id ftdtic:ADA186685
record_format openpolar
spelling ftdtic:ADA186685 2023-05-15T15:39:45+02:00 Active and Passive Remote Sensing of Ice. Kong, Jin A MASSACHUSETTS INST OF TECH CAMBRIDGE RESEARCH LAB OF ELECTRONICS 1987-07-31 text/html http://www.dtic.mil/docs/citations/ADA186685 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA186685 en eng http://www.dtic.mil/docs/citations/ADA186685 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS Snow Ice and Permafrost Radiofrequency Wave Propagation *ELECTROMAGNETIC SCATTERING *SEA ICE ANISOTROPY BACKSCATTERING SCATTERING CROSS SECTIONS LAYERS CROSS POLARIZATION MOMENTS ELECTROMAGNETIC WAVE PROPAGATION FORMULATIONS MIXING ORIENTATION(DIRECTION) BISTATIC DETECTION COEFFICIENTS CORRELATION SCATTERING VARIATIONS MIXTURES PHASE MATHEMATICAL MODELS POLARIZATION COVARIANCE BARROW(ALASKA) RADAR POLARIMETRY CLUTTER GREENS FUNCTIONS ICE MEAN APPROXIMATION(MATHEMATICS) NONLINEAR SYSTEMS SNOW COVER LENGTH VERTICAL ORIENTATION WAVE PROPAGATION HORIZONTAL ORIENTATION DIELECTRIC PROPERTIES MICROWAVES REMOTE SYSTEMS ELLIPSOIDS VOLUME Permittivity Multiphase mixtures Active detectors Volume scattering. Text 1987 ftdtic 2016-02-21T14:25:54Z We have studied volume scattering effects of snow-covered sea ice with a three-layer random medium model for microwave remote sensing. Strong fluctuation theory and bilocal approximation are applied to calculate the effective permittivities for snow and sea ice. Wave scattering theory, in conjunction with the distorted Born approximation, is then used to compute bistatic coefficients and backscattering cross sections. We also derived a general mixing formula for discrete scatterers immersed in a host medium. The results are applicable to general multiphase mixtures, and the scattering ellipsoids of the different phases can have different sizes and arbitrary ellipticity distribution and axis orientation, i.e., the mixture may be isotropic or anisotropic. The Mueller matrix and polarization covariance matrix are described for polarimetric radar systems. Clutter is modelled by a layer of random permittivity, described by a three-dimensional correlation function, with variance, and horizontal and vertical correlation lengths. Study of the strong fluctuation theory for a bounded layer of random discrete scatterers is extended to include high-order co-polarized and cross-polarized second moments. We have derived the dyadic Green's function for a two-layer anisotropic medium. The Born approximation is used to calculate the scattered fields. Electromagnetic wave propagation and scattering in an anisotropic random medium was examined with Dyson equation for the mean field. This is solved by bilocal and nonlinear approximations and with Bethe-Salpeter equation for the correlation of field. Text Barrow Ice permafrost Sea ice Alaska Defense Technical Information Center: DTIC Technical Reports database Mueller ENVELOPE(55.533,55.533,-66.917,-66.917)
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
*ELECTROMAGNETIC SCATTERING
*SEA ICE
ANISOTROPY
BACKSCATTERING
SCATTERING CROSS SECTIONS
LAYERS
CROSS POLARIZATION
MOMENTS
ELECTROMAGNETIC WAVE PROPAGATION
FORMULATIONS
MIXING
ORIENTATION(DIRECTION)
BISTATIC DETECTION
COEFFICIENTS
CORRELATION
SCATTERING
VARIATIONS
MIXTURES
PHASE
MATHEMATICAL MODELS
POLARIZATION
COVARIANCE
BARROW(ALASKA)
RADAR
POLARIMETRY
CLUTTER
GREENS FUNCTIONS
ICE
MEAN
APPROXIMATION(MATHEMATICS)
NONLINEAR SYSTEMS
SNOW COVER
LENGTH
VERTICAL ORIENTATION
WAVE PROPAGATION
HORIZONTAL ORIENTATION
DIELECTRIC PROPERTIES
MICROWAVES
REMOTE SYSTEMS
ELLIPSOIDS
VOLUME
Permittivity
Multiphase mixtures
Active detectors
Volume scattering.
spellingShingle Snow
Ice and Permafrost
Radiofrequency Wave Propagation
*ELECTROMAGNETIC SCATTERING
*SEA ICE
ANISOTROPY
BACKSCATTERING
SCATTERING CROSS SECTIONS
LAYERS
CROSS POLARIZATION
MOMENTS
ELECTROMAGNETIC WAVE PROPAGATION
FORMULATIONS
MIXING
ORIENTATION(DIRECTION)
BISTATIC DETECTION
COEFFICIENTS
CORRELATION
SCATTERING
VARIATIONS
MIXTURES
PHASE
MATHEMATICAL MODELS
POLARIZATION
COVARIANCE
BARROW(ALASKA)
RADAR
POLARIMETRY
CLUTTER
GREENS FUNCTIONS
ICE
MEAN
APPROXIMATION(MATHEMATICS)
NONLINEAR SYSTEMS
SNOW COVER
LENGTH
VERTICAL ORIENTATION
WAVE PROPAGATION
HORIZONTAL ORIENTATION
DIELECTRIC PROPERTIES
MICROWAVES
REMOTE SYSTEMS
ELLIPSOIDS
VOLUME
Permittivity
Multiphase mixtures
Active detectors
Volume scattering.
Kong, Jin A
Active and Passive Remote Sensing of Ice.
topic_facet Snow
Ice and Permafrost
Radiofrequency Wave Propagation
*ELECTROMAGNETIC SCATTERING
*SEA ICE
ANISOTROPY
BACKSCATTERING
SCATTERING CROSS SECTIONS
LAYERS
CROSS POLARIZATION
MOMENTS
ELECTROMAGNETIC WAVE PROPAGATION
FORMULATIONS
MIXING
ORIENTATION(DIRECTION)
BISTATIC DETECTION
COEFFICIENTS
CORRELATION
SCATTERING
VARIATIONS
MIXTURES
PHASE
MATHEMATICAL MODELS
POLARIZATION
COVARIANCE
BARROW(ALASKA)
RADAR
POLARIMETRY
CLUTTER
GREENS FUNCTIONS
ICE
MEAN
APPROXIMATION(MATHEMATICS)
NONLINEAR SYSTEMS
SNOW COVER
LENGTH
VERTICAL ORIENTATION
WAVE PROPAGATION
HORIZONTAL ORIENTATION
DIELECTRIC PROPERTIES
MICROWAVES
REMOTE SYSTEMS
ELLIPSOIDS
VOLUME
Permittivity
Multiphase mixtures
Active detectors
Volume scattering.
description We have studied volume scattering effects of snow-covered sea ice with a three-layer random medium model for microwave remote sensing. Strong fluctuation theory and bilocal approximation are applied to calculate the effective permittivities for snow and sea ice. Wave scattering theory, in conjunction with the distorted Born approximation, is then used to compute bistatic coefficients and backscattering cross sections. We also derived a general mixing formula for discrete scatterers immersed in a host medium. The results are applicable to general multiphase mixtures, and the scattering ellipsoids of the different phases can have different sizes and arbitrary ellipticity distribution and axis orientation, i.e., the mixture may be isotropic or anisotropic. The Mueller matrix and polarization covariance matrix are described for polarimetric radar systems. Clutter is modelled by a layer of random permittivity, described by a three-dimensional correlation function, with variance, and horizontal and vertical correlation lengths. Study of the strong fluctuation theory for a bounded layer of random discrete scatterers is extended to include high-order co-polarized and cross-polarized second moments. We have derived the dyadic Green's function for a two-layer anisotropic medium. The Born approximation is used to calculate the scattered fields. Electromagnetic wave propagation and scattering in an anisotropic random medium was examined with Dyson equation for the mean field. This is solved by bilocal and nonlinear approximations and with Bethe-Salpeter equation for the correlation of field.
author2 MASSACHUSETTS INST OF TECH CAMBRIDGE RESEARCH LAB OF ELECTRONICS
format Text
author Kong, Jin A
author_facet Kong, Jin A
author_sort Kong, Jin 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 1987
url http://www.dtic.mil/docs/citations/ADA186685
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA186685
long_lat ENVELOPE(55.533,55.533,-66.917,-66.917)
geographic Mueller
geographic_facet Mueller
genre Barrow
Ice
permafrost
Sea ice
Alaska
genre_facet Barrow
Ice
permafrost
Sea ice
Alaska
op_source DTIC AND NTIS
op_relation http://www.dtic.mil/docs/citations/ADA186685
op_rights APPROVED FOR PUBLIC RELEASE
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