Satellite-based estimates of Antarctic surface meltwater fluxes
This study generates novel satellite-derived estimates of Antarctic-wide annual (1999-2009) surface meltwater production using an empirical relationship between radar backscatter from the QuikSCAT (QSCAT) satellite and melt calculated from in situ energy balance observations. The resulting QSCAT-der...
Published in: | Geophysical Research Letters |
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Main Authors: | , , , , |
Format: | Text |
Language: | unknown |
Published: |
Clark Digital Commons
2013
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Subjects: | |
Online Access: | https://commons.clarku.edu/faculty_geography/226 https://doi.org/10.1002/2013GL058138 https://commons.clarku.edu/context/faculty_geography/article/1225/viewcontent/GeogFacWorks_Frey_Satellite_2013.pdf |
Summary: | This study generates novel satellite-derived estimates of Antarctic-wide annual (1999-2009) surface meltwater production using an empirical relationship between radar backscatter from the QuikSCAT (QSCAT) satellite and melt calculated from in situ energy balance observations. The resulting QSCAT-derived melt fluxes significantly agree with output from the regional climate model RACMO2.1 and with independent ground-based observations. The high-resolution (4.45 km) QSCAT-based melt fluxes uniquely detect interannually persistent and intense melt (>400 mm water equivalent (w.e.) year-1) on interior Larsen C Ice Shelf that is not simulated by RACMO2.1. This supports a growing understanding of the importance of a föhn effect in this region and quantifies the resulting locally enhanced melting that is spatially consistent with recently observed Larsen C thinning. These new results highlight important cryosphere-climate interactions and processes that are presently not fully captured by the coarser-resolution (27 km) regional climate model. Key Points Novel satellite-based estimates of Antarctic surface meltwater production Broad agreement among satellite, ground, and climate model melt results High melt on inner Larsen C Ice Shelf likely results from a föhn effect ©2013. American Geophysical Union. All Rights Reserved. |
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