Spatial extent and temporal variability of Greenland firn aquifers detected by ground and airborne radars-Reference-Cited by-同舟云学术

Spatial extent and temporal variability of Greenland firn aquifers detected by ground and airborne radars

Published:2016-12 Issue:12 Volume:121 Page:2381-2398
ISSN:2169-9003
Container-title:Journal of Geophysical Research: Earth Surface
language:en
Short-container-title:J. Geophys. Res. Earth Surf.

Author:

Miège Clément¹^ORCID,Forster Richard R.¹^ORCID,Brucker Ludovic²³^ORCID,Koenig Lora S.⁴^ORCID,Solomon D. Kip⁵,Paden John D.⁶^ORCID,Box Jason E.⁷,Burgess Evan W.¹,Miller Julie Z.¹⁸,McNerney Laura¹,Brautigam Noah¹,Fausto Robert S.⁷^ORCID,Gogineni Sivaprasad⁶

Affiliation:

1. Department of Geography University of Utah Salt Lake City Utah USA

2. Cryospheric Sciences Laboratory, Code 615 NASA Goddard Space Flight Center Greenbelt Maryland USA

3. Universities Space Research Association Goddard Earth Sciences Technology and Research Studies and Investigations Columbia Maryland USA

4. National Snow and Ice Data Center, Cooperative Institute for Research in Environmental Sciences University of Colorado Boulder Boulder Colorado USA

5. Department of Geology and Geophysics University of Utah Salt Lake City Utah USA

6. Center for Remote Sensing of Ice Sheets University of Kansas Lawrence Kansas USA

7. Geological Survey of Denmark and Greenland (GEUS) Copenhagen Denmark

8. Byrd Climate and Research Center Ohio State University Columbus Ohio USA

Funder

Office of the Director

Oklahoma Space Grant Consortium

Publisher

American Geophysical Union (AGU)

Subject

Earth-Surface Processes,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1002/2016JF003869

Reference49 articles.

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2. Benson C. S.(1962) Stratigraphic studies in the snow and firn of the Greenland ice sheet CRREL Res. Rep. 70.

3. Complex dielectric permittivity measurements from ground-penetrating radar data to estimate snow liquid water content in the pendular regime

4. A spatially calibrated model of annual accumulation rate on the Greenland Ice Sheet (1958-2007)

5. Persistent englacial drainage features in the Greenland Ice Sheet

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