Radar Altimetric Studies of Polar Ice

Active microwave sensors are known to provide valuable information regarding snow and ice surfaces in the polar regions, where darkness and cloud cover prevail. Here, data collected in the Arctic by a Ku-band microwave radar altimeter, designed and constructed in the UK, are analysed. The two main c...

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Bibliographic Details
Main Author: Drinkwater, Mark Roland
Format: Thesis
Language:English
Published: Apollo - University of Cambridge Repository 1987
Subjects:
Online Access:https://dx.doi.org/10.17863/cam.14165
https://www.repository.cam.ac.uk/handle/1810/268053
id ftdatacite:10.17863/cam.14165
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spelling ftdatacite:10.17863/cam.14165 2023-05-15T15:07:42+02:00 Radar Altimetric Studies of Polar Ice Drinkwater, Mark Roland 1987 https://dx.doi.org/10.17863/cam.14165 https://www.repository.cam.ac.uk/handle/1810/268053 en eng Apollo - University of Cambridge Repository All Rights Reserved https://www.rioxx.net/licenses/all-rights-reserved/ Text Thesis article-journal ScholarlyArticle 1987 ftdatacite https://doi.org/10.17863/cam.14165 2021-11-05T12:55:41Z Active microwave sensors are known to provide valuable information regarding snow and ice surfaces in the polar regions, where darkness and cloud cover prevail. Here, data collected in the Arctic by a Ku-band microwave radar altimeter, designed and constructed in the UK, are analysed. The two main components of this study comprise data gathered in the East Greenland Sea marginal ice zone and over two Svalbard ice caps. A systematic treatment is made of the electromagnetic properties of snow and ice at 13.81 GHz, and the differences between various polar surface media are highlighted. Theoretical and empirical models are presented which enable calculation of the relevant dielectric and scattering properties of snow and ice layers. Parametric studies are undertaken to give insight into the range of scattering conditions likely to be encountered by a radar altimeter in the regions investigated. Examples of altimetric data and results of their analysis are presented, demonstrating the effects of different ice types and terrain upon incident altimeter pulses. Waveforms are characterised by their shape, and certain forms are linked with particular physical properties of the surface. To this a variety of supporting information is added in order to verify and validate interpretations of these results. Algorithms are proposed which enable geophysical information to be derived from altimetric data. Thesis Arctic East Greenland Greenland Greenland Sea Svalbard DataCite Metadata Store (German National Library of Science and Technology) Arctic Greenland Svalbard
institution Open Polar
collection DataCite Metadata Store (German National Library of Science and Technology)
op_collection_id ftdatacite
language English
description Active microwave sensors are known to provide valuable information regarding snow and ice surfaces in the polar regions, where darkness and cloud cover prevail. Here, data collected in the Arctic by a Ku-band microwave radar altimeter, designed and constructed in the UK, are analysed. The two main components of this study comprise data gathered in the East Greenland Sea marginal ice zone and over two Svalbard ice caps. A systematic treatment is made of the electromagnetic properties of snow and ice at 13.81 GHz, and the differences between various polar surface media are highlighted. Theoretical and empirical models are presented which enable calculation of the relevant dielectric and scattering properties of snow and ice layers. Parametric studies are undertaken to give insight into the range of scattering conditions likely to be encountered by a radar altimeter in the regions investigated. Examples of altimetric data and results of their analysis are presented, demonstrating the effects of different ice types and terrain upon incident altimeter pulses. Waveforms are characterised by their shape, and certain forms are linked with particular physical properties of the surface. To this a variety of supporting information is added in order to verify and validate interpretations of these results. Algorithms are proposed which enable geophysical information to be derived from altimetric data.
format Thesis
author Drinkwater, Mark Roland
spellingShingle Drinkwater, Mark Roland
Radar Altimetric Studies of Polar Ice
author_facet Drinkwater, Mark Roland
author_sort Drinkwater, Mark Roland
title Radar Altimetric Studies of Polar Ice
title_short Radar Altimetric Studies of Polar Ice
title_full Radar Altimetric Studies of Polar Ice
title_fullStr Radar Altimetric Studies of Polar Ice
title_full_unstemmed Radar Altimetric Studies of Polar Ice
title_sort radar altimetric studies of polar ice
publisher Apollo - University of Cambridge Repository
publishDate 1987
url https://dx.doi.org/10.17863/cam.14165
https://www.repository.cam.ac.uk/handle/1810/268053
geographic Arctic
Greenland
Svalbard
geographic_facet Arctic
Greenland
Svalbard
genre Arctic
East Greenland
Greenland
Greenland Sea
Svalbard
genre_facet Arctic
East Greenland
Greenland
Greenland Sea
Svalbard
op_rights All Rights Reserved
https://www.rioxx.net/licenses/all-rights-reserved/
op_doi https://doi.org/10.17863/cam.14165
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