Acceleration and spatial rheology of Larsen C Ice Shelf, Antarctic Peninsula - Wikidata - awgldk - TriplyDB

Acceleration and spatial rheology of Larsen C Ice Shelf, Antarctic Peninsula

Acceleration and spatial rheology of Larsen C Ice Shelf, Antarctic Peninsula

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Marine ice regulates the future stability of a large Antarctic ice shelf.Massive subsurface ice formed by refreezing of ice-shelf melt ponds Channelized Melting Drives Thinning Under a Rapidly Melting Antarctic Ice Shelf Marine ice formation in a suture zone on the Larsen C Ice Shelf and its influence on ice shelf dynamics The structure and effect of suture zones in the Larsen C Ice Shelf, Antarctica Basal crevasses on the Larsen C Ice Shelf, Antarctica: Implications for meltwater ponding and hydrofracture Impact of tide-topography interactions on basal melting of Larsen C Ice Shelf, Antarctica A constitutive framework for predicting weakening and reduced buttressing of ice shelves based on observations of the progressive deterioration of the remnant Larsen B Ice Shelf Revealing the early ice flow patterns with historical Declassified Intelligence Satellite Photographs back to 1960s

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Acceleration and spatial rheology of Larsen C Ice Shelf, Antarctic Peninsula

http://www.wikidata.org/entity/Q58318088

description

im Mai 2011 veröffentlichter wissenschaftlicher Artikel

@de

wetenschappelijk artikel

@nl

наукова стаття, опублікована в травні 2011

@uk

name

Acceleration and spatial rheology of Larsen C Ice Shelf, Antarctic Peninsula

@en

Acceleration and spatial rheology of Larsen C Ice Shelf, Antarctic Peninsula

@nl

type

label

Acceleration and spatial rheology of Larsen C Ice Shelf, Antarctic Peninsula

@en

Acceleration and spatial rheology of Larsen C Ice Shelf, Antarctic Peninsula

@nl

prefLabel

Acceleration and spatial rheology of Larsen C Ice Shelf, Antarctic Peninsula

@en

Acceleration and spatial rheology of Larsen C Ice Shelf, Antarctic Peninsula

@nl

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Geophysical Research Letters

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Acceleration and spatial rheology of Larsen C Ice Shelf, Antarctic Peninsula

@en

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A. Khazendar

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

E. Larour

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Accelerated ice discharge from the Antarctic Peninsula following the collapse of Larsen B ice shelf

Numerical modelling and data assimilation of the Larsen B ice shelf, Antarctic Peninsula.

Larsen ice shelf has progressively thinned.

Present stability of the Larsen C ice shelf, Antarctic Peninsula

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

Roles of marine ice, rheology, and fracture in the flow and stability of the Brunt/Stancomb-Wills Ice Shelf

Larsen B Ice Shelf rheology preceding its disintegration inferred by a control method

Rheology of the Ronne Ice Shelf, Antarctica, inferred from satellite radar interferometry data using an inverse control method

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scholarly article

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10.1029/2011GL046775

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9

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38

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2011-05-13T00:00:00Z

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