An objective technique for Arctic cloud analysis using multispectral AVHRR satellite imagery

An established cloud analysis routine has been modified for use in the Arctic. The separation of clouds from the snow and sea ice backgrounds is accomplished through a multispectral technique which utilizes VHRR channel 2 (visible), channel 3 (near infrared) and channel 4 (infrared) data. The primar...

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Main Author: Barron, John P.
Other Authors: Durkee, Philip A., Wash, Carlyle H.
Format: Thesis
Language:English
Published: Monterey, California. Naval Postgraduate School 1988
Subjects:
Online Access:https://hdl.handle.net/10945/23335
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record_format openpolar
spelling ftnavalpschool:oai:calhoun.nps.edu:10945/23335 2024-06-09T07:43:26+00:00 An objective technique for Arctic cloud analysis using multispectral AVHRR satellite imagery Barron, John P. Durkee, Philip A. Wash, Carlyle H. 1988-03 80 p. application/pdf https://hdl.handle.net/10945/23335 en_US eng Monterey, California. Naval Postgraduate School https://hdl.handle.net/10945/23335 This publication is a work of the U.S. Government as defined in Title 17, United States Code, Section 101. Copyright protection is not available for this work in the United States. arctic cloud analysis AVHRR channel 3 snow/cloud discrimination Meteorology Thesis 1988 ftnavalpschool 2024-05-15T00:18:56Z An established cloud analysis routine has been modified for use in the Arctic. The separation of clouds from the snow and sea ice backgrounds is accomplished through a multispectral technique which utilizes VHRR channel 2 (visible), channel 3 (near infrared) and channel 4 (infrared) data. The primary means of cloud identification is based on a derived channel 3 reflectance image. At this wavelength, a significant contrast exists between liquid clouds and the arctic backgrounds, unlike in the standard visible and infrared images. The channel 3 reflectance is obtained by first using the channel 4 emission temperature to estimate the thermal emission component of the total channel 3 radiance. This thermal emission component is subsequently removed from the total radiance, leaving only the solar reflectance component available for analysis. Since many ice clouds do not exhibit a substantially greater reflectance is channel 3, the routine exploits differences in transmissive characteristics between channels 3 and 4 for identification. The routine was applied to six case studies which had been analyzed by three independent experts to establish 'ground truth'. Verification of the cloud analysis results, through a comparison to the subjective analyses, yielded impressive statistics. A success rate of 77.9% was obtained with an arguably small data base of 131 undisputed scenes Approved for public release; distribution is unlimited. Lieutenant, United States Navy http://archive.org/details/anobjectivetechn1094523335 Thesis Arctic Sea ice Naval Postgraduate School: Calhoun Arctic
institution Open Polar
collection Naval Postgraduate School: Calhoun
op_collection_id ftnavalpschool
language English
topic arctic cloud analysis
AVHRR channel 3
snow/cloud discrimination
Meteorology
spellingShingle arctic cloud analysis
AVHRR channel 3
snow/cloud discrimination
Meteorology
Barron, John P.
An objective technique for Arctic cloud analysis using multispectral AVHRR satellite imagery
topic_facet arctic cloud analysis
AVHRR channel 3
snow/cloud discrimination
Meteorology
description An established cloud analysis routine has been modified for use in the Arctic. The separation of clouds from the snow and sea ice backgrounds is accomplished through a multispectral technique which utilizes VHRR channel 2 (visible), channel 3 (near infrared) and channel 4 (infrared) data. The primary means of cloud identification is based on a derived channel 3 reflectance image. At this wavelength, a significant contrast exists between liquid clouds and the arctic backgrounds, unlike in the standard visible and infrared images. The channel 3 reflectance is obtained by first using the channel 4 emission temperature to estimate the thermal emission component of the total channel 3 radiance. This thermal emission component is subsequently removed from the total radiance, leaving only the solar reflectance component available for analysis. Since many ice clouds do not exhibit a substantially greater reflectance is channel 3, the routine exploits differences in transmissive characteristics between channels 3 and 4 for identification. The routine was applied to six case studies which had been analyzed by three independent experts to establish 'ground truth'. Verification of the cloud analysis results, through a comparison to the subjective analyses, yielded impressive statistics. A success rate of 77.9% was obtained with an arguably small data base of 131 undisputed scenes Approved for public release; distribution is unlimited. Lieutenant, United States Navy http://archive.org/details/anobjectivetechn1094523335
author2 Durkee, Philip A.
Wash, Carlyle H.
format Thesis
author Barron, John P.
author_facet Barron, John P.
author_sort Barron, John P.
title An objective technique for Arctic cloud analysis using multispectral AVHRR satellite imagery
title_short An objective technique for Arctic cloud analysis using multispectral AVHRR satellite imagery
title_full An objective technique for Arctic cloud analysis using multispectral AVHRR satellite imagery
title_fullStr An objective technique for Arctic cloud analysis using multispectral AVHRR satellite imagery
title_full_unstemmed An objective technique for Arctic cloud analysis using multispectral AVHRR satellite imagery
title_sort objective technique for arctic cloud analysis using multispectral avhrr satellite imagery
publisher Monterey, California. Naval Postgraduate School
publishDate 1988
url https://hdl.handle.net/10945/23335
geographic Arctic
geographic_facet Arctic
genre Arctic
Sea ice
genre_facet Arctic
Sea ice
op_relation https://hdl.handle.net/10945/23335
op_rights This publication is a work of the U.S. Government as defined in Title 17, United States Code, Section 101. Copyright protection is not available for this work in the United States.
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