Analyzing links between simulated Laptev Sea sea ice and atmospheric conditions over adjoining landmasses using causal-effect networks
The connection between permafrost and sea ice in the Arctic is not fully understood. As a first step, we investigate how sea ice interacts with the atmosphere over the permafrost landscape. Prior research established that Arctic-wide sea-ice loss can lead to a warming over circumpolar landmasses. Ho...
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ftcopernicus:oai:publications.copernicus.org:tcd84025 2023-05-15T15:00:47+02:00 Analyzing links between simulated Laptev Sea sea ice and atmospheric conditions over adjoining landmasses using causal-effect networks Rehder, Zoé Niederdrenk, Anne Laura Kaleschke, Lars Kutzbach, Lars 2020-03-10 application/pdf https://doi.org/10.5194/tc-2020-60 https://tc.copernicus.org/preprints/tc-2020-60/ eng eng doi:10.5194/tc-2020-60 https://tc.copernicus.org/preprints/tc-2020-60/ eISSN: 1994-0424 Text 2020 ftcopernicus https://doi.org/10.5194/tc-2020-60 2020-07-20T16:22:21Z The connection between permafrost and sea ice in the Arctic is not fully understood. As a first step, we investigate how sea ice interacts with the atmosphere over the permafrost landscape. Prior research established that Arctic-wide sea-ice loss can lead to a warming over circumpolar landmasses. However, it is still unclear which physical mechanisms drive this connection. We address this by identifying these physical mechanisms as well as local and large-scale drivers of sea-ice cover with a focus on one region with highly variable sea-ice cover and high sea-ice productivity: the Laptev Sea region. We analyze the output of coupled a ocean-sea ice-atmosphere-hydrological discharge model with two statistical methods. With the recently developed Causal Effect Networks we identify temporal links between different variables, while we use composites of high- and low-sea-ice-cover years to reveal spatial patterns and mean changes in variables. We find that in the model local sea-ice cover is a driven rather than a driving variable. Springtime melt of sea ice in the Laptev Sea is mainly controlled by atmospheric large-scale circulation, mediated through meridional wind speed and ice export. During refreeze in fall thermodynamic variables and feedback mechanisms are important - sea-ice cover is interconnected with air temperature, thermal radiation and specific humidity. Though low sea-ice cover leads to an enhanced southward transport of heat and moisture throughout summer, links from sea-ice cover to the atmosphere over land are weak, and both sea ice in the Laptev Sea and the atmospheric conditions over the adjacent landmasses are mainly controlled by common external drivers. Text Arctic Ice laptev Laptev Sea permafrost Sea ice Copernicus Publications: E-Journals Arctic Laptev Sea |
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Open Polar |
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Copernicus Publications: E-Journals |
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ftcopernicus |
language |
English |
description |
The connection between permafrost and sea ice in the Arctic is not fully understood. As a first step, we investigate how sea ice interacts with the atmosphere over the permafrost landscape. Prior research established that Arctic-wide sea-ice loss can lead to a warming over circumpolar landmasses. However, it is still unclear which physical mechanisms drive this connection. We address this by identifying these physical mechanisms as well as local and large-scale drivers of sea-ice cover with a focus on one region with highly variable sea-ice cover and high sea-ice productivity: the Laptev Sea region. We analyze the output of coupled a ocean-sea ice-atmosphere-hydrological discharge model with two statistical methods. With the recently developed Causal Effect Networks we identify temporal links between different variables, while we use composites of high- and low-sea-ice-cover years to reveal spatial patterns and mean changes in variables. We find that in the model local sea-ice cover is a driven rather than a driving variable. Springtime melt of sea ice in the Laptev Sea is mainly controlled by atmospheric large-scale circulation, mediated through meridional wind speed and ice export. During refreeze in fall thermodynamic variables and feedback mechanisms are important - sea-ice cover is interconnected with air temperature, thermal radiation and specific humidity. Though low sea-ice cover leads to an enhanced southward transport of heat and moisture throughout summer, links from sea-ice cover to the atmosphere over land are weak, and both sea ice in the Laptev Sea and the atmospheric conditions over the adjacent landmasses are mainly controlled by common external drivers. |
format |
Text |
author |
Rehder, Zoé Niederdrenk, Anne Laura Kaleschke, Lars Kutzbach, Lars |
spellingShingle |
Rehder, Zoé Niederdrenk, Anne Laura Kaleschke, Lars Kutzbach, Lars Analyzing links between simulated Laptev Sea sea ice and atmospheric conditions over adjoining landmasses using causal-effect networks |
author_facet |
Rehder, Zoé Niederdrenk, Anne Laura Kaleschke, Lars Kutzbach, Lars |
author_sort |
Rehder, Zoé |
title |
Analyzing links between simulated Laptev Sea sea ice and atmospheric conditions over adjoining landmasses using causal-effect networks |
title_short |
Analyzing links between simulated Laptev Sea sea ice and atmospheric conditions over adjoining landmasses using causal-effect networks |
title_full |
Analyzing links between simulated Laptev Sea sea ice and atmospheric conditions over adjoining landmasses using causal-effect networks |
title_fullStr |
Analyzing links between simulated Laptev Sea sea ice and atmospheric conditions over adjoining landmasses using causal-effect networks |
title_full_unstemmed |
Analyzing links between simulated Laptev Sea sea ice and atmospheric conditions over adjoining landmasses using causal-effect networks |
title_sort |
analyzing links between simulated laptev sea sea ice and atmospheric conditions over adjoining landmasses using causal-effect networks |
publishDate |
2020 |
url |
https://doi.org/10.5194/tc-2020-60 https://tc.copernicus.org/preprints/tc-2020-60/ |
geographic |
Arctic Laptev Sea |
geographic_facet |
Arctic Laptev Sea |
genre |
Arctic Ice laptev Laptev Sea permafrost Sea ice |
genre_facet |
Arctic Ice laptev Laptev Sea permafrost Sea ice |
op_source |
eISSN: 1994-0424 |
op_relation |
doi:10.5194/tc-2020-60 https://tc.copernicus.org/preprints/tc-2020-60/ |
op_doi |
https://doi.org/10.5194/tc-2020-60 |
_version_ |
1766332849164648448 |