publisher:10.1038/s41467-023-36580-3
Observational evidence for on-shelf heat transport driven by dense water export in the Weddell Sea
Darelius, Elin, Daae, Kjersti, Dundas, Vår, Fer, Ilker, Hellmer, Hartmut H ORCID: https://orcid.org/0000-0002-9357-9853, Janout, Markus ORCID: https://orcid.org/0000-0003-4908-2855, Nicholls, Keith W, Sallée, Jean-Baptiste and Østerhus, Svein
;
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Abstract
The transport of oceanic heat towards the Antarctic continental margin is central to the mass balance of the Antarctic Ice Sheet. Recent modeling efforts challenge our view on where and how the on-shelf heat flux occurs, suggesting that it is largest where dense shelf waters cascade down the continental slope. Here we provide observational evidence supporting this claim. Using records from moored instruments, we link the downslope flow of dense water from the Filchner overflow to upslope and on-shelf flow of warm water.
Item Type
Article
Authors
Darelius, Elin, Daae, Kjersti, Dundas, Vår, Fer, Ilker, Hellmer, Hartmut H ORCID: https://orcid.org/0000-0002-9357-9853, Janout, Markus ORCID: https://orcid.org/0000-0003-4908-2855, Nicholls, Keith W, Sallée, Jean-Baptiste and Østerhus, Svein
;
Divisions
Primary Division
Primary Topic
Helmholtz Programs > Helmholtz Research Programs > CHANGING EARTH (2021-2027) > PT2:Ocean and Cryosphere in Climate
Publication Status
Published
Eprint ID
59932
DOI
10.1038/s41467-023-36580-3
Cite as
Darelius, E.
,
Daae, K.
,
Dundas, V.
,
Fer, I.
,
Hellmer, H. H.
,
Janout, M.
,
Nicholls, K. W.
,
Sallée, J. B.
and
Østerhus, S.
(2023):
Observational evidence for on-shelf heat transport driven by dense water export in the Weddell Sea
,
Nature Communications,
14
(1),
p. 1022
.
doi: 10.1038/s41467-023-36580-3
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