Reversal of Ross Sea shelf water freshening is linked to a persistent decline in Antarctic sea ice since the mid-2010s

Since the mid-2010s, a sharp rebound in dense shelf water (DSW) salinity has been observed in the Ross Sea, coinciding with a persistent decline in sea ice around Antarctica. Despite extensive scientific study and significant attention given to these two phenomena due to their potential influence on...

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Bibliografische Detailangaben

Hauptverfasser:	Taekyun Kim, Sung-Ho Choo, Jae-Hong Moon, Emilia Kyung Jin, Daehyuk Kim, Hyeonsoo Cha
Format:	Artigo
Sprache:	Inglês
Veröffentlicht:	IOP Publishing 2025-01-01
Schriftenreihe:	Environmental Research Letters
Schlagworte:	Ross Sea dense shelf water salinity rebound polynya expansion Antarctic sea ice decline asymmetric wind response
Online-Zugang:	https://doi.org/10.1088/1748-9326/ae0f3f
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