Decline in Surface Melt Duration on Larsen C Ice Shelf Revealed by The Advanced Scatterometer (ASCAT)

Author:

Bevan Suzanne Louise1ORCID,Luckman Adrian John1ORCID,Kuipers Munneke Peter2ORCID,Hubbard Bryn3ORCID,Kulessa Bernd1ORCID,Ashmore David William4ORCID

Affiliation:

1. Geography Department, College of Science; Swansea University; Swansea UK

2. Institute for Marine and Atmospheric research Utrecht; Utrecht University; Utrecht Netherlands

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

4. School of Environmental Sciences; University of Liverpool; Liverpool UK

Funder

Natural Environment Research Council

Publisher

American Geophysical Union (AGU)

Subject

General Earth and Planetary Sciences,Environmental Science (miscellaneous)

Reference45 articles.

1. Passive microwave-derived snow melt regions on the Greenland Ice Sheet;Abdalati;Geophysical Research Letters,1995

2. Variable basal melt rates of Antarctic Peninsula Ice Shelves, 1994-2016;Adusumilli;Geophysical Research Letters,2018

3. Quantifying vulnerability of Antarctic ice shelves to hydrofracture using microwave scattering properties;Alley;Remote Sensing of Environment,2018

4. Comparison of methods for melt detection over Greenland using active and passive microwave measurements;Ashcraft;International Journal of Remote Sensing,2006

5. Trends in Antarctic Peninsula surface melting conditions from observations and regional climate modeling;Barrand;Journal of Geophysical Research: Earth Surface,2013

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