Revisiting Antarctic ice loss due to marine ice-cliff instability

Predictions for sea-level rise this century due to melt from Antarctica range from zero to more than one metre. The highest predictions are driven by the controversial marine ice-cliff instability (MICI) hypothesis, which assumes that coastal ice cliffs can rapidly collapse after ice shelves disinte...

Celý popis

Uloženo v:

Podrobná bibliografie
Vydáno v:	Nature (London) Ročník 566; číslo 7742; s. 58 - 64
Hlavní autoři:	Edwards, Tamsin L., Brandon, Mark A., Durand, Gael, Edwards, Neil R., Golledge, Nicholas R., Holden, Philip B., Nias, Isabel J., Payne, Antony J., Ritz, Catherine, Wernecke, Andreas
Médium:	Journal Article
Jazyk:	angličtina
Vydáno:	London Nature Publishing Group UK 01.02.2019 Nature Publishing Group
Témata:	704/106/125 704/106/694/1108 704/106/694/2786 Antarctic ice Causes of Cliffs Climate change Collapse Environmental aspects Environmental Sciences Forecasts and trends Geophysical research Global Changes Global warming Greenhouse effect Greenhouse gases Humanities and Social Sciences Hypotheses Ice Ice sheets Ice shelves Instability Interglacial periods Land ice Mathematical models multidisciplinary Ocean temperature Pliocene Science Science (multidisciplinary) Sea level Sea level changes Sea level rise Sea level variations Sheet modelling Stability Star & galaxy formation Surface-ice melting Antarctica
ISSN:	0028-0836, 1476-4687, 1476-4687
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!