Active microwave remote sensing of an anisotropic random medium layer
A two-layer anisotropic random medium model has been developed to study the active remote sensing of the earth. The dyadic Green's function for a two-layer anisotropic medium is developed and used in conjunction with the first-order Born approximation to calculate the backscattering coefficient...
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ftnasantrs:oai:casi.ntrs.nasa.gov:19860032798 2023-05-15T18:17:58+02:00 Active microwave remote sensing of an anisotropic random medium layer Lee, J. K. Kong, J. A. Unclassified, Unlimited, Publicly available Nov 1, 1985 http://ntrs.nasa.gov/search.jsp?R=19860032798 unknown http://ntrs.nasa.gov/search.jsp?R=19860032798 Accession ID: 86A17536 Copyright Other Sources 43 IEEE Transactions on Geoscience and Remote Sensing; GE-23; 910-923 AD-A169046 1985 ftnasantrs 2012-02-15T16:42:36Z A two-layer anisotropic random medium model has been developed to study the active remote sensing of the earth. The dyadic Green's function for a two-layer anisotropic medium is developed and used in conjunction with the first-order Born approximation to calculate the backscattering coefficients. It is shown that strong cross-polarization occurs in the single scattering process and is indispensable in the interpretation of radar measurements of sea ice at different frequencies, polarizations, and viewing angles. The effects of anisotropy on the angular responses of backscattering coefficients are also illustrated. Other/Unknown Material Sea ice NASA Technical Reports Server (NTRS) |
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NASA Technical Reports Server (NTRS) |
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43 |
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43 Lee, J. K. Kong, J. A. Active microwave remote sensing of an anisotropic random medium layer |
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43 |
description |
A two-layer anisotropic random medium model has been developed to study the active remote sensing of the earth. The dyadic Green's function for a two-layer anisotropic medium is developed and used in conjunction with the first-order Born approximation to calculate the backscattering coefficients. It is shown that strong cross-polarization occurs in the single scattering process and is indispensable in the interpretation of radar measurements of sea ice at different frequencies, polarizations, and viewing angles. The effects of anisotropy on the angular responses of backscattering coefficients are also illustrated. |
format |
Other/Unknown Material |
author |
Lee, J. K. Kong, J. A. |
author_facet |
Lee, J. K. Kong, J. A. |
author_sort |
Lee, J. K. |
title |
Active microwave remote sensing of an anisotropic random medium layer |
title_short |
Active microwave remote sensing of an anisotropic random medium layer |
title_full |
Active microwave remote sensing of an anisotropic random medium layer |
title_fullStr |
Active microwave remote sensing of an anisotropic random medium layer |
title_full_unstemmed |
Active microwave remote sensing of an anisotropic random medium layer |
title_sort |
active microwave remote sensing of an anisotropic random medium layer |
publishDate |
1985 |
url |
http://ntrs.nasa.gov/search.jsp?R=19860032798 |
op_coverage |
Unclassified, Unlimited, Publicly available |
genre |
Sea ice |
genre_facet |
Sea ice |
op_source |
Other Sources |
op_relation |
http://ntrs.nasa.gov/search.jsp?R=19860032798 Accession ID: 86A17536 |
op_rights |
Copyright |
_version_ |
1766193817823739904 |