Wind-induced variability of warm water on the Southern Bellingshausen Sea continental shelf

Ria Oelerich, Karen J. Heywood, Gillian M. Damerell, Andrew F. Thompson

Research output: Contribution to journalArticlepeer-review

2 Citations (Scopus)
13 Downloads (Pure)

Abstract

The Bellingshausen Sea hosts heat transport onto the continental shelf, potentially enhancing ice shelf basal melt. Here, we use the GLORYS12V1 1993–2018 reanalysis to identify physical processes that set seasonal and interannual variability of water mass properties in the Eltanin and Latady Bays on the southern Bellingshausen Sea continental shelf. Annual means of potential temperature from 300 m to the seabed reveal interannual variability and allow separation into warm and cold regimes. The Amundsen Sea Low (ASL) is more intense and extends further east during the warm regime than the cold regime. In the warm regime, a wind-induced reduction of sea ice concentration near the coast increases surface heat loss, convection, and formation of cold dense water in winter, associated with a decrease in heat content of the southern Bellingshausen Sea over time and a net northward heat transport. In contrast, in the cold regime, increased sea ice concentration reduces surface heat loss and thus formation of cold, dense water. Combined with an increase in heat content over time and a net southward heat transport, this results in a warming of the southern Bellingshausen Sea. This suggests that variability in the deep water temperature in the southern Bellingshausen Sea is primarily due to local surface heat fluxes above the shelf. The variability of surface heat fluxes is related to the variability of the ASL and its influence on sea ice extent and local formation of cold, dense water in winter.

Original languageEnglish
Article numbere2022JC018636
JournalJournal of Geophysical Research - Oceans
Volume127
Issue number11
Early online date26 Oct 2022
DOIs
Publication statusPublished - Nov 2022

Keywords

  • Amundsen Sea Low
  • Bellingshausen Sea
  • GLORYS12V1 reanalysis
  • cold water formation
  • frontal jet
  • heat transport

Cite this