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    In-Flight Calibration of the Nimbus-7 Earth Radiation Budget (ERB) Sensors. Part II: Short-Term Perturbations

    Source: Journal of Atmospheric and Oceanic Technology:;1995:;volume( 012 ):;issue: 006::page 1150
    Author:
    Kyle, H. Lee
    ,
    Hucek, Richard
    ,
    Ardanuy, Philip
    ,
    Penn, Lanning
    ,
    Groveman, Brian
    ,
    Hickey, John
    ,
    Maschoff, Robert
    DOI: 10.1175/1520-0426(1995)012<1150:IFCOTE>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: This paper describes the production calibration adjustment algorithms used to remove thermal perturbation and stray light noise signals from the Nimbus-7 earth radiation budget (ERB) measurements. Sunlight, both direct and scattered from the sensor baffles, contaminated the ERB measurements at satellite sunrise and sunset. The problem covered subsatellite solar zenith angles from 90° to 120° and reduced the usefulness of the longwave spectral radiation measurements. Scattered light corrections are made from 90° to 99° while orbit-by-orbit interpolation is used frown 99° to 121°. Tests indicate that in the mean the midpoint interpolation error is less than 1 W m?2 with a standard deviation of about 5 W m?2. Thermal perturbations on the total channel 12 (0.2?50 ?m) appeared to be always less than 0.3%. However, the Suprasil-W domes on the otherwise similar shortwave channels 13 and 14 in some way helped produce thermal perturbations of up to 6% or more in channel 13 (0.2?3.8 ?m and up to 3% or more in channel 14 (0.7?2.8 ?m). These perturbations arose from variations in external radiant heating during the day, night, sunrise, and sunset. In addition, the on/off cycles of the ERB and neighboring experiments produced day-to-day variations. The algorithms described here helped produce a stable 9-year-long measurement set. No thermal corrections were made in channel 12 and the obvious thermal perturbations in channels 13 and 14 were corrected. The absolute accuracy of the calibrated measurements is difficult to determine. The remaining uncertainty depends on the perturbing functions that were greater at high latitudes, near satellite sunrise and sunset, than in the Tropics. In June and July, the corrections for the daytime thermal perturbations near the North Pole may be too large by 3?5 W m?2. In general, the Nimbus-7 ERB products show good agreement with the follow-on Earth Radiation Budget Experiment (ERBE) products.
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      In-Flight Calibration of the Nimbus-7 Earth Radiation Budget (ERB) Sensors. Part II: Short-Term Perturbations

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4146145
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    • Journal of Atmospheric and Oceanic Technology

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    contributor authorKyle, H. Lee
    contributor authorHucek, Richard
    contributor authorArdanuy, Philip
    contributor authorPenn, Lanning
    contributor authorGroveman, Brian
    contributor authorHickey, John
    contributor authorMaschoff, Robert
    date accessioned2017-06-09T14:01:02Z
    date available2017-06-09T14:01:02Z
    date copyright1995/12/01
    date issued1995
    identifier issn0739-0572
    identifier otherams-1097.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4146145
    description abstractThis paper describes the production calibration adjustment algorithms used to remove thermal perturbation and stray light noise signals from the Nimbus-7 earth radiation budget (ERB) measurements. Sunlight, both direct and scattered from the sensor baffles, contaminated the ERB measurements at satellite sunrise and sunset. The problem covered subsatellite solar zenith angles from 90° to 120° and reduced the usefulness of the longwave spectral radiation measurements. Scattered light corrections are made from 90° to 99° while orbit-by-orbit interpolation is used frown 99° to 121°. Tests indicate that in the mean the midpoint interpolation error is less than 1 W m?2 with a standard deviation of about 5 W m?2. Thermal perturbations on the total channel 12 (0.2?50 ?m) appeared to be always less than 0.3%. However, the Suprasil-W domes on the otherwise similar shortwave channels 13 and 14 in some way helped produce thermal perturbations of up to 6% or more in channel 13 (0.2?3.8 ?m and up to 3% or more in channel 14 (0.7?2.8 ?m). These perturbations arose from variations in external radiant heating during the day, night, sunrise, and sunset. In addition, the on/off cycles of the ERB and neighboring experiments produced day-to-day variations. The algorithms described here helped produce a stable 9-year-long measurement set. No thermal corrections were made in channel 12 and the obvious thermal perturbations in channels 13 and 14 were corrected. The absolute accuracy of the calibrated measurements is difficult to determine. The remaining uncertainty depends on the perturbing functions that were greater at high latitudes, near satellite sunrise and sunset, than in the Tropics. In June and July, the corrections for the daytime thermal perturbations near the North Pole may be too large by 3?5 W m?2. In general, the Nimbus-7 ERB products show good agreement with the follow-on Earth Radiation Budget Experiment (ERBE) products.
    publisherAmerican Meteorological Society
    titleIn-Flight Calibration of the Nimbus-7 Earth Radiation Budget (ERB) Sensors. Part II: Short-Term Perturbations
    typeJournal Paper
    journal volume12
    journal issue6
    journal titleJournal of Atmospheric and Oceanic Technology
    identifier doi10.1175/1520-0426(1995)012<1150:IFCOTE>2.0.CO;2
    journal fristpage1150
    journal lastpage1162
    treeJournal of Atmospheric and Oceanic Technology:;1995:;volume( 012 ):;issue: 006
    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
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