Marine ice regulates the future stability of a large Antarctic ice shelf. - Wikidata - awgldk - TriplyDB

Marine ice regulates the future stability of a large Antarctic ice shelf.

Marine ice regulates the future stability of a large Antarctic ice shelf.

http://www.wikidata.org/entity/Q37720185

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Ocean-driven thinning enhances iceberg calving and retreat of Antarctic ice shelves Basal channels drive active surface hydrology and transverse ice shelf fracture.Ice and firn heterogeneity within Larsen C Ice Shelf from borehole optical televiewing Dynamic changes on the Wilkins Ice Shelf during the 2006–2009 retreat derived from satellite observations Hard rock landforms generate 130 km ice shelf channels through water focusing in basal corrugations Fracture propagation and stability of ice shelves governed by ice shelf heterogeneity Evolution of a supercooled Ice Shelf Water plume with an actively growing subice platelet matrix

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Marine ice regulates the future stability of a large Antarctic ice shelf.

http://www.wikidata.org/entity/Q37720185

description

article científic

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article scientifique

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articolo scientifico

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artigo científico

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bilimsel makale

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scientific article published on 22 April 2014

@en

vedecký článok

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vetenskaplig artikel

@sv

videnskabelig artikel

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vědecký článek

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name

Marine ice regulates the future stability of a large Antarctic ice shelf.

@en

Marine ice regulates the future stability of a large Antarctic ice shelf.

@nl

type

label

Marine ice regulates the future stability of a large Antarctic ice shelf.

@en

Marine ice regulates the future stability of a large Antarctic ice shelf.

@nl

prefLabel

Marine ice regulates the future stability of a large Antarctic ice shelf.

@en

Marine ice regulates the future stability of a large Antarctic ice shelf.

@nl

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Nature Communications

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Marine ice regulates the future stability of a large Antarctic ice shelf.

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Edward C King

http://www.w3.org/2001/XMLSchema#string

Peter R Sammonds

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P2860

Extensive dynamic thinning on the margins of the Greenland and Antarctic ice sheets.

Antarctic ice-sheet loss driven by basal melting of ice shelves.

Larsen ice shelf has progressively thinned.

Twenty-first-century warming of a large Antarctic ice-shelf cavity by a redirected coastal current.

Ice flow of the Antarctic ice sheet.

Marine ice formation in a suture zone on the Larsen C Ice Shelf and its influence on ice shelf dynamics

Basal crevasses in Larsen C Ice Shelf and implications for their global abundance

Present stability of the Larsen C ice shelf, Antarctic Peninsula

Surface structure and stability of the Larsen C ice shelf, Antarctic Peninsula

Creep deformation and buttressing capacity of damaged ice shelves: theory and application to Larsen C ice shelf

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3707

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scholarly article

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10.1038/NCOMMS4707

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5

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2014-04-22T00:00:00Z

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261769696

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24751641

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