Satellite-based estimates of Antarctic surface meltwater fluxes
Author Posting. © American Geophysical Union, 2013. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Geophysical Research Letters 40 (2013): 6148–6153, doi:10.1002/2013GL058138. This study genera...
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ftwhoas:oai:darchive.mblwhoilibrary.org:1912/6427 2023-05-15T13:53:14+02:00 Satellite-based estimates of Antarctic surface meltwater fluxes Trusel, Luke D. Frey, Karen E. Das, Sarah B. Munneke, Peter Kuipers van den Broeke, Michiel R. 2013-12-04 text/plain application/pdf application/postscript application/msword https://hdl.handle.net/1912/6427 en_US eng John Wiley & Sons https://doi.org/10.1002/2013GL058138 Geophysical Research Letters 40 (2013): 6148–6153 https://hdl.handle.net/1912/6427 doi:10.1002/2013GL058138 Geophysical Research Letters 40 (2013): 6148–6153 doi:10.1002/2013GL058138 Antarctica Surface melt Ice shelves Remote sensing Article 2013 ftwhoas https://doi.org/10.1002/2013GL058138 2022-05-28T22:59:01Z Author Posting. © American Geophysical Union, 2013. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Geophysical Research Letters 40 (2013): 6148–6153, doi:10.1002/2013GL058138. 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. This research was supported by NASA Headquarters under the NASA Earth and Space Science Fellowship Program (grant NNX12AO01H), the NASA Cryospheric Sciences Program (grant NNX10AP09G), and the NSF Antarctic Sciences Section (grant ANT-063203). 2014-06-04 Article in Journal/Newspaper Antarc* Antarctic Antarctica Ice Shelf Ice Shelves Woods Hole Scientific Community: WHOAS (Woods Hole Open Access Server) Antarctic Geophysical Research Letters 40 23 6148 6153 |
institution |
Open Polar |
collection |
Woods Hole Scientific Community: WHOAS (Woods Hole Open Access Server) |
op_collection_id |
ftwhoas |
language |
English |
topic |
Antarctica Surface melt Ice shelves Remote sensing |
spellingShingle |
Antarctica Surface melt Ice shelves Remote sensing Trusel, Luke D. Frey, Karen E. Das, Sarah B. Munneke, Peter Kuipers van den Broeke, Michiel R. Satellite-based estimates of Antarctic surface meltwater fluxes |
topic_facet |
Antarctica Surface melt Ice shelves Remote sensing |
description |
Author Posting. © American Geophysical Union, 2013. This article is posted here by permission of American Geophysical Union for personal use, not for redistribution. The definitive version was published in Geophysical Research Letters 40 (2013): 6148–6153, doi:10.1002/2013GL058138. 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. This research was supported by NASA Headquarters under the NASA Earth and Space Science Fellowship Program (grant NNX12AO01H), the NASA Cryospheric Sciences Program (grant NNX10AP09G), and the NSF Antarctic Sciences Section (grant ANT-063203). 2014-06-04 |
format |
Article in Journal/Newspaper |
author |
Trusel, Luke D. Frey, Karen E. Das, Sarah B. Munneke, Peter Kuipers van den Broeke, Michiel R. |
author_facet |
Trusel, Luke D. Frey, Karen E. Das, Sarah B. Munneke, Peter Kuipers van den Broeke, Michiel R. |
author_sort |
Trusel, Luke D. |
title |
Satellite-based estimates of Antarctic surface meltwater fluxes |
title_short |
Satellite-based estimates of Antarctic surface meltwater fluxes |
title_full |
Satellite-based estimates of Antarctic surface meltwater fluxes |
title_fullStr |
Satellite-based estimates of Antarctic surface meltwater fluxes |
title_full_unstemmed |
Satellite-based estimates of Antarctic surface meltwater fluxes |
title_sort |
satellite-based estimates of antarctic surface meltwater fluxes |
publisher |
John Wiley & Sons |
publishDate |
2013 |
url |
https://hdl.handle.net/1912/6427 |
geographic |
Antarctic |
geographic_facet |
Antarctic |
genre |
Antarc* Antarctic Antarctica Ice Shelf Ice Shelves |
genre_facet |
Antarc* Antarctic Antarctica Ice Shelf Ice Shelves |
op_source |
Geophysical Research Letters 40 (2013): 6148–6153 doi:10.1002/2013GL058138 |
op_relation |
https://doi.org/10.1002/2013GL058138 Geophysical Research Letters 40 (2013): 6148–6153 https://hdl.handle.net/1912/6427 doi:10.1002/2013GL058138 |
op_doi |
https://doi.org/10.1002/2013GL058138 |
container_title |
Geophysical Research Letters |
container_volume |
40 |
container_issue |
23 |
container_start_page |
6148 |
op_container_end_page |
6153 |
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1766258249336619008 |