Reassessing the role of the Antarctic Slope Current in poleward ocean heat transport
The Antarctic Slope Current (ASC) is often considered a barrier to the poleward transport of Circumpolar Deep Water (CDW), yet its vast extent has hindered circumpolar analysis of this relationship. Here, we use a high-resolution global ocean-sea ice
Authors
- Taimoor Sohail (ORCID: https://orcid.org/0000-0002-4162-3269)
- Matthew H. England (ORCID: https://orcid.org/0000-0001-9696-2930)
- Fabio Boeira Dias (ORCID: https://orcid.org/0000-0002-2965-2120)
- Ellie Q. Y. Ong (ORCID: https://orcid.org/0000-0002-0392-7915)
- Paul Spence (ORCID: https://orcid.org/0000-0001-5156-2204)
- Wilma G. C. Huneke (ORCID: https://orcid.org/0000-0001-8624-365X)
- Wilton Aguiar (ORCID: https://orcid.org/0000-0003-2453-9791)
- Adele K. Morrison (ORCID: https://orcid.org/0000-0002-9904-4980)
Institutions
- Australian National University (AU)
- University of Tasmania (AU)
- UNSW Sydney (AU)
Publication Details
- Published
- 2025-09-04
- DOI
- https://doi.org/10.22541/essoar.175700056.62702833/v1
- Primary Topic
- Cryospheric studies and observations
- Type
- article
- Field-Weighted Citation Impact
- 0.00
Funders
- National Computational Infrastructure
- Australian Government
- Climate Extremes
- National Cancer Institute