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1000 Titel
  • Sources of low-frequency variability in observed Antarctic sea ice
1000 Autor/in
  1. Bonan, David B. |
  2. Dörr, Jakob |
  3. Wills, Robert C. J. |
  4. Thompson, Andrew F. |
  5. Årthun, Marius |
1000 Erscheinungsjahr 2024
1000 Publikationstyp
  1. Artikel |
1000 Online veröffentlicht
  • 2024-04-30
1000 Erschienen in
1000 Quellenangabe
  • 18(4):2141-2159
1000 Copyrightjahr
  • 2024
1000 Lizenz
1000 Verlagsversion
  • https://doi.org/10.5194/tc-18-2141-2024 |
1000 Publikationsstatus
1000 Begutachtungsstatus
1000 Sprache der Publikation
1000 Abstract/Summary
  • <jats:p>Abstract. Antarctic sea ice has exhibited significant variability over the satellite record, including a period of prolonged and gradual expansion, as well as a period of sudden decline. A number of mechanisms have been proposed to explain this variability, but how each mechanism manifests spatially and temporally remains poorly understood. Here, we use a statistical method called low-frequency component analysis to analyze the spatiotemporal structure of observed Antarctic sea ice concentration variability. The identified patterns reveal distinct modes of low-frequency sea ice variability. The leading mode, which accounts for the large-scale, gradual expansion of sea ice, is associated with the Interdecadal Pacific Oscillation and resembles the observed sea surface temperature trend pattern that climate models have trouble reproducing. The second mode is associated with the central Pacific El Niño–Southern Oscillation (ENSO) and the Southern Annular Mode and accounts for most of the sea ice variability in the Ross Sea. The third mode is associated with the eastern Pacific ENSO and Amundsen Sea Low and accounts for most of the pan-Antarctic sea ice variability and almost all of the sea ice variability in the Weddell Sea. The third mode is also related to periods of abrupt Antarctic sea ice decline that are associated with a weakening of the circumpolar westerlies, which favors surface warming through a shoaling of the ocean mixed layer and decreased northward Ekman heat transport. Broadly, these results suggest that climate model biases in long-term Antarctic sea ice and large-scale sea surface temperature trends are related to each other and that eastern Pacific ENSO variability is a key ingredient for abrupt Antarctic sea ice changes. </jats:p>
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  1. https://frl.publisso.de/adhoc/uri/Qm9uYW4sIERhdmlkwqBCLg==|https://frl.publisso.de/adhoc/uri/RMO2cnIsIEpha29i|https://frl.publisso.de/adhoc/uri/V2lsbHMsIFJvYmVydMKgQy7CoEou|https://frl.publisso.de/adhoc/uri/VGhvbXBzb24sIEFuZHJld8KgRi4=|https://frl.publisso.de/adhoc/uri/w4VydGh1biwgTWFyaXVz
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1000 Förderer
  1. Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung |
  2. National Science Foundation |
  3. Office of Naval Research |
  4. Trond Mohn stiftelse |
1000 Fördernummer
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  2. -
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  4. -
1000 Förderprogramm
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1000 Dateien
  1. Sources of low-frequency variability in observed Antarctic sea ice
1000 Förderung
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    1000 Förderer Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung |
    1000 Förderprogramm -
    1000 Fördernummer -
  2. 1000 joinedFunding-child
    1000 Förderer National Science Foundation |
    1000 Förderprogramm -
    1000 Fördernummer -
  3. 1000 joinedFunding-child
    1000 Förderer Office of Naval Research |
    1000 Förderprogramm -
    1000 Fördernummer -
  4. 1000 joinedFunding-child
    1000 Förderer Trond Mohn stiftelse |
    1000 Förderprogramm -
    1000 Fördernummer -
1000 Objektart article
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1000 Erstellt am 2024-05-10T15:43:41.079+0200
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1000 Zuletzt bearbeitet 2024-05-15T07:25:54.877+0200
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