Warm-Air Advection Over Melting Sea-Ice: A Lagrangian Case Study
Abstract Observations from the 2014 Arctic Clouds in Summer Experiment indicate that, in summer, warm-air advection over melting sea-ice results in a strong surface melting feedback forced by a very strong surface-based temperature inversion and fog formation exerting additional heat flux on the sur...
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Online Access: | http://dx.doi.org/10.1007/s10546-020-00590-1 http://link.springer.com/content/pdf/10.1007/s10546-020-00590-1.pdf http://link.springer.com/article/10.1007/s10546-020-00590-1/fulltext.html |
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crspringernat:10.1007/s10546-020-00590-1 2023-05-15T14:54:09+02:00 Warm-Air Advection Over Melting Sea-Ice: A Lagrangian Case Study You, Cheng Tjernström, Michael Devasthale, Abhay Stockholm University 2020 http://dx.doi.org/10.1007/s10546-020-00590-1 http://link.springer.com/content/pdf/10.1007/s10546-020-00590-1.pdf http://link.springer.com/article/10.1007/s10546-020-00590-1/fulltext.html en eng Springer Science and Business Media LLC https://creativecommons.org/licenses/by/4.0 https://creativecommons.org/licenses/by/4.0 CC-BY Boundary-Layer Meteorology volume 179, issue 1, page 99-116 ISSN 0006-8314 1573-1472 Atmospheric Science journal-article 2020 crspringernat https://doi.org/10.1007/s10546-020-00590-1 2022-01-04T14:45:10Z Abstract Observations from the 2014 Arctic Clouds in Summer Experiment indicate that, in summer, warm-air advection over melting sea-ice results in a strong surface melting feedback forced by a very strong surface-based temperature inversion and fog formation exerting additional heat flux on the surface. Here, we analyze this case further using a combination of reanalysis dataset and satellite products in a Lagrangian framework, thereby extending the view spatially from the local icebreaker observations into a Langrangian perspective. The results confirm that warm-air advection induces a positive net surface-energy-budget anomaly, exerting positive longwave radiation and turbulent heat flux on the surface. Additionally, as warm and moist air penetrates farther into the Arctic, cloud-top cooling and surface mixing eventually erode the surface inversion downstream. The initial surface inversion splits into two elevated inversions while the air columns below the elevated inversions transform into well-mixed layers. Article in Journal/Newspaper Arctic Sea ice Springer Nature (via Crossref) Arctic Boundary-Layer Meteorology 179 1 99 116 |
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Springer Nature (via Crossref) |
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English |
topic |
Atmospheric Science |
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Atmospheric Science You, Cheng Tjernström, Michael Devasthale, Abhay Warm-Air Advection Over Melting Sea-Ice: A Lagrangian Case Study |
topic_facet |
Atmospheric Science |
description |
Abstract Observations from the 2014 Arctic Clouds in Summer Experiment indicate that, in summer, warm-air advection over melting sea-ice results in a strong surface melting feedback forced by a very strong surface-based temperature inversion and fog formation exerting additional heat flux on the surface. Here, we analyze this case further using a combination of reanalysis dataset and satellite products in a Lagrangian framework, thereby extending the view spatially from the local icebreaker observations into a Langrangian perspective. The results confirm that warm-air advection induces a positive net surface-energy-budget anomaly, exerting positive longwave radiation and turbulent heat flux on the surface. Additionally, as warm and moist air penetrates farther into the Arctic, cloud-top cooling and surface mixing eventually erode the surface inversion downstream. The initial surface inversion splits into two elevated inversions while the air columns below the elevated inversions transform into well-mixed layers. |
author2 |
Stockholm University |
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-Air Advection Over Melting Sea-Ice: A Lagrangian Case Study |
title_short |
Warm-Air Advection Over Melting Sea-Ice: A Lagrangian Case Study |
title_full |
Warm-Air Advection Over Melting Sea-Ice: A Lagrangian Case Study |
title_fullStr |
Warm-Air Advection Over Melting Sea-Ice: A Lagrangian Case Study |
title_full_unstemmed |
Warm-Air Advection Over Melting Sea-Ice: A Lagrangian Case Study |
title_sort |
warm-air advection over melting sea-ice: a lagrangian case study |
publisher |
Springer Science and Business Media LLC |
publishDate |
2020 |
url |
http://dx.doi.org/10.1007/s10546-020-00590-1 http://link.springer.com/content/pdf/10.1007/s10546-020-00590-1.pdf http://link.springer.com/article/10.1007/s10546-020-00590-1/fulltext.html |
geographic |
Arctic |
geographic_facet |
Arctic |
genre |
Arctic Sea ice |
genre_facet |
Arctic Sea ice |
op_source |
Boundary-Layer Meteorology volume 179, issue 1, page 99-116 ISSN 0006-8314 1573-1472 |
op_rights |
https://creativecommons.org/licenses/by/4.0 https://creativecommons.org/licenses/by/4.0 |
op_rightsnorm |
CC-BY |
op_doi |
https://doi.org/10.1007/s10546-020-00590-1 |
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Boundary-Layer Meteorology |
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179 |
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1 |
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99 |
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116 |
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