Observational evidence for on-shelf heat transport driven by dense water export in the Weddell Sea


Contact
enquiries [ at ] symplectic.co.uk

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
Divisions
Primary Division
Primary Topic
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


Download
[thumbnail of Observational evidence for on-shelf heat transport driven by dense water export in the Weddell Sea.pdf]
Preview
PDF
Observational evidence for on-shelf heat transport driven by dense water export in the Weddell Sea.pdf - Other

Download (1MB) | Preview

Share
Add to AnyAdd to TwitterAdd to FacebookAdd to LinkedinAdd to PinterestAdd to Email


Citation

Research Platforms

Campaigns
PS > 124


Actions
Edit Item Edit Item