Microwave Emission from Polar Surfaces.

Based on the work described in this report, our observations and modeling work have revealed several considerations which are central to understanding the physical basis for the application and interpretation of thin ice algorithms for passive microwave imagery. We have shown that passive microwave...

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Bibliographic Details
Main Author: Grenfell, Thomas C.
Other Authors: WASHINGTON UNIV SEATTLE DEPT OF ATMOSPHERIC SCIENCES
Format: Text
Language:English
Published: 1998
Subjects:
Ari
Online Access:http://www.dtic.mil/docs/citations/ADA343249
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA343249
id ftdtic:ADA343249
record_format openpolar
spelling ftdtic:ADA343249 2023-05-15T18:17:52+02:00 Microwave Emission from Polar Surfaces. Grenfell, Thomas C. WASHINGTON UNIV SEATTLE DEPT OF ATMOSPHERIC SCIENCES 1998-04-01 text/html http://www.dtic.mil/docs/citations/ADA343249 http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA343249 en eng http://www.dtic.mil/docs/citations/ADA343249 APPROVED FOR PUBLIC RELEASE DTIC AND NTIS Radiofrequency Wave Propagation Geography *MICROWAVES *POLAR CAP ALGORITHMS EMISSION PHYSICAL PROPERTIES PASSIVE SYSTEMS RADIATIVE TRANSFER SURFACES MICROWAVE FREQUENCY EMISSIVITY Text 1998 ftdtic 2016-02-19T22:26:42Z Based on the work described in this report, our observations and modeling work have revealed several considerations which are central to understanding the physical basis for the application and interpretation of thin ice algorithms for passive microwave imagery. We have shown that passive microwave measurements provide one of the most robust remote sensing techniques for distinguishing among sea ice types including the thin ice types that are pivotal for regional energy considerations. We have found that current theories applicable at microwave frequencies (multi layer SFT wave theory, for example) and in the visible and infrared (radiative transfer theory) can reproduce the radiation signatures of FY ice types quite well incorporating the actual physical structure of the ice. As a result of the cooperative work carried out during the electromagnetics ARI, the determination of the wavelength regions and physical situations appropriate for the application of various radiation models has been improved considerably, and our results, both theoretical and observational, have demonstrate the levels of accuracy of the models. It is clear that our understanding of the microwave emissivities of sea ice and their relation to other types of remote sensing signatures has increased significantly in the course of this grant. Text Sea ice Defense Technical Information Center: DTIC Technical Reports database Ari ENVELOPE(147.813,147.813,59.810,59.810)
institution Open Polar
collection Defense Technical Information Center: DTIC Technical Reports database
op_collection_id ftdtic
language English
topic Radiofrequency Wave Propagation
Geography
*MICROWAVES
*POLAR CAP
ALGORITHMS
EMISSION
PHYSICAL PROPERTIES
PASSIVE SYSTEMS
RADIATIVE TRANSFER
SURFACES
MICROWAVE FREQUENCY
EMISSIVITY
spellingShingle Radiofrequency Wave Propagation
Geography
*MICROWAVES
*POLAR CAP
ALGORITHMS
EMISSION
PHYSICAL PROPERTIES
PASSIVE SYSTEMS
RADIATIVE TRANSFER
SURFACES
MICROWAVE FREQUENCY
EMISSIVITY
Grenfell, Thomas C.
Microwave Emission from Polar Surfaces.
topic_facet Radiofrequency Wave Propagation
Geography
*MICROWAVES
*POLAR CAP
ALGORITHMS
EMISSION
PHYSICAL PROPERTIES
PASSIVE SYSTEMS
RADIATIVE TRANSFER
SURFACES
MICROWAVE FREQUENCY
EMISSIVITY
description Based on the work described in this report, our observations and modeling work have revealed several considerations which are central to understanding the physical basis for the application and interpretation of thin ice algorithms for passive microwave imagery. We have shown that passive microwave measurements provide one of the most robust remote sensing techniques for distinguishing among sea ice types including the thin ice types that are pivotal for regional energy considerations. We have found that current theories applicable at microwave frequencies (multi layer SFT wave theory, for example) and in the visible and infrared (radiative transfer theory) can reproduce the radiation signatures of FY ice types quite well incorporating the actual physical structure of the ice. As a result of the cooperative work carried out during the electromagnetics ARI, the determination of the wavelength regions and physical situations appropriate for the application of various radiation models has been improved considerably, and our results, both theoretical and observational, have demonstrate the levels of accuracy of the models. It is clear that our understanding of the microwave emissivities of sea ice and their relation to other types of remote sensing signatures has increased significantly in the course of this grant.
author2 WASHINGTON UNIV SEATTLE DEPT OF ATMOSPHERIC SCIENCES
format Text
author Grenfell, Thomas C.
author_facet Grenfell, Thomas C.
author_sort Grenfell, Thomas C.
title Microwave Emission from Polar Surfaces.
title_short Microwave Emission from Polar Surfaces.
title_full Microwave Emission from Polar Surfaces.
title_fullStr Microwave Emission from Polar Surfaces.
title_full_unstemmed Microwave Emission from Polar Surfaces.
title_sort microwave emission from polar surfaces.
publishDate 1998
url http://www.dtic.mil/docs/citations/ADA343249
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA343249
long_lat ENVELOPE(147.813,147.813,59.810,59.810)
geographic Ari
geographic_facet Ari
genre Sea ice
genre_facet Sea ice
op_source DTIC AND NTIS
op_relation http://www.dtic.mil/docs/citations/ADA343249
op_rights APPROVED FOR PUBLIC RELEASE
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