Sea-Ice Freeboard Retrieval Using Digital Photon-Counting Laser Altimetry
Airborne and spaceborne altimeters provide measurements of sea-ice elevation, from which sea-ice freeboard and thickness may be derived. Observations of the Arctic ice pack by satellite altimeters indicate a significant decline in ice thickness, and volume, over the last decade. NASA's Ice, Clo...
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ftnasantrs:oai:casi.ntrs.nasa.gov:20150004436 2023-05-15T15:06:58+02:00 Sea-Ice Freeboard Retrieval Using Digital Photon-Counting Laser Altimetry Farrell, Sinead L. Connor, Laurence N. Walsh, Kaitlin M. Brunt, Kelly M. Ruth, Julia M. Kuhn, John M. Unclassified, Unlimited, Publicly available October 2015 application/pdf http://hdl.handle.net/2060/20150004436 unknown Document ID: 20150004436 http://hdl.handle.net/2060/20150004436 Copyright, Distribution under U.S. Government purpose rights CASI Geosciences (General) Earth Resources and Remote Sensing GSFC-E-DAA-TN20642 Annals of Glaciology (e-ISSN 1727-5644); 56; 69; 167-174 2015 ftnasantrs 2019-07-21T00:16:32Z Airborne and spaceborne altimeters provide measurements of sea-ice elevation, from which sea-ice freeboard and thickness may be derived. Observations of the Arctic ice pack by satellite altimeters indicate a significant decline in ice thickness, and volume, over the last decade. NASA's Ice, Cloud and land Elevation Satellite-2 (ICESat-2) is a next-generation laser altimeter designed to continue key sea-ice observations through the end of this decade. An airborne simulator for ICESat-2, the Multiple Altimeter Beam Experimental Lidar (MABEL), has been deployed to gather pre-launch data for mission development. We present an analysis of MABEL data gathered over sea ice in the Greenland Sea and assess the capabilities of photon-counting techniques for sea-ice freeboard retrieval. We compare freeboard estimates in the marginal ice zone derived from MABEL photon-counting data with coincident data collected by a conventional airborne laser altimeter. We find that freeboard estimates agree to within 0.03m in the areas where sea-ice floes were interspersed with wide leads, and to within 0.07m elsewhere. MABEL data may also be used to infer sea-ice thickness, and when compared with coincident but independent ice thickness estimates, MABEL ice thicknesses agreed to within 0.65m or better. Other/Unknown Material Arctic Greenland Greenland Sea ice pack Sea ice NASA Technical Reports Server (NTRS) Arctic Greenland Mabel ENVELOPE(-44.683,-44.683,-60.667,-60.667) |
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Open Polar |
collection |
NASA Technical Reports Server (NTRS) |
op_collection_id |
ftnasantrs |
language |
unknown |
topic |
Geosciences (General) Earth Resources and Remote Sensing |
spellingShingle |
Geosciences (General) Earth Resources and Remote Sensing Farrell, Sinead L. Connor, Laurence N. Walsh, Kaitlin M. Brunt, Kelly M. Ruth, Julia M. Kuhn, John M. Sea-Ice Freeboard Retrieval Using Digital Photon-Counting Laser Altimetry |
topic_facet |
Geosciences (General) Earth Resources and Remote Sensing |
description |
Airborne and spaceborne altimeters provide measurements of sea-ice elevation, from which sea-ice freeboard and thickness may be derived. Observations of the Arctic ice pack by satellite altimeters indicate a significant decline in ice thickness, and volume, over the last decade. NASA's Ice, Cloud and land Elevation Satellite-2 (ICESat-2) is a next-generation laser altimeter designed to continue key sea-ice observations through the end of this decade. An airborne simulator for ICESat-2, the Multiple Altimeter Beam Experimental Lidar (MABEL), has been deployed to gather pre-launch data for mission development. We present an analysis of MABEL data gathered over sea ice in the Greenland Sea and assess the capabilities of photon-counting techniques for sea-ice freeboard retrieval. We compare freeboard estimates in the marginal ice zone derived from MABEL photon-counting data with coincident data collected by a conventional airborne laser altimeter. We find that freeboard estimates agree to within 0.03m in the areas where sea-ice floes were interspersed with wide leads, and to within 0.07m elsewhere. MABEL data may also be used to infer sea-ice thickness, and when compared with coincident but independent ice thickness estimates, MABEL ice thicknesses agreed to within 0.65m or better. |
format |
Other/Unknown Material |
author |
Farrell, Sinead L. Connor, Laurence N. Walsh, Kaitlin M. Brunt, Kelly M. Ruth, Julia M. Kuhn, John M. |
author_facet |
Farrell, Sinead L. Connor, Laurence N. Walsh, Kaitlin M. Brunt, Kelly M. Ruth, Julia M. Kuhn, John M. |
author_sort |
Farrell, Sinead L. |
title |
Sea-Ice Freeboard Retrieval Using Digital Photon-Counting Laser Altimetry |
title_short |
Sea-Ice Freeboard Retrieval Using Digital Photon-Counting Laser Altimetry |
title_full |
Sea-Ice Freeboard Retrieval Using Digital Photon-Counting Laser Altimetry |
title_fullStr |
Sea-Ice Freeboard Retrieval Using Digital Photon-Counting Laser Altimetry |
title_full_unstemmed |
Sea-Ice Freeboard Retrieval Using Digital Photon-Counting Laser Altimetry |
title_sort |
sea-ice freeboard retrieval using digital photon-counting laser altimetry |
publishDate |
2015 |
url |
http://hdl.handle.net/2060/20150004436 |
op_coverage |
Unclassified, Unlimited, Publicly available |
long_lat |
ENVELOPE(-44.683,-44.683,-60.667,-60.667) |
geographic |
Arctic Greenland Mabel |
geographic_facet |
Arctic Greenland Mabel |
genre |
Arctic Greenland Greenland Sea ice pack Sea ice |
genre_facet |
Arctic Greenland Greenland Sea ice pack Sea ice |
op_source |
CASI |
op_relation |
Document ID: 20150004436 http://hdl.handle.net/2060/20150004436 |
op_rights |
Copyright, Distribution under U.S. Government purpose rights |
_version_ |
1766338549976662016 |