The response of sea ice and high-salinity shelf water in the Ross Ice Shelf Polynya to cyclonic atmosphere circulations
Coastal polynyas in the Ross Sea are important source regions of high-salinity shelf water (HSSW) - the precursor of Antarctic Bottom Water thatsupplies the lower limb of the thermohaline circulation. Here, the responseof sea ice production and HSSW formation to synoptic-scale and mesoscalecyclones...
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ftunivhelsihelda:oai:helda.helsinki.fi:10138/356249 2024-01-07T09:39:16+01:00 The response of sea ice and high-salinity shelf water in the Ross Ice Shelf Polynya to cyclonic atmosphere circulations Wang, Xiaoqiao Zhang, Zhaoru Dinniman, Michael S. Uotila, Petteri Li, Xichen Zhou, Meng Institute for Atmospheric and Earth System Research (INAR) 2023-03-16T07:19:01Z 20 application/pdf http://hdl.handle.net/10138/356249 eng eng COPERNICUS GESELLSCHAFT MBH 10.5194/tc-17-1107-2023 Wang , X , Zhang , Z , Dinniman , M S , Uotila , P , Li , X & Zhou , M 2023 , ' The response of sea ice and high-salinity shelf water in the Ross Ice Shelf Polynya to cyclonic atmosphere circulations ' , Cryosphere , vol. 17 , no. 3 , pp. 1107-1126 . https://doi.org/10.5194/tc-17-1107-2023 ORCID: /0000-0002-2939-7561/work/131065181 85150169948 1d5fe8e1-b114-463d-8bcf-c6107f0288c8 http://hdl.handle.net/10138/356249 000943811600001 cc_by openAccess info:eu-repo/semantics/openAccess 114 Physical sciences 1171 Geosciences Article publishedVersion 2023 ftunivhelsihelda 2023-12-14T00:13:34Z Coastal polynyas in the Ross Sea are important source regions of high-salinity shelf water (HSSW) - the precursor of Antarctic Bottom Water thatsupplies the lower limb of the thermohaline circulation. Here, the responseof sea ice production and HSSW formation to synoptic-scale and mesoscalecyclones was investigated for the Ross Ice Shelf Polynya (RISP) using acoupled ocean-sea ice-ice shelf model targeted on the Ross Sea. Whensynoptic-scale cyclones prevailed over RISP, sea ice production (SIP)increased rapidly by 20 %-30 % over the entire RISP. During the passage of mesoscale cyclones, SIP increased by about 2 times over the western RISP but decreased over the eastern RISP, resulting respectively from enhancement inthe offshore and onshore winds. HSSW formation mainly occurred in thewestern RISP and was enhanced responding to the SIP increase under bothtypes of cyclones. Promoted HSSW formation could persist for 12-60 h after the decay of the cyclones. The HSSW exports across the DrygalskiTrough and the Glomar Challenger Trough were positively correlated with themeridional wind. Such correlations are mainly controlled by variations ingeostrophic ocean currents that result from sea surface elevation change and density differences. Peer reviewed Article in Journal/Newspaper Antarc* Antarctic Ice Shelf Ross Ice Shelf Ross Sea Sea ice HELDA – University of Helsinki Open Repository Antarctic Ross Sea Ross Ice Shelf The Cryosphere 17 3 1107 1126 |
institution |
Open Polar |
collection |
HELDA – University of Helsinki Open Repository |
op_collection_id |
ftunivhelsihelda |
language |
English |
topic |
114 Physical sciences 1171 Geosciences |
spellingShingle |
114 Physical sciences 1171 Geosciences Wang, Xiaoqiao Zhang, Zhaoru Dinniman, Michael S. Uotila, Petteri Li, Xichen Zhou, Meng The response of sea ice and high-salinity shelf water in the Ross Ice Shelf Polynya to cyclonic atmosphere circulations |
topic_facet |
114 Physical sciences 1171 Geosciences |
description |
Coastal polynyas in the Ross Sea are important source regions of high-salinity shelf water (HSSW) - the precursor of Antarctic Bottom Water thatsupplies the lower limb of the thermohaline circulation. Here, the responseof sea ice production and HSSW formation to synoptic-scale and mesoscalecyclones was investigated for the Ross Ice Shelf Polynya (RISP) using acoupled ocean-sea ice-ice shelf model targeted on the Ross Sea. Whensynoptic-scale cyclones prevailed over RISP, sea ice production (SIP)increased rapidly by 20 %-30 % over the entire RISP. During the passage of mesoscale cyclones, SIP increased by about 2 times over the western RISP but decreased over the eastern RISP, resulting respectively from enhancement inthe offshore and onshore winds. HSSW formation mainly occurred in thewestern RISP and was enhanced responding to the SIP increase under bothtypes of cyclones. Promoted HSSW formation could persist for 12-60 h after the decay of the cyclones. The HSSW exports across the DrygalskiTrough and the Glomar Challenger Trough were positively correlated with themeridional wind. Such correlations are mainly controlled by variations ingeostrophic ocean currents that result from sea surface elevation change and density differences. Peer reviewed |
author2 |
Institute for Atmospheric and Earth System Research (INAR) |
format |
Article in Journal/Newspaper |
author |
Wang, Xiaoqiao Zhang, Zhaoru Dinniman, Michael S. Uotila, Petteri Li, Xichen Zhou, Meng |
author_facet |
Wang, Xiaoqiao Zhang, Zhaoru Dinniman, Michael S. Uotila, Petteri Li, Xichen Zhou, Meng |
author_sort |
Wang, Xiaoqiao |
title |
The response of sea ice and high-salinity shelf water in the Ross Ice Shelf Polynya to cyclonic atmosphere circulations |
title_short |
The response of sea ice and high-salinity shelf water in the Ross Ice Shelf Polynya to cyclonic atmosphere circulations |
title_full |
The response of sea ice and high-salinity shelf water in the Ross Ice Shelf Polynya to cyclonic atmosphere circulations |
title_fullStr |
The response of sea ice and high-salinity shelf water in the Ross Ice Shelf Polynya to cyclonic atmosphere circulations |
title_full_unstemmed |
The response of sea ice and high-salinity shelf water in the Ross Ice Shelf Polynya to cyclonic atmosphere circulations |
title_sort |
response of sea ice and high-salinity shelf water in the ross ice shelf polynya to cyclonic atmosphere circulations |
publisher |
COPERNICUS GESELLSCHAFT MBH |
publishDate |
2023 |
url |
http://hdl.handle.net/10138/356249 |
geographic |
Antarctic Ross Sea Ross Ice Shelf |
geographic_facet |
Antarctic Ross Sea Ross Ice Shelf |
genre |
Antarc* Antarctic Ice Shelf Ross Ice Shelf Ross Sea Sea ice |
genre_facet |
Antarc* Antarctic Ice Shelf Ross Ice Shelf Ross Sea Sea ice |
op_relation |
10.5194/tc-17-1107-2023 Wang , X , Zhang , Z , Dinniman , M S , Uotila , P , Li , X & Zhou , M 2023 , ' The response of sea ice and high-salinity shelf water in the Ross Ice Shelf Polynya to cyclonic atmosphere circulations ' , Cryosphere , vol. 17 , no. 3 , pp. 1107-1126 . https://doi.org/10.5194/tc-17-1107-2023 ORCID: /0000-0002-2939-7561/work/131065181 85150169948 1d5fe8e1-b114-463d-8bcf-c6107f0288c8 http://hdl.handle.net/10138/356249 000943811600001 |
op_rights |
cc_by openAccess info:eu-repo/semantics/openAccess |
container_title |
The Cryosphere |
container_volume |
17 |
container_issue |
3 |
container_start_page |
1107 |
op_container_end_page |
1126 |
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1787429467059126272 |