Heat, salt, and volume transports in the eastern Eurasian Basin of the Arctic Ocean from 2 years of mooring observations
This study discusses along-slope volume, heat, and salt transports derived from observations collected in 2013–2015 using a cross-slope array of six moorings ranging from 250 to 3900 m in the eastern Eurasian Basin (EB) of the Arctic Ocean. These observations demonstrate that in the upper 780 m laye...
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ftcopernicus:oai:publications.copernicus.org:os67430 2023-05-15T15:05:53+02:00 Heat, salt, and volume transports in the eastern Eurasian Basin of the Arctic Ocean from 2 years of mooring observations Pnyushkov, Andrey V. Polyakov, Igor V. Rember, Robert Ivanov, Vladimir V. Alkire, Matthew B. Ashik, Igor M. Baumann, Till M. Alekseev, Genrikh V. Sundfjord, Arild 2018-11-30 application/pdf https://doi.org/10.5194/os-14-1349-2018 https://os.copernicus.org/articles/14/1349/2018/ eng eng doi:10.5194/os-14-1349-2018 https://os.copernicus.org/articles/14/1349/2018/ eISSN: 1812-0792 Text 2018 ftcopernicus https://doi.org/10.5194/os-14-1349-2018 2020-07-20T16:23:04Z This study discusses along-slope volume, heat, and salt transports derived from observations collected in 2013–2015 using a cross-slope array of six moorings ranging from 250 to 3900 m in the eastern Eurasian Basin (EB) of the Arctic Ocean. These observations demonstrate that in the upper 780 m layer, the along-slope boundary current advected, on average, 5.1±0.1 Sv of water, predominantly in the eastward (shallow-to-right) direction. Monthly net volume transports across the Laptev Sea slope vary widely, from <math xmlns="http://www.w3.org/1998/Math/MathML" id="M2" display="inline" overflow="scroll" dspmath="mathml"><mrow><mo>∼</mo><mn mathvariant="normal">0.3</mn><mo>±</mo><mn mathvariant="normal">0.8</mn></mrow></math> <svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="54pt" height="10pt" class="svg-formula" dspmath="mathimg" md5hash="ce0352cb99ace134c91fc8ed9607d24f"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="os-14-1349-2018-ie00001.svg" width="54pt" height="10pt" src="os-14-1349-2018-ie00001.png"/></svg:svg> in April 2014 to <math xmlns="http://www.w3.org/1998/Math/MathML" id="M3" display="inline" overflow="scroll" dspmath="mathml"><mrow><mo>∼</mo><mn mathvariant="normal">9.9</mn><mo>±</mo><mn mathvariant="normal">0.8</mn></mrow></math> <svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="54pt" height="10pt" class="svg-formula" dspmath="mathimg" md5hash="6b60514a27b9d442ef200248e4e5a41e"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="os-14-1349-2018-ie00002.svg" width="54pt" height="10pt" src="os-14-1349-2018-ie00002.png"/></svg:svg> Sv in June 2014; 3.1±0.1 Sv (or 60 %) of the net transport was associated with warm and salty intermediate-depth Atlantic Water (AW). Calculated heat transport for 2013–2015 (relative to −1.8 ∘ C) was 46.0±1.7 TW, and net salt transport (relative to zero salinity) was 172±6 Mkg s −1 . Estimates for AW heat and salt transports were 32.7±1.3 TW (71 % of net heat transport) and 112±4 Mkg s −1 (65 % of net salt transport). The variability of currents explains ∼90 % of the variability in the heat and salt transports. The remaining ∼10 % is controlled by temperature and salinity anomalies together with the temporal variability of the AW layer thickness. The annual mean volume transports decreased by 25 % from 5.8±0.2 Sv in 2013–2014 to 4.4±0.2 Sv in 2014–2015, suggesting that changes in the transports at interannual and longer timescales in the eastern EB may be significant. Text Arctic Arctic Ocean laptev Laptev Sea Copernicus Publications: E-Journals Arctic Arctic Ocean Laptev Sea Ocean Science 14 6 1349 1371 |
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Open Polar |
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Copernicus Publications: E-Journals |
op_collection_id |
ftcopernicus |
language |
English |
description |
This study discusses along-slope volume, heat, and salt transports derived from observations collected in 2013–2015 using a cross-slope array of six moorings ranging from 250 to 3900 m in the eastern Eurasian Basin (EB) of the Arctic Ocean. These observations demonstrate that in the upper 780 m layer, the along-slope boundary current advected, on average, 5.1±0.1 Sv of water, predominantly in the eastward (shallow-to-right) direction. Monthly net volume transports across the Laptev Sea slope vary widely, from <math xmlns="http://www.w3.org/1998/Math/MathML" id="M2" display="inline" overflow="scroll" dspmath="mathml"><mrow><mo>∼</mo><mn mathvariant="normal">0.3</mn><mo>±</mo><mn mathvariant="normal">0.8</mn></mrow></math> <svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="54pt" height="10pt" class="svg-formula" dspmath="mathimg" md5hash="ce0352cb99ace134c91fc8ed9607d24f"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="os-14-1349-2018-ie00001.svg" width="54pt" height="10pt" src="os-14-1349-2018-ie00001.png"/></svg:svg> in April 2014 to <math xmlns="http://www.w3.org/1998/Math/MathML" id="M3" display="inline" overflow="scroll" dspmath="mathml"><mrow><mo>∼</mo><mn mathvariant="normal">9.9</mn><mo>±</mo><mn mathvariant="normal">0.8</mn></mrow></math> <svg:svg xmlns:svg="http://www.w3.org/2000/svg" width="54pt" height="10pt" class="svg-formula" dspmath="mathimg" md5hash="6b60514a27b9d442ef200248e4e5a41e"><svg:image xmlns:xlink="http://www.w3.org/1999/xlink" xlink:href="os-14-1349-2018-ie00002.svg" width="54pt" height="10pt" src="os-14-1349-2018-ie00002.png"/></svg:svg> Sv in June 2014; 3.1±0.1 Sv (or 60 %) of the net transport was associated with warm and salty intermediate-depth Atlantic Water (AW). Calculated heat transport for 2013–2015 (relative to −1.8 ∘ C) was 46.0±1.7 TW, and net salt transport (relative to zero salinity) was 172±6 Mkg s −1 . Estimates for AW heat and salt transports were 32.7±1.3 TW (71 % of net heat transport) and 112±4 Mkg s −1 (65 % of net salt transport). The variability of currents explains ∼90 % of the variability in the heat and salt transports. The remaining ∼10 % is controlled by temperature and salinity anomalies together with the temporal variability of the AW layer thickness. The annual mean volume transports decreased by 25 % from 5.8±0.2 Sv in 2013–2014 to 4.4±0.2 Sv in 2014–2015, suggesting that changes in the transports at interannual and longer timescales in the eastern EB may be significant. |
format |
Text |
author |
Pnyushkov, Andrey V. Polyakov, Igor V. Rember, Robert Ivanov, Vladimir V. Alkire, Matthew B. Ashik, Igor M. Baumann, Till M. Alekseev, Genrikh V. Sundfjord, Arild |
spellingShingle |
Pnyushkov, Andrey V. Polyakov, Igor V. Rember, Robert Ivanov, Vladimir V. Alkire, Matthew B. Ashik, Igor M. Baumann, Till M. Alekseev, Genrikh V. Sundfjord, Arild Heat, salt, and volume transports in the eastern Eurasian Basin of the Arctic Ocean from 2 years of mooring observations |
author_facet |
Pnyushkov, Andrey V. Polyakov, Igor V. Rember, Robert Ivanov, Vladimir V. Alkire, Matthew B. Ashik, Igor M. Baumann, Till M. Alekseev, Genrikh V. Sundfjord, Arild |
author_sort |
Pnyushkov, Andrey V. |
title |
Heat, salt, and volume transports in the eastern Eurasian Basin of the Arctic Ocean from 2 years of mooring observations |
title_short |
Heat, salt, and volume transports in the eastern Eurasian Basin of the Arctic Ocean from 2 years of mooring observations |
title_full |
Heat, salt, and volume transports in the eastern Eurasian Basin of the Arctic Ocean from 2 years of mooring observations |
title_fullStr |
Heat, salt, and volume transports in the eastern Eurasian Basin of the Arctic Ocean from 2 years of mooring observations |
title_full_unstemmed |
Heat, salt, and volume transports in the eastern Eurasian Basin of the Arctic Ocean from 2 years of mooring observations |
title_sort |
heat, salt, and volume transports in the eastern eurasian basin of the arctic ocean from 2 years of mooring observations |
publishDate |
2018 |
url |
https://doi.org/10.5194/os-14-1349-2018 https://os.copernicus.org/articles/14/1349/2018/ |
geographic |
Arctic Arctic Ocean Laptev Sea |
geographic_facet |
Arctic Arctic Ocean Laptev Sea |
genre |
Arctic Arctic Ocean laptev Laptev Sea |
genre_facet |
Arctic Arctic Ocean laptev Laptev Sea |
op_source |
eISSN: 1812-0792 |
op_relation |
doi:10.5194/os-14-1349-2018 https://os.copernicus.org/articles/14/1349/2018/ |
op_doi |
https://doi.org/10.5194/os-14-1349-2018 |
container_title |
Ocean Science |
container_volume |
14 |
container_issue |
6 |
container_start_page |
1349 |
op_container_end_page |
1371 |
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1766337570136915968 |