Rain and ice flagging of Envisat altimeter and MWR data

Altimetry range, wave height, and wind speed measurements are often corrupted by two effects over the ocean: rain and sea-ice. Radiometer measurements, which provide the altimetric wet troposphere correction, are similarly corrupted by the presence of rain or sea-ice in the instrument's footpri...

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Main Authors: John Lillibridge, Remko Scharroo
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Published: 2005
Subjects:
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.652.2017
http://eprints.soton.ac.uk/17318/1/Salz_final_lillibridge.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.652.2017 2023-05-15T18:16:19+02:00 Rain and ice flagging of Envisat altimeter and MWR data John Lillibridge Remko Scharroo The Pennsylvania State University CiteSeerX Archives 2005 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.652.2017 http://eprints.soton.ac.uk/17318/1/Salz_final_lillibridge.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.652.2017 http://eprints.soton.ac.uk/17318/1/Salz_final_lillibridge.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://eprints.soton.ac.uk/17318/1/Salz_final_lillibridge.pdf text 2005 ftciteseerx 2016-01-08T16:26:38Z Altimetry range, wave height, and wind speed measurements are often corrupted by two effects over the ocean: rain and sea-ice. Radiometer measurements, which provide the altimetric wet troposphere correction, are similarly corrupted by the presence of rain or sea-ice in the instrument's footprint. To avoid contamination of sea surface height measurements, it is imperative that data influenced by either of these effects be edited out. The waveform “peakiness ” parameter, available on the GDR data sets is effective at identifying sea-ice returns when stringent thresholds are applied. The mean relationship between backscatter (0) at the two altimeter frequencies allows one to flag data impacted by both rain and sea-ice. We present here a new method for flagging rain or sea-ice contaminated data, based on two-dimensional histograms of 0. 1. Text Sea ice Unknown
institution Open Polar
collection Unknown
op_collection_id ftciteseerx
language English
description Altimetry range, wave height, and wind speed measurements are often corrupted by two effects over the ocean: rain and sea-ice. Radiometer measurements, which provide the altimetric wet troposphere correction, are similarly corrupted by the presence of rain or sea-ice in the instrument's footprint. To avoid contamination of sea surface height measurements, it is imperative that data influenced by either of these effects be edited out. The waveform “peakiness ” parameter, available on the GDR data sets is effective at identifying sea-ice returns when stringent thresholds are applied. The mean relationship between backscatter (0) at the two altimeter frequencies allows one to flag data impacted by both rain and sea-ice. We present here a new method for flagging rain or sea-ice contaminated data, based on two-dimensional histograms of 0. 1.
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author John Lillibridge
Remko Scharroo
spellingShingle John Lillibridge
Remko Scharroo
Rain and ice flagging of Envisat altimeter and MWR data
author_facet John Lillibridge
Remko Scharroo
author_sort John Lillibridge
title Rain and ice flagging of Envisat altimeter and MWR data
title_short Rain and ice flagging of Envisat altimeter and MWR data
title_full Rain and ice flagging of Envisat altimeter and MWR data
title_fullStr Rain and ice flagging of Envisat altimeter and MWR data
title_full_unstemmed Rain and ice flagging of Envisat altimeter and MWR data
title_sort rain and ice flagging of envisat altimeter and mwr data
publishDate 2005
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.652.2017
http://eprints.soton.ac.uk/17318/1/Salz_final_lillibridge.pdf
genre Sea ice
genre_facet Sea ice
op_source http://eprints.soton.ac.uk/17318/1/Salz_final_lillibridge.pdf
op_relation http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.652.2017
http://eprints.soton.ac.uk/17318/1/Salz_final_lillibridge.pdf
op_rights Metadata may be used without restrictions as long as the oai identifier remains attached to it.
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