Strong Ocean Melting Feedback During the Recent Retreat of Thwaites Glacier

Accelerating ice loss from Thwaites Glacier is contributing approximately 5% of global sea‐level rise, and could add tens of centimeters to sea level over the coming centuries. We use an ocean model to calculate sub‐ice melting for a succession of Digital Elevation Models of the main trunk of Thwait...

Celý popis

Uloženo v:

Podrobná bibliografie
Vydáno v:	Geophysical research letters Ročník 50; číslo 8
Hlavní autoři:	Holland, Paul R., Bevan, Suzanne L., Luckman, Adrian J.
Médium:	Journal Article
Jazyk:	angličtina
Vydáno:	Washington John Wiley & Sons, Inc 28.04.2023 Wiley
Témata:	Ablation Antarctic Ice Sheet Anthropogenic climate changes Anthropogenic factors Climate change Digital Elevation Models Emissions Evolution Feedback Gases Glaciation Glacier melting Glacier retreat Glaciers Global warming Greenhouse effect Greenhouse gases Human influences Ice Ice melting Ice sheets ice‐ocean interaction Inflow Melting Meltwater Mitigation Ocean currents Ocean models Ocean temperature Ocean warming Oceans Sea level sea‐level rise Southern Ocean Thwaites Glacier Water circulation Water column Water inflow
ISSN:	0094-8276, 1944-8007
On-line přístup:	Získat plný text
Tagy:	Přidat tag Žádné tagy, Buďte první, kdo vytvoří štítek k tomuto záznamu!

Buďte první, kdo okomentuje tento záznam!