Influence of Sea Ice Anomalies on Antarctic Precipitation Using Source Attribution
We conduct sensitivity experiments using a climate model that has an explicit water source tagging capability forced by prescribed composites of sea ice concentrations (SIC) and corresponding SSTs to understand the impact of sea ice anomalies on regional evaporation, moisture transport, and source–r...
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ftcopernicus:oai:publications.copernicus.org:tcd75599 2023-05-15T13:35:06+02:00 Influence of Sea Ice Anomalies on Antarctic Precipitation Using Source Attribution Wang, Hailong Fyke, Jeremy Lenaerts, Jan Nusbaumer, Jesse Singh, Hansi Noone, David Rasch, Philip 2019-06-12 application/pdf https://doi.org/10.5194/tc-2019-69 https://www.the-cryosphere-discuss.net/tc-2019-69/ eng eng doi:10.5194/tc-2019-69 https://www.the-cryosphere-discuss.net/tc-2019-69/ eISSN: 1994-0424 Text 2019 ftcopernicus https://doi.org/10.5194/tc-2019-69 2019-12-24T09:49:03Z We conduct sensitivity experiments using a climate model that has an explicit water source tagging capability forced by prescribed composites of sea ice concentrations (SIC) and corresponding SSTs to understand the impact of sea ice anomalies on regional evaporation, moisture transport, and source–receptor relationships for precipitation over Antarctica. Surface sensible heat fluxes, evaporation, and column-integrated water vapor are larger over Southern Ocean (SO) areas with lower SIC, but changes in Antarctic precipitation and its source attribution with SICs reflect a strong spatial variability. Among the tagged source regions, the Southern Ocean (south of 50° S) contributes the most (40 %) to the Antarctic total precipitation, followed by more northerly ocean basins, most notably the S. Pacific Ocean (27 %), S. Indian Ocean (16 %) and S. Atlantic Ocean (11 %). The annual mean Antarctic precipitation is about 150 Gt/year more in the “low” SIC case than in the “high” SIC case. This difference is larger than the model-simulated interannual variability of Antarctic precipitation (99 Gt/year). The contrast in contribution from the S. Ocean, 102 Gt/year, is even more significant, compared to the interannual variability of 35 Gt/year in Antarctic precipitation that originates from the S. Ocean. The horizontal transport pathways from individual vapor source regions to Antarctica are largely determined by large-scale atmospheric circulation patterns. Vapor from lower latitude source regions takes elevated pathways to Antarctica. In contrast, vapor from the Southern Ocean moves southward within the lower troposphere to the Antarctic continent, so the contribution of nearby sources also depends on regional coastal topography. The impact of sea ice anomalies on regional Antarctic precipitation also depends on atmospheric circulation changes that result from the prescribed composite SIC/SST perturbations. In particular, regional wind anomalies along with surface evaporation changes determine regional shifts in the zonal and meridional moisture fluxes that can explain some of the resultant precipitation changes. Text Antarc* Antarctic Antarctica Sea ice Southern Ocean Copernicus Publications: E-Journals Antarctic Indian Pacific Southern Ocean The Antarctic |
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Open Polar |
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Copernicus Publications: E-Journals |
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ftcopernicus |
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English |
description |
We conduct sensitivity experiments using a climate model that has an explicit water source tagging capability forced by prescribed composites of sea ice concentrations (SIC) and corresponding SSTs to understand the impact of sea ice anomalies on regional evaporation, moisture transport, and source–receptor relationships for precipitation over Antarctica. Surface sensible heat fluxes, evaporation, and column-integrated water vapor are larger over Southern Ocean (SO) areas with lower SIC, but changes in Antarctic precipitation and its source attribution with SICs reflect a strong spatial variability. Among the tagged source regions, the Southern Ocean (south of 50° S) contributes the most (40 %) to the Antarctic total precipitation, followed by more northerly ocean basins, most notably the S. Pacific Ocean (27 %), S. Indian Ocean (16 %) and S. Atlantic Ocean (11 %). The annual mean Antarctic precipitation is about 150 Gt/year more in the “low” SIC case than in the “high” SIC case. This difference is larger than the model-simulated interannual variability of Antarctic precipitation (99 Gt/year). The contrast in contribution from the S. Ocean, 102 Gt/year, is even more significant, compared to the interannual variability of 35 Gt/year in Antarctic precipitation that originates from the S. Ocean. The horizontal transport pathways from individual vapor source regions to Antarctica are largely determined by large-scale atmospheric circulation patterns. Vapor from lower latitude source regions takes elevated pathways to Antarctica. In contrast, vapor from the Southern Ocean moves southward within the lower troposphere to the Antarctic continent, so the contribution of nearby sources also depends on regional coastal topography. The impact of sea ice anomalies on regional Antarctic precipitation also depends on atmospheric circulation changes that result from the prescribed composite SIC/SST perturbations. In particular, regional wind anomalies along with surface evaporation changes determine regional shifts in the zonal and meridional moisture fluxes that can explain some of the resultant precipitation changes. |
format |
Text |
author |
Wang, Hailong Fyke, Jeremy Lenaerts, Jan Nusbaumer, Jesse Singh, Hansi Noone, David Rasch, Philip |
spellingShingle |
Wang, Hailong Fyke, Jeremy Lenaerts, Jan Nusbaumer, Jesse Singh, Hansi Noone, David Rasch, Philip Influence of Sea Ice Anomalies on Antarctic Precipitation Using Source Attribution |
author_facet |
Wang, Hailong Fyke, Jeremy Lenaerts, Jan Nusbaumer, Jesse Singh, Hansi Noone, David Rasch, Philip |
author_sort |
Wang, Hailong |
title |
Influence of Sea Ice Anomalies on Antarctic Precipitation Using Source Attribution |
title_short |
Influence of Sea Ice Anomalies on Antarctic Precipitation Using Source Attribution |
title_full |
Influence of Sea Ice Anomalies on Antarctic Precipitation Using Source Attribution |
title_fullStr |
Influence of Sea Ice Anomalies on Antarctic Precipitation Using Source Attribution |
title_full_unstemmed |
Influence of Sea Ice Anomalies on Antarctic Precipitation Using Source Attribution |
title_sort |
influence of sea ice anomalies on antarctic precipitation using source attribution |
publishDate |
2019 |
url |
https://doi.org/10.5194/tc-2019-69 https://www.the-cryosphere-discuss.net/tc-2019-69/ |
geographic |
Antarctic Indian Pacific Southern Ocean The Antarctic |
geographic_facet |
Antarctic Indian Pacific Southern Ocean The Antarctic |
genre |
Antarc* Antarctic Antarctica Sea ice Southern Ocean |
genre_facet |
Antarc* Antarctic Antarctica Sea ice Southern Ocean |
op_source |
eISSN: 1994-0424 |
op_relation |
doi:10.5194/tc-2019-69 https://www.the-cryosphere-discuss.net/tc-2019-69/ |
op_doi |
https://doi.org/10.5194/tc-2019-69 |
_version_ |
1766060851338412032 |