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    An Evaluation of Depth Resolution Requirements for Optical Profiling in Coastal Waters

    Source: Journal of Atmospheric and Oceanic Technology:;2004:;volume( 021 ):;issue: 007::page 1059
    Author:
    Zibordi, Giuseppe
    ,
    D'Alimonte, Davide
    ,
    Berthon, Jean-François
    DOI: 10.1175/1520-0426(2004)021<1059:AEODRR>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Wave perturbations induce uncertainties in subsurface quantities determined from the extrapolation of optical measurements taken at different depths. An analysis of these uncertainties was made using data collected in the northern Adriatic Sea coastal waters over a wide range of environmental conditions with a profiling system having a 6-Hz acquisition rate, ?0.1 m s?1 deployment speed, radiance sensors with 20° full angle field of view, and irradiance collectors of ?1-cm diameter. The uncertainties were quantified as a function of the depth resolution of radiance and irradiance profiles through the percent differences between the subsurface values computed from full and reduced resolution profiles (the latter synthetically created by removing data from the former). The applied method made the analysis independent from instrument calibration; from perturbations induced by instrument self-shading, deployment structure, and bottom effects; and from environmental variability caused by seawater and illumination changes during casts. The results displayed a significant increase in uncertainties with decreasing depth resolution. For instance, in the 443?665-nm spectral range with a depth resolution of 12.5 cm, the largest uncertainties were observed for the subsurface downward irradiance, Ed(0?, ?), and the near-surface diffuse attenuation coefficient, Kd(?), with spectral average uncertainties of 5.5% and 11.7%, respectively. With the same depth resolution, the smallest uncertainties were observed for the subsurface upwelling radiance, Lu(0?, ?), and upward irradiance, Eu(0?, ?), showing spectral average values of 1.0% and 0.6%, respectively. The uncertainties in the irradiance reflectance, R(?); the Q factor, Qn(?); and the normalized water-leaving radiance, LWN(?), gave values in keeping with those of the quantities used for their computation. The uncertainties were also analyzed as a function of sea state Ss and diffuse attenuation coefficient Kd at 490 nm. These values were used to estimate the depth resolution requirements restricting below given thresholds the wave-induced uncertainties in the computed subsurface optical quantities. To satisfy a 2% maximum uncertainty in the 443?665-nm spectral range, for the specific instrumental and environmental conditions characterizing the data used in the analysis, results suggested minimum depth resolutions of 11, 40, 3, and 2 cm, for Lu(0?, ?), Eu(0?, ?), Ed(0?, ?), and Kd(?), respectively.
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      An Evaluation of Depth Resolution Requirements for Optical Profiling in Coastal Waters

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4159868
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    • Journal of Atmospheric and Oceanic Technology

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    contributor authorZibordi, Giuseppe
    contributor authorD'Alimonte, Davide
    contributor authorBerthon, Jean-François
    date accessioned2017-06-09T14:38:18Z
    date available2017-06-09T14:38:18Z
    date copyright2004/07/01
    date issued2004
    identifier issn0739-0572
    identifier otherams-2332.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4159868
    description abstractWave perturbations induce uncertainties in subsurface quantities determined from the extrapolation of optical measurements taken at different depths. An analysis of these uncertainties was made using data collected in the northern Adriatic Sea coastal waters over a wide range of environmental conditions with a profiling system having a 6-Hz acquisition rate, ?0.1 m s?1 deployment speed, radiance sensors with 20° full angle field of view, and irradiance collectors of ?1-cm diameter. The uncertainties were quantified as a function of the depth resolution of radiance and irradiance profiles through the percent differences between the subsurface values computed from full and reduced resolution profiles (the latter synthetically created by removing data from the former). The applied method made the analysis independent from instrument calibration; from perturbations induced by instrument self-shading, deployment structure, and bottom effects; and from environmental variability caused by seawater and illumination changes during casts. The results displayed a significant increase in uncertainties with decreasing depth resolution. For instance, in the 443?665-nm spectral range with a depth resolution of 12.5 cm, the largest uncertainties were observed for the subsurface downward irradiance, Ed(0?, ?), and the near-surface diffuse attenuation coefficient, Kd(?), with spectral average uncertainties of 5.5% and 11.7%, respectively. With the same depth resolution, the smallest uncertainties were observed for the subsurface upwelling radiance, Lu(0?, ?), and upward irradiance, Eu(0?, ?), showing spectral average values of 1.0% and 0.6%, respectively. The uncertainties in the irradiance reflectance, R(?); the Q factor, Qn(?); and the normalized water-leaving radiance, LWN(?), gave values in keeping with those of the quantities used for their computation. The uncertainties were also analyzed as a function of sea state Ss and diffuse attenuation coefficient Kd at 490 nm. These values were used to estimate the depth resolution requirements restricting below given thresholds the wave-induced uncertainties in the computed subsurface optical quantities. To satisfy a 2% maximum uncertainty in the 443?665-nm spectral range, for the specific instrumental and environmental conditions characterizing the data used in the analysis, results suggested minimum depth resolutions of 11, 40, 3, and 2 cm, for Lu(0?, ?), Eu(0?, ?), Ed(0?, ?), and Kd(?), respectively.
    publisherAmerican Meteorological Society
    titleAn Evaluation of Depth Resolution Requirements for Optical Profiling in Coastal Waters
    typeJournal Paper
    journal volume21
    journal issue7
    journal titleJournal of Atmospheric and Oceanic Technology
    identifier doi10.1175/1520-0426(2004)021<1059:AEODRR>2.0.CO;2
    journal fristpage1059
    journal lastpage1073
    treeJournal of Atmospheric and Oceanic Technology:;2004:;volume( 021 ):;issue: 007
    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