Comparison of Envisat radar and airborne laser altimeter measurements over Arctic sea ice

Sea ice thickness is a crucial, but very undersampled cryospheric parameter of fundamental importance for climate modeling. Advances in satellite altimetry have enabled the measurement of sea ice freeboard using satellite microwave altimeters. Unfortunately, validation of these new techniques has su...

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Main Authors: Connor, LN, Laxon, SW, Ridout, AL, Krabill, WB, McAdoo, DC
Format: Article in Journal/Newspaper
Language:unknown
Published: ELSEVIER SCIENCE INC 2009
Subjects:
Online Access:http://discovery.ucl.ac.uk/154918/
id ftucl:oai:eprints.ucl.ac.uk.OAI2:154918
record_format openpolar
spelling ftucl:oai:eprints.ucl.ac.uk.OAI2:154918 2023-05-15T15:10:43+02:00 Comparison of Envisat radar and airborne laser altimeter measurements over Arctic sea ice Connor, LN Laxon, SW Ridout, AL Krabill, WB McAdoo, DC 2009-03-16 http://discovery.ucl.ac.uk/154918/ unknown ELSEVIER SCIENCE INC REMOTE SENS ENVIRON , 113 (3) 563 - 570. (2009) Satellite altimetry Radar altimeter Laser altimetry Sea ice thickness Snow depth PROCESSING SCHEME THICKNESS MOTION OCEAN COVER SHEET MAPS Article 2009 ftucl 2016-01-21T23:11:26Z Sea ice thickness is a crucial, but very undersampled cryospheric parameter of fundamental importance for climate modeling. Advances in satellite altimetry have enabled the measurement of sea ice freeboard using satellite microwave altimeters. Unfortunately, validation of these new techniques has suffered from a lack of ground truth measurements. Therefore, an airborne campaign was carried out in March 2006 using laser altimetry and photo imagery to validate sea ice elevation measurements derived from the Envisat/RA-2 microwave altimeter.We present a comparative analysis of Envisat/RA-2 sea ice elevation processing with collocated airborne measurements collected north of the Canadian Archipelago. Consistent overall relationships between block-averaged airborne laser and Envisat elevations are found, over both leads and floes, along the full 1300 km aircraft track. The fine resolution of the airborne laser altimeter data is exploited to evaluate elevation variability within the RA-2 ground footprint. Our analysis shows good agreement between RA-2 derived sea ice elevations and those measured by airborne laser altimetry, particularly over refrozen leads where the overall mean difference is about I cm. Notwithstanding this small 1 cm mean difference. we identify a larger elevation uncertainty (of order 10 cm) associated with the uncertain location of dominant radar targets within the particular RA-2 footprint. Sources of measurement uncertainty or ambiguity are identified, and include snow accumulation, tracking noise, and the limited coverage of airborne measurements. Published by Elsevier Inc. Article in Journal/Newspaper Arctic Canadian Archipelago Sea ice University College London: UCL Discovery Arctic
institution Open Polar
collection University College London: UCL Discovery
op_collection_id ftucl
language unknown
topic Satellite altimetry
Radar altimeter
Laser altimetry
Sea ice thickness
Snow depth
PROCESSING SCHEME
THICKNESS
MOTION
OCEAN
COVER
SHEET
MAPS
spellingShingle Satellite altimetry
Radar altimeter
Laser altimetry
Sea ice thickness
Snow depth
PROCESSING SCHEME
THICKNESS
MOTION
OCEAN
COVER
SHEET
MAPS
Connor, LN
Laxon, SW
Ridout, AL
Krabill, WB
McAdoo, DC
Comparison of Envisat radar and airborne laser altimeter measurements over Arctic sea ice
topic_facet Satellite altimetry
Radar altimeter
Laser altimetry
Sea ice thickness
Snow depth
PROCESSING SCHEME
THICKNESS
MOTION
OCEAN
COVER
SHEET
MAPS
description Sea ice thickness is a crucial, but very undersampled cryospheric parameter of fundamental importance for climate modeling. Advances in satellite altimetry have enabled the measurement of sea ice freeboard using satellite microwave altimeters. Unfortunately, validation of these new techniques has suffered from a lack of ground truth measurements. Therefore, an airborne campaign was carried out in March 2006 using laser altimetry and photo imagery to validate sea ice elevation measurements derived from the Envisat/RA-2 microwave altimeter.We present a comparative analysis of Envisat/RA-2 sea ice elevation processing with collocated airborne measurements collected north of the Canadian Archipelago. Consistent overall relationships between block-averaged airborne laser and Envisat elevations are found, over both leads and floes, along the full 1300 km aircraft track. The fine resolution of the airborne laser altimeter data is exploited to evaluate elevation variability within the RA-2 ground footprint. Our analysis shows good agreement between RA-2 derived sea ice elevations and those measured by airborne laser altimetry, particularly over refrozen leads where the overall mean difference is about I cm. Notwithstanding this small 1 cm mean difference. we identify a larger elevation uncertainty (of order 10 cm) associated with the uncertain location of dominant radar targets within the particular RA-2 footprint. Sources of measurement uncertainty or ambiguity are identified, and include snow accumulation, tracking noise, and the limited coverage of airborne measurements. Published by Elsevier Inc.
format Article in Journal/Newspaper
author Connor, LN
Laxon, SW
Ridout, AL
Krabill, WB
McAdoo, DC
author_facet Connor, LN
Laxon, SW
Ridout, AL
Krabill, WB
McAdoo, DC
author_sort Connor, LN
title Comparison of Envisat radar and airborne laser altimeter measurements over Arctic sea ice
title_short Comparison of Envisat radar and airborne laser altimeter measurements over Arctic sea ice
title_full Comparison of Envisat radar and airborne laser altimeter measurements over Arctic sea ice
title_fullStr Comparison of Envisat radar and airborne laser altimeter measurements over Arctic sea ice
title_full_unstemmed Comparison of Envisat radar and airborne laser altimeter measurements over Arctic sea ice
title_sort comparison of envisat radar and airborne laser altimeter measurements over arctic sea ice
publisher ELSEVIER SCIENCE INC
publishDate 2009
url http://discovery.ucl.ac.uk/154918/
geographic Arctic
geographic_facet Arctic
genre Arctic
Canadian Archipelago
Sea ice
genre_facet Arctic
Canadian Archipelago
Sea ice
op_source REMOTE SENS ENVIRON , 113 (3) 563 - 570. (2009)
_version_ 1766341694355144704