Sustained ocean cooling insufficient to reverse sea level rise from Antarctica

Global mean sea level has risen at an accelerating rate in the last decade and will continue to rise for centuries. The Amundsen Sea Embayment in West Antarctica is a critical region for present and future ice loss, however most studies consider only a worst-case future for the region. Here we use i...

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Vydané v:	Communications earth & environment Ročník 5; číslo 1; s. 150 - 9
Hlavní autori:	Alevropoulos-Borrill, Alanna, Golledge, Nicholas R., Cornford, Stephen L., Lowry, Daniel P., Krapp, Mario
Médium:	Journal Article
Jazyk:	English
Vydavateľské údaje:	London Nature Publishing Group 01.12.2024 Nature Portfolio
Predmet:	Ablation Bays Discharge Glaciation Global sea level Ice Ice sheet models Ice sheets Ice shelves Land ice Mean sea level Melting Oceans Rivers Sea level Sea level changes Sea level rise Sensitivity Sheet modelling Amundsen Sea Antarctica
ISSN:	2662-4435, 2662-4435
On-line prístup:	Získať plný text
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