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    Physical Basis, Premises, and Self-Consistency Checks of Aerosol Retrievals from TRMM VIRS

    Source: Journal of Applied Meteorology:;2000:;volume( 039 ):;issue: 012::page 2259
    Author:
    Ignatov, Alexander
    ,
    Stowe, Larry
    DOI: 10.1175/1520-0450(2001)040<2259:PBPASC>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: This paper outlines the processing stream for aerosol retrievals over oceans from the visible and infrared scanner [VIRS; a five-channel radiometer similar to the National Oceanic and Atmospheric Administration?s Advanced Very High Resolution Radiometer (AVHRR)] aboard the Tropical Rainfall Measuring Mission (TRMM) satellite, launched in November 1997. Emphasis is on 1) the applying the previously developed AVHRR second-generation aerosol retrieval algorithm to VIRS data to derive an aerosol parameter, indicative of particle size; 2) removing the unwanted ?thermal leak? signal in the 1.61-?m channel; 3) giving examples of the first aerosol retrievals from space at this wavelength; and 4) assessing the accuracy of the retrievals with theoretical error analyses and empirical self- and interconsistency checks. Aerosol optical depths τA1 and τA2 are retrieved from reflected solar radiances in VIRS channels 1 and 2 centered at wavelengths ?1 = 0.63 and ?2 = 1.61 ?m, using two independent lookup tables. When τA1 and τA2 exceed a certain threshold τAmin an effective Ångström exponent α related to particle size is derived as α = ?ln(τA1/τA2)/ln(?1/?2). Channel 2 is contaminated by a thermal leak, originating from a secondary spectral response peak centered at ?5.2 ?m. If uncorrected, it leads to errors in τA2 of 100% or more. To minimize this error, nighttime VIRS ?dark? radiances in channel 2 have been related empirically to radiances in channels 4 and 5 (10.8 and 12 ?m, respectively), and view angle through regression analyses. The reflected component in channel-2 daytime measurements is estimated by subtracting the empirically derived thermal component from the total signal and is used in the retrieval of τA2. Theoretical error analysis is used to identify the limitations of the VIRS retrieval algorithm, whereas actual retrievals are preliminarily evaluated using a set of specially developed empirical checks. The checks show, on average, a high degree of self- and interconsistency but also identify problems with the retrievals, the most noteworthy being trends in retrieved optical depths with viewing and illumination angles. These problems will be tackled in the next-generation aerosol retrieval algorithm.
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      Physical Basis, Premises, and Self-Consistency Checks of Aerosol Retrievals from TRMM VIRS

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4148518
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    contributor authorIgnatov, Alexander
    contributor authorStowe, Larry
    date accessioned2017-06-09T14:08:13Z
    date available2017-06-09T14:08:13Z
    date copyright2000/12/01
    date issued2000
    identifier issn0894-8763
    identifier otherams-13104.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4148518
    description abstractThis paper outlines the processing stream for aerosol retrievals over oceans from the visible and infrared scanner [VIRS; a five-channel radiometer similar to the National Oceanic and Atmospheric Administration?s Advanced Very High Resolution Radiometer (AVHRR)] aboard the Tropical Rainfall Measuring Mission (TRMM) satellite, launched in November 1997. Emphasis is on 1) the applying the previously developed AVHRR second-generation aerosol retrieval algorithm to VIRS data to derive an aerosol parameter, indicative of particle size; 2) removing the unwanted ?thermal leak? signal in the 1.61-?m channel; 3) giving examples of the first aerosol retrievals from space at this wavelength; and 4) assessing the accuracy of the retrievals with theoretical error analyses and empirical self- and interconsistency checks. Aerosol optical depths τA1 and τA2 are retrieved from reflected solar radiances in VIRS channels 1 and 2 centered at wavelengths ?1 = 0.63 and ?2 = 1.61 ?m, using two independent lookup tables. When τA1 and τA2 exceed a certain threshold τAmin an effective Ångström exponent α related to particle size is derived as α = ?ln(τA1/τA2)/ln(?1/?2). Channel 2 is contaminated by a thermal leak, originating from a secondary spectral response peak centered at ?5.2 ?m. If uncorrected, it leads to errors in τA2 of 100% or more. To minimize this error, nighttime VIRS ?dark? radiances in channel 2 have been related empirically to radiances in channels 4 and 5 (10.8 and 12 ?m, respectively), and view angle through regression analyses. The reflected component in channel-2 daytime measurements is estimated by subtracting the empirically derived thermal component from the total signal and is used in the retrieval of τA2. Theoretical error analysis is used to identify the limitations of the VIRS retrieval algorithm, whereas actual retrievals are preliminarily evaluated using a set of specially developed empirical checks. The checks show, on average, a high degree of self- and interconsistency but also identify problems with the retrievals, the most noteworthy being trends in retrieved optical depths with viewing and illumination angles. These problems will be tackled in the next-generation aerosol retrieval algorithm.
    publisherAmerican Meteorological Society
    titlePhysical Basis, Premises, and Self-Consistency Checks of Aerosol Retrievals from TRMM VIRS
    typeJournal Paper
    journal volume39
    journal issue12
    journal titleJournal of Applied Meteorology
    identifier doi10.1175/1520-0450(2001)040<2259:PBPASC>2.0.CO;2
    journal fristpage2259
    journal lastpage2277
    treeJournal of Applied Meteorology:;2000:;volume( 039 ):;issue: 012
    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