Sudden increase in tidal response linked to calving and acceleration at a large Greenland outlet glacier

Author:

de Juan Julia1,Elósegui Pedro1,Nettles Meredith2,Larsen Tine B.3,Davis James L.4,Hamilton Gordon S.5,Stearns Leigh A.6,Andersen Morten L.,Ekström Göran2,Ahlstrøm Andreas P.3,Stenseng Lars7,Khan S. Abbas7,Forsberg René7

Affiliation:

1. Institute for Space Sciences; CSIC-IEEC; Barcelona; Spain

2. Lamont-Doherty Earth Observatory; Columbia University; Palisades; New York; USA

3. Geological Survey of Denmark and Greenland; Copenhagen; Denmark

4. Harvard-Smithsonian Center for Astrophysics; Cambridge; Massachusetts; USA

5. Climate Change Institute; University of Maine; Orono; Maine; USA

6. Department of Geology; University of Kansas; Lawrence; Kansas; USA

7. DTU Space; National Space Institute; Copenhagen; Denmark

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Reference32 articles.

1. Glacier, fjord, and seismic response to recent large calving events, Jakobshavn Isbrae, Greenland;Amundson;Geophys. Res. Lett.,2008

2. Tidal forcing of basal seismicity of ice stream C, West Antarctica, observed far inland;Anandakrishnan;J. Geophys. Res.,1997

3. Ice stream D flow speed is strongly modulated by the tide beneath the Ross Ice Shelf;Anandakrishnan;Geophys. Res. Lett.,2003

4. Surface melt and its effect on Helheim Glacier dynamics;Andersen;Eos Trans. AGU,2009

5. Tidally controlled stick-slip discharge of a West Antarctic Ice Stream;Bindschadler;Science,2003

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