Ocean Stratification and Low Melt Rates at the Ross Ice Shelf Grounding Zone-Reference-Cited by-同舟云学术

Ocean Stratification and Low Melt Rates at the Ross Ice Shelf Grounding Zone

Published:2018-10 Issue:10 Volume:123 Page:7438-7452
ISSN:2169-9275
Container-title:Journal of Geophysical Research: Oceans
language:en
Short-container-title:J. Geophys. Res. Oceans

Author:

Begeman Carolyn Branecky¹^ORCID,Tulaczyk Slawek M.¹^ORCID,Marsh Oliver J.²^ORCID,Mikucki Jill A.³^ORCID,Stanton Timothy P.⁴^ORCID,Hodson Timothy O.⁵^ORCID,Siegfried Matthew R.⁶^ORCID,Powell Ross D.⁵^ORCID,Christianson Knut⁷^ORCID,King Matt A.⁸^ORCID

Affiliation:

1. Department of Earth and Planetary Sciences University of California Santa Cruz CA USA

2. Gateway Antarctica University of Canterbury Christchurch New Zealand

3. Department of Microbiology University of Tennessee, Knoxville Knoxville TN USA

4. Department of Oceanography U.S. Naval Postgraduate School Monterey CA USA

5. Department of Geology and Environmental Geosciences Northern Illinois University DeKalb IL USA

6. Department of Geophysics Stanford University Stanford CA USA

7. Department of Earth and Space Sciences University of Washington Seattle WA USA

8. Surveying and Spatial Sciences, School of Land and Food University of Tasmania Hobart Tasmania Australia

Funder

Australian Research Council

Division of Graduate Education

Division of Ocean Sciences

Division of Antarctic Sciences

National Aeronautics and Space Administration

Gordon and Betty Moore Foundation

Publisher

American Geophysical Union (AGU)

Subject

Earth and Planetary Sciences (miscellaneous),Space and Planetary Science,Geochemistry and Petrology,Geophysics,Oceanography

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1029/2018JC013987

Reference80 articles.

1. Open-ocean deep convection due to thermobaricity: 1. Scaling argument

2. The bottom boundary layer of the deep ocean

3. Ocean variability contributing to basal melt rate near the ice front of Ross Ice Shelf, Antarctica

4. Phase‐sensitive FMCW radar system for high‐precision Antarctic ice shelf profile monitoring

5. Does Rotation Influence Double-Diffusive Fluxes in Polar Oceans?

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