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1000 Titel
  • Altered Weddell Sea warm- and dense-water pathways in response to 21st-century climate change
1000 Autor/in
  1. Nissen, Cara |
  2. Timmermann, Ralph |
  3. van Caspel, Mathias |
  4. Wekerle, Claudia |
1000 Verlag
  • Copernicus Publications
1000 Erscheinungsjahr 2024
1000 Publikationstyp
  1. Artikel |
1000 Online veröffentlicht
  • 2024-01-22
1000 Erschienen in
1000 Quellenangabe
  • 20(1):85-101
1000 Copyrightjahr
  • 2024
1000 Lizenz
1000 Verlagsversion
  • https://doi.org/10.5194/os-20-85-2024 |
1000 Publikationsstatus
1000 Begutachtungsstatus
1000 Sprache der Publikation
1000 Abstract/Summary
  • <jats:p>Abstract. The transport of water masses with ocean circulation is a key component of the global climate system. In this context, the Filchner Trough in the southern Weddell Sea is critical, as it is a hotspot for the cross-shelf-break exchange of Dense Shelf Water and Warm Deep Water. We present results from Lagrangian particle tracking experiments in a global-ocean–sea-ice model (FESOM-1.4) which includes ice-shelf cavities and has eddy-permitting resolution on the southern Weddell Sea continental shelf. With backward and forward experiments, we assess changes between a present-day and a future (SSP5-8.5) time slice in the origin of waters reaching the Filchner Ice Shelf front and the fate of waters leaving it. We show that particles reaching the ice-shelf front from the open ocean originate from 173 % greater depths by 2100 (median; 776 m as compared to 284 m for the present day), while waters leaving the cavity towards the open ocean end up at 35 % shallower depths (550 m as compared to 850 m for the present day). Pathways of water leaving the continental shelf increasingly occur in the upper ocean, while the on-shelf flow of waters that might reach the ice-shelf cavity, i.e., at deeper layers, becomes more important by 2100. Simultaneously, median transit times between the Filchner Ice Shelf front and the continental shelf break decrease (increase) by 6 (9.5) months in the backward (forward) experiments. In conclusion, our study demonstrates the sensitivity of regional circulation patterns in the southern Weddell Sea to ongoing climate change, with direct implications for ice-shelf basal melt rates and local ecosystems. </jats:p>
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1000 Förderer
  1. Horizon 2020 |
  2. HORIZON EUROPE Climate, Energy and Mobility |
1000 Fördernummer
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1000 Förderprogramm
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  2. -
1000 Dateien
1000 Förderung
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    1000 Förderer Horizon 2020 |
    1000 Förderprogramm -
    1000 Fördernummer -
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    1000 Förderer HORIZON EUROPE Climate, Energy and Mobility |
    1000 Förderprogramm -
    1000 Fördernummer -
1000 Objektart article
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1000 @id frl:6482171.rdf
1000 Erstellt am 2024-05-24T03:22:43.487+0200
1000 Erstellt von 322
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1000 Zuletzt bearbeitet 2024-05-27T10:18:41.591+0200
1000 Objekt bearb. Mon May 27 10:18:41 CEST 2024
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