Physical Conditions of Fast Glacier Flow: 1. Measurements From Boreholes Drilled to the Bed of Store Glacier, West Greenland-Reference-Cited by-同舟云学术

Physical Conditions of Fast Glacier Flow: 1. Measurements From Boreholes Drilled to the Bed of Store Glacier, West Greenland

Author:

Doyle S. H.¹^ORCID,Hubbard B.¹^ORCID,Christoffersen P.²^ORCID,Young T. J.²³^ORCID,Hofstede C.⁴^ORCID,Bougamont M.²^ORCID,Box J. E.⁵^ORCID,Hubbard A.⁶

Affiliation:

1. Centre for Glaciology, Department of Geography and Earth Sciences; Aberystwyth University; Aberystwyth UK

2. Scott Polar Research Institute; Cambridge University; Cambridge UK

3. British Antarctic Survey; National Environmental Research Council; Cambridge UK

4. Helmholtz Centre for Polar and Marine Research; Alfred Wegener Institute; Bremerhaven Germany

5. Glaciology and Climate, Geological Survey of Denmark and Greenland; Copenhagen Denmark

6. Centre for Arctic Gas Hydrate, Environment and Climate, Department of Geology; Arctic University of Norway; Tromsø Norway

Funder

UK National Environment Research Council

Research Council of Norway through its Centres of Excellence

Publisher

American Geophysical Union (AGU)

Subject

Earth-Surface Processes,Geophysics

Link

Reference119 articles.

3. Moulin density controls drainage development beneath the Greenland Ice Sheet;Banwell;Journal of Geophysical Research: Earth Surface,2016

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