GPS-derived estimates of surface mass balance and ocean-induced basal melt for Pine Island Glacier ice shelf, Antarctica

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GPS-derived estimates of surface mass balance and ocean-induced basal melt for Pine Island Glacier ice shelf, Antarctica

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im November 2017 veröffentlichter wissenschaftlicher Artikel

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wetenschappelijk artikel

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наукова стаття, опублікована в листопаді 2017

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GPS-derived estimates of surfa ...... Glacier ice shelf, Antarctica

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GPS-derived estimates of surfa ...... Glacier ice shelf, Antarctica

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GPS-derived estimates of surfa ...... Glacier ice shelf, Antarctica

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GPS-derived estimates of surfa ...... Glacier ice shelf, Antarctica

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GPS-derived estimates of surfa ...... Glacier ice shelf, Antarctica

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GPS-derived estimates of surfa ...... Glacier ice shelf, Antarctica

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P1476

GPS-derived estimates of surfa ...... Glacier ice shelf, Antarctica

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Ben E. Smith

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C. Max Stevens

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David E. Shean

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David M. Holland

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Ian R. Joughin

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Knut Christianson

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Kristine M. Larson

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Mitchell Bushuk

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Stefan R. M. Ligtenberg

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Increased rate of acceleration on Pine Island Glacier strongly coupled to changes in gravitational driving stress

A Reconciled Estimate of Ice-Sheet Mass Balance

Strong sensitivity of Pine Island ice-shelf melting to climatic variability.

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

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

Ice-shelf melting around Antarctica.

Mechanisms driving variability in the ocean forcing of Pine Island Glacier.

Calving fluxes and basal melt rates of Antarctic ice shelves.

Changes in West Antarctic ice stream dynamics observed with ALOS PALSAR data

Widespread, rapid grounding line retreat of Pine Island, Thwaites, Smith, and Kohler glaciers, West Antarctica, from 1992 to 2011

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2655-2674

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scholarly article

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10.5194/TC-11-2655-2017

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2017-11-21T00:00:00Z

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