Basal Crevasse Formation on Byrd Glacier, East Antarctica, as Proxy for Past Subglacial Flooding Events-Reference-Cited by-同舟云学术

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Basal Crevasse Formation on Byrd Glacier, East Antarctica, as Proxy for Past Subglacial Flooding Events

Published:2021-08 Issue:15 Volume:48 Page:
ISSN:0094-8276
Container-title:Geophysical Research Letters
language:en
Short-container-title:Geophys Res Lett

Author:

Child Sarah F.¹²^ORCID,Stearns Leigh A.¹³^ORCID,Veen C. J.⁴^ORCID,Elósegui Pedro⁵⁶^ORCID

Affiliation:

1. Department of Geology University of Kansas Lawrence KS USA

2. Cooperative Institute for Research in Environmental Sciences University of Colorado Boulder CO USA

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

4. Department of Geography & Atmospheric Sciences University of Kansas Lawrence KS USA

5. Massachusetts Institute of Technology Haystack Observatory Westford MA USA

6. Institute of Marine Sciences ICM‐CSIC Barcelona Spain

Funder

Division of Antarctic Sciences

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Geophysics

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2020GL090978

Reference66 articles.

1. Mapping the grounding zone of the Ross Ice Shelf, Antarctica, using ICESat laser altimetry

2. Antarctic subglacial lakes drain through sediment-floored canals: theory and model testing on real and idealized domains

3. Basal channels drive active surface hydrology and transverse ice shelf fracture

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