The role of upper-ocean heat content in the regional variability of Arctic sea ice at sub-seasonal timescales
Abstract Q ml Q 300 Q ml Q 300 anomalies act as a precursor for wintertime sea ice variability in the Barents and Kara seas, with considerable strengthening and expansion of this link from 1980–2000 and 2001–2021 in both reanalyses. Our results highlight the role played by upper-ocean heat content in modulating the interannual variability of Arctic sea ice at sub-seasonal timescales. Heat stored in the ocean has important implications for the predictability of sea ice, calling for improvements in forecast initialization and a focus upon regional predictions in the Arctic region.
- Standort
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Deutsche Nationalbibliothek Frankfurt am Main
- Umfang
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Online-Ressource
- Sprache
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Englisch
- Erschienen in
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The role of upper-ocean heat content in the regional variability of Arctic sea ice at sub-seasonal timescales ; volume:18 ; number:5 ; year:2024 ; pages:2357-2379 ; extent:23
The Cryosphere ; 18, Heft 5 (2024), 2357-2379 (gesamt 23)
- Urheber
- DOI
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10.5194/tc-18-2357-2024
- URN
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urn:nbn:de:101:1-2405160427347.650249464688
- Rechteinformation
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Open Access; Der Zugriff auf das Objekt ist unbeschränkt möglich.
- Letzte Aktualisierung
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14.08.2025, 10:46 MESZ
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Beteiligte
- Bianco, Elena
- Iovino, Doroteaciro
- Masina, Simona
- Materia, Stefano
- Ruggieri, Paolo
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