Contrasting melt regime in the Ice Grounding Zone of Thwaites Glacier, West Antarctica

The contribution of Thwaites Glacier, Antarctica, to sea level rise is influenced by how quickly warm salty seawater of Circumpolar Deep Water origin melts basal ice near its grounding line. Satellite observations reveal tidally forced kilometer-scale seawater intrusions beneath grounded ice that fo...

Celý popis

Podrobná bibliografia

Vydané v:	Proceedings of the National Academy of Sciences - PNAS Ročník 122; číslo 48; s. e2512626122
Hlavní autori:	Gadi, Ratnakar, Rignot, Eric, Menemenlis, Dimitris, Scheuchl, Bernd
Médium:	Journal Article
Jazyk:	English
Vydavateľské údaje:	United States 02.12.2025
Predmet:	glaciology Antarctica southern ocean grounding line sea level rise
ISSN:	1091-6490, 1091-6490
On-line prístup:	Zistit podrobnosti o prístupe
Tagy:	Pridať tag Žiadne tagy, Buďte prvý, kto otaguje tento záznam!