Future warming of Circumpolar Deep Water linked to surface buoyancy forcing
Circumpolar Deep Water (CDW) is the warmest water mass in the Southern Ocean and its transport onto the Antarctic continental shelf is the main contributor of heat to the region. Observations suggest that CDW has warmed and shifted poleward in recent
Authors
- Hannah Dawson (ORCID: https://orcid.org/0000-0001-9113-1329)
- Hangyu Meng (ORCID: https://orcid.org/0000-0001-5310-3079)
- Andrew McC. Hogg (ORCID: https://orcid.org/0000-0001-5898-7635)
- 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)
Publication Details
- Published
- 2025-08-25
- DOI
- https://doi.org/10.22541/essoar.175611204.40750783/v1
- Primary Topic
- Arctic and Antarctic ice dynamics
- Type
- article
- Field-Weighted Citation Impact
- 0.00
Funders
- National Computational Infrastructure
- Australian Government
- Climate Extremes
- National Cancer Institute