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    Characterization and Correction of Relative Humidity Measurements from Vaisala RS80-A Radiosondes at Cold Temperatures

    Source: Journal of Atmospheric and Oceanic Technology:;2001:;volume( 018 ):;issue: 002::page 135
    Author:
    Miloshevich, Larry M.
    ,
    Vömel, Holger
    ,
    Paukkunen, Ari
    ,
    Heymsfield, Andrew J.
    ,
    Oltmans, Samuel J.
    DOI: 10.1175/1520-0426(2001)018<0135:CACORH>2.0.CO;2
    Publisher: American Meteorological Society
    Abstract: Radiosonde relative humidity (RH) measurements are known to be unreliable at cold temperatures. This study characterizes radiosonde RH measurements from Vaisala RS80-A thin-film capacitive sensors in the temperature range 0° to ?70°C. Sources of measurement error are identified, and two approaches for correcting the errors are presented. The corrections given in this paper apply only to the Vaisala RS80-A sensor, although the RS80-H sensor is briefly discussed for comparison. A temperature-dependent correction factor is derived from statistical analysis of simultaneous RH measurements from RS80-A radiosondes and the NOAA cryogenic frostpoint hygrometer. The mean RS80-A measurement error is shown to be a dry bias that increases with decreasing temperature, and the multiplicative correction factor is about 1.3 at ?35°C, 1.6 at ?50°C, 2.0 at ?60°C, and 2.4 at ?70°C. The fractional uncertainty in the mean of corrected measurements, when large datasets are considered statistically, increases from 0.06 at 0°C to 0.11 at ?70°C. The fractional uncertainty for correcting an individual sounding is about ±0.2, which is larger because this statistical approach considers only the mean value of measurement errors that are not purely temperature dependent. The correction must not be used outside the temperature range 0° to ?70°C, because it is a meaningless extrapolation of a polynomial curve fit. Laboratory measurements of sensor response conducted at Vaisala are used to characterize some of the individual sources of RS80-A measurement error. A correction factor is derived for the dominant RS80-A measurement error at cold temperatures: an inaccurate approximation for the sensor?s temperature dependence in the data processing algorithm. The correction factor for temperature-dependence error is about 1.1 at ?35°C, 1.4 at ?50°C, 1.8 at ?60°C, and 2.5 at ?70°C. Dependences and typical magnitudes are given for measurement errors that result from the temperature dependence of the sensor?s time constant, and from several smaller bias errors and random uncertainties.
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      Characterization and Correction of Relative Humidity Measurements from Vaisala RS80-A Radiosondes at Cold Temperatures

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    contributor authorMiloshevich, Larry M.
    contributor authorVömel, Holger
    contributor authorPaukkunen, Ari
    contributor authorHeymsfield, Andrew J.
    contributor authorOltmans, Samuel J.
    date accessioned2017-06-09T14:21:57Z
    date available2017-06-09T14:21:57Z
    date copyright2001/02/01
    date issued2001
    identifier issn0739-0572
    identifier otherams-1804.pdf
    identifier urihttp://onlinelibrary.yabesh.ir/handle/yetl/4154001
    description abstractRadiosonde relative humidity (RH) measurements are known to be unreliable at cold temperatures. This study characterizes radiosonde RH measurements from Vaisala RS80-A thin-film capacitive sensors in the temperature range 0° to ?70°C. Sources of measurement error are identified, and two approaches for correcting the errors are presented. The corrections given in this paper apply only to the Vaisala RS80-A sensor, although the RS80-H sensor is briefly discussed for comparison. A temperature-dependent correction factor is derived from statistical analysis of simultaneous RH measurements from RS80-A radiosondes and the NOAA cryogenic frostpoint hygrometer. The mean RS80-A measurement error is shown to be a dry bias that increases with decreasing temperature, and the multiplicative correction factor is about 1.3 at ?35°C, 1.6 at ?50°C, 2.0 at ?60°C, and 2.4 at ?70°C. The fractional uncertainty in the mean of corrected measurements, when large datasets are considered statistically, increases from 0.06 at 0°C to 0.11 at ?70°C. The fractional uncertainty for correcting an individual sounding is about ±0.2, which is larger because this statistical approach considers only the mean value of measurement errors that are not purely temperature dependent. The correction must not be used outside the temperature range 0° to ?70°C, because it is a meaningless extrapolation of a polynomial curve fit. Laboratory measurements of sensor response conducted at Vaisala are used to characterize some of the individual sources of RS80-A measurement error. A correction factor is derived for the dominant RS80-A measurement error at cold temperatures: an inaccurate approximation for the sensor?s temperature dependence in the data processing algorithm. The correction factor for temperature-dependence error is about 1.1 at ?35°C, 1.4 at ?50°C, 1.8 at ?60°C, and 2.5 at ?70°C. Dependences and typical magnitudes are given for measurement errors that result from the temperature dependence of the sensor?s time constant, and from several smaller bias errors and random uncertainties.
    publisherAmerican Meteorological Society
    titleCharacterization and Correction of Relative Humidity Measurements from Vaisala RS80-A Radiosondes at Cold Temperatures
    typeJournal Paper
    journal volume18
    journal issue2
    journal titleJournal of Atmospheric and Oceanic Technology
    identifier doi10.1175/1520-0426(2001)018<0135:CACORH>2.0.CO;2
    journal fristpage135
    journal lastpage156
    treeJournal of Atmospheric and Oceanic Technology:;2001:;volume( 018 ):;issue: 002
    contenttypeFulltext
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