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1000 Titel
  • Modeling seasonal-to-decadal ocean–cryosphere interactions along the Sabrina Coast, East Antarctica
1000 Autor/in
  1. Kusahara, Kazuya |
  2. Hirano, Daisuke |
  3. Fujii, Masakazu |
  4. Fraser, Alexander D. |
  5. Tamura, Takeshi |
  6. Mizobata, Kohei |
  7. Williams, Guy D. |
  8. Aoki, Shigeru |
1000 Verlag
  • Copernicus Publications
1000 Erscheinungsjahr 2024
1000 Publikationstyp
  1. Artikel |
1000 Online veröffentlicht
  • 2024-01-03
1000 Erschienen in
1000 Quellenangabe
  • 18(1):43-73
1000 Copyrightjahr
  • 2024
1000 Lizenz
1000 Verlagsversion
  • https://doi.org/10.5194/tc-18-43-2024 |
1000 Publikationsstatus
1000 Begutachtungsstatus
1000 Sprache der Publikation
1000 Abstract/Summary
  • <jats:p>Abstract. The Totten Ice Shelf (TIS) and Moscow University Ice Shelf (MUIS), along the Sabrina Coast of Wilkes Land, are the floating seaward terminuses of the second-largest freshwater reservoir in the East Antarctic Ice Sheet. Being a marine ice sheet, it is vulnerable to the surrounding ocean conditions. Recent comprehensive oceanographic observations, including bathymetric measurements off the Sabrina Coast, have shed light on the widespread intrusion of warm modified Circumpolar Deep Water (mCDW) onto the continental shelf and the intense ice–ocean interaction beneath the TIS. However, the spatiotemporal coverage of the observation is very limited. Here, we use an ocean–sea ice–ice shelf model with updated bathymetry to better understand the regional ocean circulations and ocean–cryosphere interactions. The model successfully captured the widespread intrusions of mCDW, local sea ice production and the ocean heat and volume transports into the TIS cavity, facilitating an examination of the overturning ocean circulation within the ice shelf cavities and the resultant basal melting. We found notable differences in the temporal variability in ice shelf basal melting across the two adjacent ice shelves of the TIS and the western part of the MUIS. Ocean heat transport by mCDW controls the low-frequency interannual-to-decadal variability in ice–ocean interactions, but the sea ice production in the Dalton Polynya strongly modifies the signals, explaining the regional difference between the two ice shelves. The formation of a summertime eastward-flowing undercurrent beneath the westward-flowing Antarctic Slope Current is found to play an important role in the seasonal delivery of ocean heat to the continental shelf. </jats:p>
1000 Liste der Beteiligten
  1. https://frl.publisso.de/adhoc/uri/S3VzYWhhcmEsIEthenV5YQ==|https://frl.publisso.de/adhoc/uri/SGlyYW5vLCBEYWlzdWtl|https://frl.publisso.de/adhoc/uri/RnVqaWksIE1hc2FrYXp1|https://frl.publisso.de/adhoc/uri/RnJhc2VyLCBBbGV4YW5kZXLCoEQu|https://frl.publisso.de/adhoc/uri/VGFtdXJhLCBUYWtlc2hp|https://frl.publisso.de/adhoc/uri/TWl6b2JhdGEsIEtvaGVp|https://frl.publisso.de/adhoc/uri/V2lsbGlhbXMsIEd1ecKgRC4=|https://frl.publisso.de/adhoc/uri/QW9raSwgU2hpZ2VydQ==
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  • DeepGreen-ID: 71533662881f452a8473e9e45aee3723 ; metadata provieded by: DeepGreen (https://www.oa-deepgreen.de/api/v1/), LIVIVO search scope life sciences (http://z3950.zbmed.de:6210/livivo), Crossref Unified Resource API (https://api.crossref.org/swagger-ui/index.html), to.science.api (https://frl.publisso.de/), ZDB JSON-API (beta) (https://zeitschriftendatenbank.de/api/), lobid - Dateninfrastruktur für Bibliotheken (https://lobid.org/resources/search)
1000 Label
1000 Förderer
  1. Japan Society for the Promotion of Science |
1000 Fördernummer
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1000 Dateien
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    1000 Förderer Japan Society for the Promotion of Science |
    1000 Förderprogramm -
    1000 Fördernummer -
1000 Objektart article
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1000 Erstellt am 2024-05-23T21:04:44.399+0200
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1000 Zuletzt bearbeitet 2024-05-27T09:50:22.140+0200
1000 Objekt bearb. Mon May 27 09:50:22 CEST 2024
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