Active and Passive Remote Sensing of Ice.
This is a report on the progress that has been made in the study of active and passive remote sensing of ice during the period of February 1, 1984. During this period we have: (1) calculated the emissivity of a two-layer anisotropic random medium; and (2) participated in the microwave sea ice measur...
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ftdtic:ADA154406 2023-05-15T15:55:49+02:00 Active and Passive Remote Sensing of Ice. Kong,J A MASSACHUSETTS INST OF TECH CAMBRIDGE RESEARCH LAB OF ELECTRONICS 1984-09 text/html http://www.dtic.mil/docs/citations/ADA154406 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA154406 en eng http://www.dtic.mil/docs/citations/ADA154406 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS Snow Ice and Permafrost Radiofrequency Wave Propagation *MICROWAVES *ELECTROMAGNETIC SCATTERING *RADAR *ICE *SEA ICE MEASUREMENT SCATTERING FIELD TESTS ORIENTATION(DIRECTION) PASSIVE SYSTEMS COEFFICIENTS REMOTE DETECTORS CANOPIES INCOHERENT SCATTERING REFLECTIVITY GREENS FUNCTIONS VEGETATION AZIMUTH HEMISPHERES RADIOMETRY PLOTTING Remote sensing Text 1984 ftdtic 2016-02-21T00:22:07Z This is a report on the progress that has been made in the study of active and passive remote sensing of ice during the period of February 1, 1984. During this period we have: (1) calculated the emissivity of a two-layer anisotropic random medium; and (2) participated in the microwave sea ice measurement program at the Cold Regions Research and Engineering Laboratory (CRREL). The emissivity of a two-layer anisotropic random medium has been calculated using the dyadic Green's function for a two-layer anisotropic medium and the first-order Born approximation. The emissivity is calculated by obtaining coherent and incoherent reflectivities and by making use of the relationship e=1-r. The incoherent reflectivity is obtained by integrating over the upper hemisphere the bistatic scattering coefficients obtained under the Born approximation. The theoretical results are illustrated by plotting the emissivities as functions of viewing angles and polarizations. They are used to interpret the passive microwave remote sensing data from vegetation canopy which also show strong anisotropic dependencies. Data obtained from the field measurements with corn stalks arranged in various configurations with perferred azimuthal directions are successfully interpreted with this model. It is expected that the radiometric data from CREEL measurements will also be successfully interpreted with this theoretical model. A manuscript has been prepared for submission to a journal for publication. Text Cold Regions Research and Engineering Laboratory Ice permafrost Sea ice Defense Technical Information Center: DTIC Technical Reports database |
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Open Polar |
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Defense Technical Information Center: DTIC Technical Reports database |
op_collection_id |
ftdtic |
language |
English |
topic |
Snow Ice and Permafrost Radiofrequency Wave Propagation *MICROWAVES *ELECTROMAGNETIC SCATTERING *RADAR *ICE *SEA ICE MEASUREMENT SCATTERING FIELD TESTS ORIENTATION(DIRECTION) PASSIVE SYSTEMS COEFFICIENTS REMOTE DETECTORS CANOPIES INCOHERENT SCATTERING REFLECTIVITY GREENS FUNCTIONS VEGETATION AZIMUTH HEMISPHERES RADIOMETRY PLOTTING Remote sensing |
spellingShingle |
Snow Ice and Permafrost Radiofrequency Wave Propagation *MICROWAVES *ELECTROMAGNETIC SCATTERING *RADAR *ICE *SEA ICE MEASUREMENT SCATTERING FIELD TESTS ORIENTATION(DIRECTION) PASSIVE SYSTEMS COEFFICIENTS REMOTE DETECTORS CANOPIES INCOHERENT SCATTERING REFLECTIVITY GREENS FUNCTIONS VEGETATION AZIMUTH HEMISPHERES RADIOMETRY PLOTTING Remote sensing Kong,J A Active and Passive Remote Sensing of Ice. |
topic_facet |
Snow Ice and Permafrost Radiofrequency Wave Propagation *MICROWAVES *ELECTROMAGNETIC SCATTERING *RADAR *ICE *SEA ICE MEASUREMENT SCATTERING FIELD TESTS ORIENTATION(DIRECTION) PASSIVE SYSTEMS COEFFICIENTS REMOTE DETECTORS CANOPIES INCOHERENT SCATTERING REFLECTIVITY GREENS FUNCTIONS VEGETATION AZIMUTH HEMISPHERES RADIOMETRY PLOTTING Remote sensing |
description |
This is a report on the progress that has been made in the study of active and passive remote sensing of ice during the period of February 1, 1984. During this period we have: (1) calculated the emissivity of a two-layer anisotropic random medium; and (2) participated in the microwave sea ice measurement program at the Cold Regions Research and Engineering Laboratory (CRREL). The emissivity of a two-layer anisotropic random medium has been calculated using the dyadic Green's function for a two-layer anisotropic medium and the first-order Born approximation. The emissivity is calculated by obtaining coherent and incoherent reflectivities and by making use of the relationship e=1-r. The incoherent reflectivity is obtained by integrating over the upper hemisphere the bistatic scattering coefficients obtained under the Born approximation. The theoretical results are illustrated by plotting the emissivities as functions of viewing angles and polarizations. They are used to interpret the passive microwave remote sensing data from vegetation canopy which also show strong anisotropic dependencies. Data obtained from the field measurements with corn stalks arranged in various configurations with perferred azimuthal directions are successfully interpreted with this model. It is expected that the radiometric data from CREEL measurements will also be successfully interpreted with this theoretical model. A manuscript has been prepared for submission to a journal for publication. |
author2 |
MASSACHUSETTS INST OF TECH CAMBRIDGE RESEARCH LAB OF ELECTRONICS |
format |
Text |
author |
Kong,J A |
author_facet |
Kong,J A |
author_sort |
Kong,J A |
title |
Active and Passive Remote Sensing of Ice. |
title_short |
Active and Passive Remote Sensing of Ice. |
title_full |
Active and Passive Remote Sensing of Ice. |
title_fullStr |
Active and Passive Remote Sensing of Ice. |
title_full_unstemmed |
Active and Passive Remote Sensing of Ice. |
title_sort |
active and passive remote sensing of ice. |
publishDate |
1984 |
url |
http://www.dtic.mil/docs/citations/ADA154406 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA154406 |
genre |
Cold Regions Research and Engineering Laboratory Ice permafrost Sea ice |
genre_facet |
Cold Regions Research and Engineering Laboratory Ice permafrost Sea ice |
op_source |
DTIC AND NTIS |
op_relation |
http://www.dtic.mil/docs/citations/ADA154406 |
op_rights |
APPROVED FOR PUBLIC RELEASE |
_version_ |
1766391313550278656 |