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    A Pattern Recognition Technique for Distinguishing Surface and Cloud Types in the Polar Regions

    Source: Journal of Climate and Applied Meteorology:;1987:;Volume( 026 ):;Issue: 010::page 1412
    Author:
    Ebert, Elizabeth
    DOI: 10.1175/1520-0450(1987)026<1412:APRTFD>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Measurement of polar cloud cover is important because of its strong radiative influence on the energy balance of the snow and ice surface. Conventional satellite cloud detection schemes often fail in the polar regions because the visible and thermal contrasts between cloud and surface are typically small. Nevertheless, experts looking at satellite imagery can distinguish clouds from the surface by examining the textural characteristics of the scene. This paper describes an automated pattern recognition algorithm winch identities regions of various surface and cloud types at high latitudes from visible, near-infrared, and infrared AVHRR satellite data. Five spectral features give information about the magnitude of albedos and brightness temperatures, while three textural features describe the variability and ?bumpiness? in a scene. The maximum likelihood decision rule is used to classify that region into one of seven surface categories or 11 cloud categories. The algorithm was able to classify 870 training samples with a skill of 84%. Eighteen hundred artificer samples created using a Monte Carlo technique were classified with a skill of 92%, which represents the theoretical limit of class separability using the given features. Both the near-infrared information and the textural information proved to be especially useful in detecting high-latitude cloudiness. The algorithm experienced some difficulty identifying thin stratus over snow and ice and thin cirrus over land and water, situations which also prove difficult for most other cloud detection schemes. When tested on AVHRR imagery from a different date, the algorithm showed a skill of 83% as verified against the analyses of three independent experts. Significant variability was encountered among the experts, underlining the need for an objective routine. This algorithm performed more accurately thin others constructed with alternate feature sets corresponding to various existing cloud detection schemes.
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      A Pattern Recognition Technique for Distinguishing Surface and Cloud Types in the Polar Regions

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4146453
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    contributor authorEbert, Elizabeth
    date accessioned2017-06-09T14:02:01Z
    date available2017-06-09T14:02:01Z
    date copyright1987/10/01
    date issued1987
    identifier issn0733-3021
    identifier otherams-11246.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4146453
    description abstractMeasurement of polar cloud cover is important because of its strong radiative influence on the energy balance of the snow and ice surface. Conventional satellite cloud detection schemes often fail in the polar regions because the visible and thermal contrasts between cloud and surface are typically small. Nevertheless, experts looking at satellite imagery can distinguish clouds from the surface by examining the textural characteristics of the scene. This paper describes an automated pattern recognition algorithm winch identities regions of various surface and cloud types at high latitudes from visible, near-infrared, and infrared AVHRR satellite data. Five spectral features give information about the magnitude of albedos and brightness temperatures, while three textural features describe the variability and ?bumpiness? in a scene. The maximum likelihood decision rule is used to classify that region into one of seven surface categories or 11 cloud categories. The algorithm was able to classify 870 training samples with a skill of 84%. Eighteen hundred artificer samples created using a Monte Carlo technique were classified with a skill of 92%, which represents the theoretical limit of class separability using the given features. Both the near-infrared information and the textural information proved to be especially useful in detecting high-latitude cloudiness. The algorithm experienced some difficulty identifying thin stratus over snow and ice and thin cirrus over land and water, situations which also prove difficult for most other cloud detection schemes. When tested on AVHRR imagery from a different date, the algorithm showed a skill of 83% as verified against the analyses of three independent experts. Significant variability was encountered among the experts, underlining the need for an objective routine. This algorithm performed more accurately thin others constructed with alternate feature sets corresponding to various existing cloud detection schemes.
    publisherAmerican Meteorological Society
    titleA Pattern Recognition Technique for Distinguishing Surface and Cloud Types in the Polar Regions
    typeJournal Paper
    journal volume26
    journal issue10
    journal titleJournal of Climate and Applied Meteorology
    identifier doi10.1175/1520-0450(1987)026<1412:APRTFD>2.0.CO;2
    journal fristpage1412
    journal lastpage1427
    treeJournal of Climate and Applied Meteorology:;1987:;Volume( 026 ):;Issue: 010
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
    yabeshDSpacePersian