Bathymetric control of tidewater glacier mass loss in northwest Greenland

It has been suggested that fjord geometry could be an important contributor to the observed mass loss variability in Greenland by modulating the flow of warm water to marine-terminating glaciers. New gravity-derived bathymetry of Greenlandic fjords confirms the link between the grounding line depth...

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Veröffentlicht in:Earth and planetary science letters 2014-09, Vol.401, p.40-46
Hauptverfasser: Porter, David F., Tinto, Kirsty J., Boghosian, Alexandra, Cochran, James R., Bell, Robin E., Manizade, Serdar S., Sonntag, John G.
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Sprache:eng
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