2001Journal of Atmospheric and Oceanic TechnologyOpen access

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

Larry M. Miloshevich, Holger Vömel, A. Paukkunen, Andrew J. Heymsfield, S. J. Oltmans

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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 0Њ to Ϫ70ЊC.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 Ϫ35ЊC, 1.6 at Ϫ50ЊC, 2.0 at Ϫ60ЊC, and 2.4 at Ϫ70ЊC.The fractional uncertainty in the mean of corrected measurements, when large datasets are considered statistically, increases from 0.06 at 0ЊC to 0.11 at Ϫ70ЊC.The fractional uncertainty for correcting an individual sounding is about Ϯ0.2, 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 0Њ to Ϫ70ЊC, 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 Ϫ35ЊC, 1.4 at Ϫ50ЊC, 1.8 at Ϫ60ЊC, and 2.5 at Ϫ70ЊC.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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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 0Њ to Ϫ70ЊC.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 Ϫ35ЊC, 1.6 at Ϫ50ЊC, 2.0 at Ϫ60ЊC, and 2.4 at Ϫ70ЊC.The fractional uncertainty in the mean of corrected measurements, when large datasets are considered statistically, increases from 0.06 at 0ЊC to 0.11 at Ϫ70ЊC.The fractional uncertainty for correcting an individual sounding is about Ϯ0.2, 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 0Њ to Ϫ70ЊC, 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 Ϫ35ЊC, 1.4 at Ϫ50ЊC, 1.8 at Ϫ60ЊC, and 2.5 at Ϫ70ЊC.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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Available 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 0Њ to Ϫ70ЊC.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 Ϫ35ЊC, 1.6 at Ϫ50ЊC, 2.0 at Ϫ60ЊC, and 2.4 at Ϫ70ЊC.The fractional uncertainty in the mean of corrected measurements, when large datasets are considered statistically, increases from 0.06 at 0ЊC to 0.11 at Ϫ70ЊC.The fractional uncertainty for correcting an individual sounding is about Ϯ0.2, 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 0Њ to Ϫ70ЊC, 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 Ϫ35ЊC, 1.4 at Ϫ50ЊC, 1.8 at Ϫ60ЊC, and 2.5 at Ϫ70ЊC.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.

Key concepts: Radiosonde, Hygrometer, Extrapolation, Relative humidity, Environmental science, Observational error, Meteorology, Range (aeronautics)

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