrow Canyon, while the rest (38%) is fed by a westward jet extending from the southern Beaufort Sea. The jet merges with the outflow from the canyon, forming the CSC. Due to these two distinct origins, the slope current in the model has a double velocity core at times. This is consistent with the double-core structure of the slope current seen in ship-based observations. Seasonal changes in the volume, heat, and freshwater transports by the slope current appear to be related to the changes in the upstream flows. A tracer diagnostic in the model suggests that the part of the slope current over the upper continental slope continues westward toward the East Siberian Sea, while the portion of the current overlying deeper isobaths flows northward into the Chukchi Borderland, where it ultimately gets entrained into the Beaufort Gyre. Our study provides a detailed and complete picture of the slope current. This work was funded by the National Key Research and Development Program of China (Grant 2017YFA0604600), the Fundamental Research Funds for the Central Universities (Grant 2019B81214), the National Natural Science Foundation of China (Grant 41676019), the Postgraduate Research & Practice Innovation Program of Jiangsu Province (Grant KYCX19_0384), the National Science Foundation (Grants OPP-1822334, ... Article in Journal/Newspaper Beaufort Sea Chukchi East Siberian Sea Sea ice Woods Hole Scientific Community: WHOAS (Woods Hole Open Access Server) Barrow Canyon ENVELOPE(-154.000,-154.000,72.500,72.500) Chukchi Borderland ENVELOPE(-165.000,-165.000,77.000,77.000) East Siberian Sea ENVELOPE(166.000,166.000,74.000,74.000) Pacific Journal of Geophysical Research: Oceans 126 5 |
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Woods Hole Scientific Community: WHOAS (Woods Hole Open Access Server) |
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description |
Author Posting. © American Geophysical Union, 2021. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Journal of Geophysical Research: Oceans 126(5), (2021): e2021JC017291, https://doi.org/10.1029/2021JC017291. A regional coupled sea ice-ocean model and mooring/shipboard measurements are used to investigate the origins, seasonality, and downstream fate of the Chukchi Slope Current (CSC). Three years (2013–2015) of model integration indicates that, in the mean, the model slope current transports ∼0.45 Sv of Pacific water northwestward along the Chukchi continental slope. Only 62% of this water emanates from Barrow Canyon, while the rest (38%) is fed by a westward jet extending from the southern Beaufort Sea. The jet merges with the outflow from the canyon, forming the CSC. Due to these two distinct origins, the slope current in the model has a double velocity core at times. This is consistent with the double-core structure of the slope current seen in ship-based observations. Seasonal changes in the volume, heat, and freshwater transports by the slope current appear to be related to the changes in the upstream flows. A tracer diagnostic in the model suggests that the part of the slope current over the upper continental slope continues westward toward the East Siberian Sea, while the portion of the current overlying deeper isobaths flows northward into the Chukchi Borderland, where it ultimately gets entrained into the Beaufort Gyre. Our study provides a detailed and complete picture of the slope current. This work was funded by the National Key Research and Development Program of China (Grant 2017YFA0604600), the Fundamental Research Funds for the Central Universities (Grant 2019B81214), the National Natural Science Foundation of China (Grant 41676019), the Postgraduate Research & Practice Innovation Program of Jiangsu Province (Grant KYCX19_0384), the National Science Foundation (Grants OPP-1822334, ... |
format |
Article in Journal/Newspaper |
author |
Leng, Hengling Spall, Michael A. Pickart, Robert S. Lin, Peigen Bai, Xuezhi |
spellingShingle |
Leng, Hengling Spall, Michael A. Pickart, Robert S. Lin, Peigen Bai, Xuezhi Origin and fate of the Chukchi Slope Current using a numerical model and in-situ data |
author_facet |
Leng, Hengling Spall, Michael A. Pickart, Robert S. Lin, Peigen Bai, Xuezhi |
author_sort |
Leng, Hengling |
title |
Origin and fate of the Chukchi Slope Current using a numerical model and in-situ data |
title_short |
Origin and fate of the Chukchi Slope Current using a numerical model and in-situ data |
title_full |
Origin and fate of the Chukchi Slope Current using a numerical model and in-situ data |
title_fullStr |
Origin and fate of the Chukchi Slope Current using a numerical model and in-situ data |
title_full_unstemmed |
Origin and fate of the Chukchi Slope Current using a numerical model and in-situ data |
title_sort |
origin and fate of the chukchi slope current using a numerical model and in-situ data |
publisher |
American Geophysical Union |
publishDate |
2021 |
url |
https://hdl.handle.net/1912/27527 |
long_lat |
ENVELOPE(-154.000,-154.000,72.500,72.500) ENVELOPE(-165.000,-165.000,77.000,77.000) ENVELOPE(166.000,166.000,74.000,74.000) |
geographic |
Barrow Canyon Chukchi Borderland East Siberian Sea Pacific |
geographic_facet |
Barrow Canyon Chukchi Borderland East Siberian Sea Pacific |
genre |
Beaufort Sea Chukchi East Siberian Sea Sea ice |
genre_facet |
Beaufort Sea Chukchi East Siberian Sea Sea ice |
op_source |
Leng, H., Spall, M. A., Pickart, R. S., Lin, P., & Bai, X. (2021). Origin and fate of the Chukchi Slope Current using a numerical model and in-situ data. Journal of Geophysical Research: Oceans, 126(5), e2021JC017291. doi:10.1029/2021JC017291 |
op_relation |
https://doi.org/10.1029/2021JC017291 Leng, H., Spall, M. A., Pickart, R. S., Lin, P., & Bai, X. (2021). Origin and fate of the Chukchi Slope Current using a numerical model and in-situ data. Journal of Geophysical Research: Oceans, 126(5), e2021JC017291. https://hdl.handle.net/1912/27527 doi:10.1029/2021JC017291 |
op_doi |
https://doi.org/10.1029/2021JC017291 |
container_title |
Journal of Geophysical Research: Oceans |
container_volume |
126 |
container_issue |
5 |
_version_ |
1766373411499540480 |