Retrieval of surface emissivity of sea ice and temperature profiles over sea ice from passive microwave radiometers

Sea ice, surface emissivity, emitting layer temperature, temperature profile, microwave radiometry. - Polar regions play a key role in the global climate. The information on atmospheric parameters in these regions is sparse. Among the polar surfaces, sea ice varies in extent and physical properties...

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Main Author: Mathew, Nizy
Format: Book
Language:English
Published: Univ. Bremen 2007
Subjects:
Online Access:http://hdl.handle.net/11858/00-1735-0000-0001-31C7-2
https://doi.org/10.23689/fidgeo-316
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spelling ftsubggeo:oai:e-docs.geo-leo.de:11858/00-1735-0000-0001-31C7-2 2024-06-09T07:43:54+00:00 Retrieval of surface emissivity of sea ice and temperature profiles over sea ice from passive microwave radiometers Mathew, Nizy 2007 application/pdf http://hdl.handle.net/11858/00-1735-0000-0001-31C7-2 https://doi.org/10.23689/fidgeo-316 eng eng Univ. Bremen Geophysik doi:10.23689/fidgeo-316 550930043 http://hdl.handle.net/11858/00-1735-0000-0001-31C7-2 http://e-docs.geo-leo.de/rights ddc:551.343 doc-type:book publishedVersion 2007 ftsubggeo https://doi.org/10.23689/fidgeo-316 2024-05-10T04:57:11Z Sea ice, surface emissivity, emitting layer temperature, temperature profile, microwave radiometry. - Polar regions play a key role in the global climate. The information on atmospheric parameters in these regions is sparse. Among the polar surfaces, sea ice varies in extent and physical properties with region and season and so does the surface emissivity. In the present study a method to retrieve the emissivity is applied over two selected regions in the Arctic, one covered by first-year ice and the other by multiyear ice and it investigates the application of them in the improvement of temperature profile retrieval ver sea ice. The retrieval of surface emissivity is done by combining simulated brightness temperatures with the satellite measured brightness temperature. In order to determine the surface emissivity of sea ice, the observations of the microwave instruments amsu (Advanced Microwave Sounding Unit) and amsr-e (Advanced Microwave Scanning Radiometer- Earth Observing System) are used. Determination of emissivity requires the knowledge of the temperature of the emitting layer. The penetration depth of microwaves in sea ice varies between millimeters and decimeters depending on the frequency and micro-physical structure. A year-round observation of temperature profiles of sea ice from the Surface Heat Budget of the Arctic Ocean (sheba) campaign at a first-year and a multiyear ice site is used to derive a set of coefficients a and b to linearly relate . thesis Book Arctic Arctic Ocean Sea ice Surface Heat Budget of the Arctic Ocean GEO-LEOe-docs (FID GEO) Arctic Arctic Ocean
institution Open Polar
collection GEO-LEOe-docs (FID GEO)
op_collection_id ftsubggeo
language English
topic ddc:551.343
spellingShingle ddc:551.343
Mathew, Nizy
Retrieval of surface emissivity of sea ice and temperature profiles over sea ice from passive microwave radiometers
topic_facet ddc:551.343
description Sea ice, surface emissivity, emitting layer temperature, temperature profile, microwave radiometry. - Polar regions play a key role in the global climate. The information on atmospheric parameters in these regions is sparse. Among the polar surfaces, sea ice varies in extent and physical properties with region and season and so does the surface emissivity. In the present study a method to retrieve the emissivity is applied over two selected regions in the Arctic, one covered by first-year ice and the other by multiyear ice and it investigates the application of them in the improvement of temperature profile retrieval ver sea ice. The retrieval of surface emissivity is done by combining simulated brightness temperatures with the satellite measured brightness temperature. In order to determine the surface emissivity of sea ice, the observations of the microwave instruments amsu (Advanced Microwave Sounding Unit) and amsr-e (Advanced Microwave Scanning Radiometer- Earth Observing System) are used. Determination of emissivity requires the knowledge of the temperature of the emitting layer. The penetration depth of microwaves in sea ice varies between millimeters and decimeters depending on the frequency and micro-physical structure. A year-round observation of temperature profiles of sea ice from the Surface Heat Budget of the Arctic Ocean (sheba) campaign at a first-year and a multiyear ice site is used to derive a set of coefficients a and b to linearly relate . thesis
format Book
author Mathew, Nizy
author_facet Mathew, Nizy
author_sort Mathew, Nizy
title Retrieval of surface emissivity of sea ice and temperature profiles over sea ice from passive microwave radiometers
title_short Retrieval of surface emissivity of sea ice and temperature profiles over sea ice from passive microwave radiometers
title_full Retrieval of surface emissivity of sea ice and temperature profiles over sea ice from passive microwave radiometers
title_fullStr Retrieval of surface emissivity of sea ice and temperature profiles over sea ice from passive microwave radiometers
title_full_unstemmed Retrieval of surface emissivity of sea ice and temperature profiles over sea ice from passive microwave radiometers
title_sort retrieval of surface emissivity of sea ice and temperature profiles over sea ice from passive microwave radiometers
publisher Univ. Bremen
publishDate 2007
url http://hdl.handle.net/11858/00-1735-0000-0001-31C7-2
https://doi.org/10.23689/fidgeo-316
geographic Arctic
Arctic Ocean
geographic_facet Arctic
Arctic Ocean
genre Arctic
Arctic Ocean
Sea ice
Surface Heat Budget of the Arctic Ocean
genre_facet Arctic
Arctic Ocean
Sea ice
Surface Heat Budget of the Arctic Ocean
op_relation Geophysik
doi:10.23689/fidgeo-316
550930043
http://hdl.handle.net/11858/00-1735-0000-0001-31C7-2
op_rights http://e-docs.geo-leo.de/rights
op_doi https://doi.org/10.23689/fidgeo-316
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