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...

Full description

Bibliographic Details
Main Author: Kong,J A
Other Authors: MASSACHUSETTS INST OF TECH CAMBRIDGE RESEARCH LAB OF ELECTRONICS
Format: Text
Language:English
Published: 1984
Subjects:
Ice
Online Access:http://www.dtic.mil/docs/citations/ADA154406
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA154406
id ftdtic:ADA154406
record_format openpolar
spelling 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
institution Open Polar
collection 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