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    On Irradiance Measurement Errors at Sea Due to Tilt of Pyranometers

    Source: Journal of Atmospheric and Oceanic Technology:;1986:;volume( 003 ):;issue: 004::page 740
    Author:
    Katsaros, Kristina B.
    ,
    Devault, John E.
    DOI: 10.1175/1520-0426(1986)003<0740:OIMEAS>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Calculations are made of errors in the measurement of solar irradiance at the sea surface. which occur when pyranometers are tilled. Tilts due to buoy or ship motion caused by wave action or a preferential tilt due to drag are considered. Errors depend on sky condition and are maximum for clear skies. They depend on soar zenith angle and on the relative azimuth of sun and tilt directions, and vary, therefore, with latitude and season or time of day. Errors as large as ±10% to ±20% in the daily average (with sign dependent on azimuth of the tilt) could be encountered for clear skies poleward of 45°N or S in the winter half of the year for a 10° preferential tilt. Instantaneous errors due to wave action can be as large. Because of the difficulty of making corrections a posteriori, gimbal mounting of pyranometers is recommended.
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      On Irradiance Measurement Errors at Sea Due to Tilt of Pyranometers

    URI
    http://yetl.yabesh.ir/yetl1/handle/yetl/4162067
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    contributor authorKatsaros, Kristina B.
    contributor authorDevault, John E.
    date accessioned2017-06-09T14:43:33Z
    date available2017-06-09T14:43:33Z
    date copyright1986/12/01
    date issued1986
    identifier issn0739-0572
    identifier otherams-253.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4162067
    description abstractCalculations are made of errors in the measurement of solar irradiance at the sea surface. which occur when pyranometers are tilled. Tilts due to buoy or ship motion caused by wave action or a preferential tilt due to drag are considered. Errors depend on sky condition and are maximum for clear skies. They depend on soar zenith angle and on the relative azimuth of sun and tilt directions, and vary, therefore, with latitude and season or time of day. Errors as large as ±10% to ±20% in the daily average (with sign dependent on azimuth of the tilt) could be encountered for clear skies poleward of 45°N or S in the winter half of the year for a 10° preferential tilt. Instantaneous errors due to wave action can be as large. Because of the difficulty of making corrections a posteriori, gimbal mounting of pyranometers is recommended.
    publisherAmerican Meteorological Society
    titleOn Irradiance Measurement Errors at Sea Due to Tilt of Pyranometers
    typeJournal Paper
    journal volume3
    journal issue4
    journal titleJournal of Atmospheric and Oceanic Technology
    identifier doi10.1175/1520-0426(1986)003<0740:OIMEAS>2.0.CO;2
    journal fristpage740
    journal lastpage745
    treeJournal of Atmospheric and Oceanic Technology:;1986:;volume( 003 ):;issue: 004
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
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