Massive subsurface ice formed by refreezing of ice-shelf melt ponds

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Ice and firn heterogeneity within Larsen C Ice Shelf from borehole optical televiewing Meltwater produced by wind–albedo interaction stored in an East Antarctic ice shelf Centuries of intense surface melt on Larsen C Ice Shelf

P2860

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Massive subsurface ice formed by refreezing of ice-shelf melt ponds

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http://www.wikidata.org/entity/Q42723942

description

2016 nî lūn-bûn

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2016年の論文

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2016年論文

@yue

2016年論文

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2016年論文

@zh-hk

2016年論文

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2016年論文

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2016年论文

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2016年论文

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2016年论文

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name

Massive subsurface ice formed by refreezing of ice-shelf melt ponds

@en

Massive subsurface ice formed by refreezing of ice-shelf melt ponds

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Massive subsurface ice formed by refreezing of ice-shelf melt ponds

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type

Item

label

Massive subsurface ice formed by refreezing of ice-shelf melt ponds

@en

Massive subsurface ice formed by refreezing of ice-shelf melt ponds

@en-gb

Massive subsurface ice formed by refreezing of ice-shelf melt ponds

@nl

prefLabel

Massive subsurface ice formed by refreezing of ice-shelf melt ponds

@en

Massive subsurface ice formed by refreezing of ice-shelf melt ponds

@en-gb

Massive subsurface ice formed by refreezing of ice-shelf melt ponds

@nl

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2-s2.0-84974625281

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Nature Communications

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Massive subsurface ice formed by refreezing of ice-shelf melt ponds

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P2093

Heidi Sevestre

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Ian Rutt

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Jean-Louis Tison

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Martin O'Leary

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Morgane Philippe

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Peter Kuipers Munneke

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Suzanne Bevan

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P2860

Bedmap2: improved ice bed, surface and thickness datasets for Antarctica

Channelized ice melting in the ocean boundary layer beneath Pine Island Glacier, Antarctica

Oceanic and atmospheric forcing of Larsen C Ice-Shelf thinning

The modelled surface mass balance of the Antarctic Peninsula at 5.5 km horizontal resolution

Constraining variable density of ice shelves using wide-angle radar measurements

Impacts of warm water on Antarctic ice shelf stability through basal channel formation

Surface melt and ponding on Larsen C Ice Shelf and the impact of föhn winds

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

Present stability of the Larsen C ice shelf, Antarctic Peninsula

Subglacial melt channels and fracture in the floating part of Pine Island Glacier, Antarctica

P2888

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11897

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scholarly article

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10.1038/NCOMMS11897

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English

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2016-06-10T00:00:00Z

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100770/

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