Warm and moist air intrusions into the winter Arctic: a Lagrangian view on the near-surface energy budgets
In this study, warm and moist air intrusions (WaMAIs) over the Arctic Ocean sectors of Barents Sea, Kara Sea, Laptev Sea, East Siberian Sea, Chukchi Sea, and Beaufort Sea in 40 recent winters (from 1979 to 2018) are identified from the ERA5 reanalysis using both Eulerian and Lagrangian views. The an...
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Copernicus Publications
2022
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ftnonlinearchiv:oai:noa.gwlb.de:cop_mods_00061589 2023-05-15T14:53:04+02:00 Warm and moist air intrusions into the winter Arctic: a Lagrangian view on the near-surface energy budgets You, Cheng Tjernström, Michael Devasthale, Abhay 2022-06 electronic https://doi.org/10.5194/acp-22-8037-2022 https://noa.gwlb.de/receive/cop_mods_00061589 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00061033/acp-22-8037-2022.pdf https://acp.copernicus.org/articles/22/8037/2022/acp-22-8037-2022.pdf eng eng Copernicus Publications Atmospheric Chemistry and Physics -- http://www.atmos-chem-phys.net/volumes_and_issues.html -- http://www.bibliothek.uni-regensburg.de/ezeit/?2069847 -- 1680-7324 https://doi.org/10.5194/acp-22-8037-2022 https://noa.gwlb.de/receive/cop_mods_00061589 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00061033/acp-22-8037-2022.pdf https://acp.copernicus.org/articles/22/8037/2022/acp-22-8037-2022.pdf https://creativecommons.org/licenses/by/4.0/ uneingeschränkt info:eu-repo/semantics/openAccess CC-BY article Verlagsveröffentlichung article Text doc-type:article 2022 ftnonlinearchiv https://doi.org/10.5194/acp-22-8037-2022 2022-06-26T23:11:40Z In this study, warm and moist air intrusions (WaMAIs) over the Arctic Ocean sectors of Barents Sea, Kara Sea, Laptev Sea, East Siberian Sea, Chukchi Sea, and Beaufort Sea in 40 recent winters (from 1979 to 2018) are identified from the ERA5 reanalysis using both Eulerian and Lagrangian views. The analysis shows that WaMAIs, fueled by Arctic blocking, cause a relative surface warming and hence a sea-ice reduction by exerting positive anomalies of net thermal irradiances and turbulent fluxes on the surface. Over Arctic Ocean sectors with land-locked sea ice in winter, such as Laptev Sea, East Siberian Sea, Chukchi Sea, and Beaufort Sea, the total surface energy-budget is dominated by net thermal irradiance. From a Lagrangian perspective, total water path (TWP) increases linearly with the downstream distance from the sea-ice edge over the completely ice-covered sectors, inducing almost linearly increasing net thermal irradiance and total surface energy-budget. However, over the Barents Sea, with an open ocean to the south, total net surface energy-budget is dominated by the surface turbulent flux. With the energy in the warm-and-moist air continuously transported to the surface, net surface turbulent flux gradually decreases with distance, especially within the first 2∘ north of the ice edge, inducing a decreasing but still positive total surface energy-budget. The boundary-layer energy-budget patterns over the Barents Sea can be categorized into three classes: radiation-dominated, turbulence-dominated, and turbulence-dominated with cold dome, comprising about 52 %, 40 %, and 8 % of all WaMAIs, respectively. Statistically, turbulence-dominated cases with or without cold dome occur along with 1 order of magnitude larger large-scale subsidence than the radiation-dominated cases. For the turbulence-dominated category, larger turbulent fluxes are exerted to the surface, probably because of stronger wind shear. In radiation-dominated WaMAIs, stratocumulus develops more strongly and triggers intensive cloud-top radiative ... Article in Journal/Newspaper Arctic Arctic Ocean Barents Sea Beaufort Sea Chukchi Chukchi Sea East Siberian Sea Kara Sea laptev Laptev Sea Sea ice Niedersächsisches Online-Archiv NOA Arctic Arctic Ocean Barents Sea Chukchi Sea East Siberian Sea ENVELOPE(166.000,166.000,74.000,74.000) Kara Sea Laptev Sea Atmospheric Chemistry and Physics 22 12 8037 8057 |
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Open Polar |
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Niedersächsisches Online-Archiv NOA |
op_collection_id |
ftnonlinearchiv |
language |
English |
topic |
article Verlagsveröffentlichung |
spellingShingle |
article Verlagsveröffentlichung You, Cheng Tjernström, Michael Devasthale, Abhay Warm and moist air intrusions into the winter Arctic: a Lagrangian view on the near-surface energy budgets |
topic_facet |
article Verlagsveröffentlichung |
description |
In this study, warm and moist air intrusions (WaMAIs) over the Arctic Ocean sectors of Barents Sea, Kara Sea, Laptev Sea, East Siberian Sea, Chukchi Sea, and Beaufort Sea in 40 recent winters (from 1979 to 2018) are identified from the ERA5 reanalysis using both Eulerian and Lagrangian views. The analysis shows that WaMAIs, fueled by Arctic blocking, cause a relative surface warming and hence a sea-ice reduction by exerting positive anomalies of net thermal irradiances and turbulent fluxes on the surface. Over Arctic Ocean sectors with land-locked sea ice in winter, such as Laptev Sea, East Siberian Sea, Chukchi Sea, and Beaufort Sea, the total surface energy-budget is dominated by net thermal irradiance. From a Lagrangian perspective, total water path (TWP) increases linearly with the downstream distance from the sea-ice edge over the completely ice-covered sectors, inducing almost linearly increasing net thermal irradiance and total surface energy-budget. However, over the Barents Sea, with an open ocean to the south, total net surface energy-budget is dominated by the surface turbulent flux. With the energy in the warm-and-moist air continuously transported to the surface, net surface turbulent flux gradually decreases with distance, especially within the first 2∘ north of the ice edge, inducing a decreasing but still positive total surface energy-budget. The boundary-layer energy-budget patterns over the Barents Sea can be categorized into three classes: radiation-dominated, turbulence-dominated, and turbulence-dominated with cold dome, comprising about 52 %, 40 %, and 8 % of all WaMAIs, respectively. Statistically, turbulence-dominated cases with or without cold dome occur along with 1 order of magnitude larger large-scale subsidence than the radiation-dominated cases. For the turbulence-dominated category, larger turbulent fluxes are exerted to the surface, probably because of stronger wind shear. In radiation-dominated WaMAIs, stratocumulus develops more strongly and triggers intensive cloud-top radiative ... |
format |
Article in Journal/Newspaper |
author |
You, Cheng Tjernström, Michael Devasthale, Abhay |
author_facet |
You, Cheng Tjernström, Michael Devasthale, Abhay |
author_sort |
You, Cheng |
title |
Warm and moist air intrusions into the winter Arctic: a Lagrangian view on the near-surface energy budgets |
title_short |
Warm and moist air intrusions into the winter Arctic: a Lagrangian view on the near-surface energy budgets |
title_full |
Warm and moist air intrusions into the winter Arctic: a Lagrangian view on the near-surface energy budgets |
title_fullStr |
Warm and moist air intrusions into the winter Arctic: a Lagrangian view on the near-surface energy budgets |
title_full_unstemmed |
Warm and moist air intrusions into the winter Arctic: a Lagrangian view on the near-surface energy budgets |
title_sort |
warm and moist air intrusions into the winter arctic: a lagrangian view on the near-surface energy budgets |
publisher |
Copernicus Publications |
publishDate |
2022 |
url |
https://doi.org/10.5194/acp-22-8037-2022 https://noa.gwlb.de/receive/cop_mods_00061589 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00061033/acp-22-8037-2022.pdf https://acp.copernicus.org/articles/22/8037/2022/acp-22-8037-2022.pdf |
long_lat |
ENVELOPE(166.000,166.000,74.000,74.000) |
geographic |
Arctic Arctic Ocean Barents Sea Chukchi Sea East Siberian Sea Kara Sea Laptev Sea |
geographic_facet |
Arctic Arctic Ocean Barents Sea Chukchi Sea East Siberian Sea Kara Sea Laptev Sea |
genre |
Arctic Arctic Ocean Barents Sea Beaufort Sea Chukchi Chukchi Sea East Siberian Sea Kara Sea laptev Laptev Sea Sea ice |
genre_facet |
Arctic Arctic Ocean Barents Sea Beaufort Sea Chukchi Chukchi Sea East Siberian Sea Kara Sea laptev Laptev Sea Sea ice |
op_relation |
Atmospheric Chemistry and Physics -- http://www.atmos-chem-phys.net/volumes_and_issues.html -- http://www.bibliothek.uni-regensburg.de/ezeit/?2069847 -- 1680-7324 https://doi.org/10.5194/acp-22-8037-2022 https://noa.gwlb.de/receive/cop_mods_00061589 https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00061033/acp-22-8037-2022.pdf https://acp.copernicus.org/articles/22/8037/2022/acp-22-8037-2022.pdf |
op_rights |
https://creativecommons.org/licenses/by/4.0/ uneingeschränkt info:eu-repo/semantics/openAccess |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.5194/acp-22-8037-2022 |
container_title |
Atmospheric Chemistry and Physics |
container_volume |
22 |
container_issue |
12 |
container_start_page |
8037 |
op_container_end_page |
8057 |
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1766324484365615104 |