Articles

Persistent warm-eddy transport to Antarctic ice shelves driven by enhanced summer westerlies

Gao, Libao; Yuan, Xiaojun; Cai, Wenju; Guo, Guijun; Yu, Weidong; Shi, Jiuxin; Qiao, Fangli; Wei, Zexun; Williams, Guy D.

The offshore ocean heat supplied to the Antarctic continental shelves by warm eddies has the potential to greatly impact the melting rates of ice shelves and subsequent global sea level rise. While featured in modeling and some observational studies, the processes around how these warm eddies form and overcome the dynamic sub-surface barrier of the Antarctic Slope Front over the upper continental slope has not yet been clarified. Here we report on the detailed observations of persistent eddies carrying warm modified Cir- cumpolar Deep Water (CDW) onto the continental shelf of Prydz Bay, East Antarctica, using subsurface mooring and hydrographic section data from 2013-2015. We show the warm-eddy transport is most active when the summer westerlies strengthen, which promotes the upwelling of CDW and initiates eddy formation and intrusions. Our study highlights the important role of warm eddies in the melting of Antarctica’s ice shelves, both now and into the future.

Keywords: Antarctic Deep Water, ocean heat, warm eddies

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Also Published In

Title
Nature Communications
DOI
https://doi.org/10.1038/s41467-024-45010-x

More About This Work

Academic Units
Lamont-Doherty Earth Observatory
Ocean and Climate Physics
Published Here
February 7, 2024