Actively evolving subglacial conduits and eskers initiate ice shelf channels at an Antarctic grounding line.

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Channelized Melting Drives Thinning Under a Rapidly Melting Antarctic Ice Shelf Detecting high spatial variability of ice shelf basal mass balance, Roi Baudouin Ice Shelf, Antarctica Hard rock landforms generate 130 km ice shelf channels through water focusing in basal corrugations

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P2860

Actively evolving subglacial conduits and eskers initiate ice shelf channels at an Antarctic grounding line.

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2017 nî lūn-bûn

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2017年の論文

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2017年論文

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2017年論文

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2017年論文

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2017年論文

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2017年论文

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2017年论文

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Actively evolving subglacial c ...... t an Antarctic grounding line.

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Actively evolving subglacial c ...... t an Antarctic grounding line.

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Actively evolving subglacial c ...... t an Antarctic grounding line.

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P1476

Actively evolving subglacial c ...... t an Antarctic grounding line.

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I J Hewitt

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K Matsuoka

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N Bergeot

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P2860

Elevation and elevation change of Greenland and Antarctica derived from CryoSat-2

Undercutting of marine-terminating glaciers in West Greenland

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

Getting around Antarctica: new high-resolution mappings of the grounded and freely-floating boundaries of the Antarctic ice sheet created for the International Polar Year

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

Meltwater produced by wind–albedo interaction stored in an East Antarctic ice shelf

Evolution of ice-shelf channels in Antarctic ice shelves

Dynamic influence of pinning points on marine ice-sheet stability: a numerical study in Dronning Maud Land, East Antarctica

Morphological properties of tunnel valleys of the southern sector of the Laurentide Ice Sheet and implications for their formation

Coupling of ice-shelf melting and buttressing is a key process in ice-sheets dynamics

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10.1038/NCOMMS15228

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English

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2017-05-09T00:00:00Z

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Actively evolving subglacial conduits and eskers initiate ice shelf channels at an Antarctic grounding line.

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P2860

P2860

Actively evolving subglacial conduits and eskers initiate ice shelf channels at an Antarctic grounding line.

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