Abstract. A dual thermistor radiosonde (DTR) comprising two
(aluminium-coated and black) sensors with different emissivities was
developed to correct the effects of solar radiation on temperature probes
based on in situ radiation measurements. Herein, the DTR performance is
characterised in terms of the uncertainty via a series of ground-based
facilities and an intercomparison radiosounding test. The DTR
characterisation procedure using laboratory facilities is as follows:
individually calibrate the temperature of the thermistors in a climate
chamber from −70 to 30 ∘C to evaluate the uncertainty of raw
temperature measurement before radiation correction; test the effect of
temperature on the resistance reading using radiosonde boards in the climate
chamber from −70 to 20 ∘C to identify a potential source of errors
owing to the boards, especially at cold temperatures; individually perform
radiation tests on thermistors at room temperature to investigate the degree of heating of aluminium-coated and black sensors (the average ratio = 1 : 2.4) and use the result for obtaining unit-specific radiation correction
formulas; and perform parameterisation of the radiation measurement and
correction formulas with five representative pairs of sensors in terms of
temperature, pressure, ventilation speed, and irradiance using an upper air
simulator. These results are combined and applied to the DTR sounding test
conducted in July 2021. Thereafter, the effective irradiance is measured
using the temperature difference between the aluminium-coated and black
sensors of the DTR. The measured irradiance is then used for the radiation
correction of the DTR aluminium-coated sensor. The radiation-corrected
temperature of the DTR is mostly consistent with that of a commercial
radiosonde (Vaisala, RS41) within the expanded uncertainty
(∼ 0.35 ∘C) of the DTR at the coverage factor k = 2. Furthermore, the
components contributing to the uncertainty of the radiation measurement and
correction are analysed. The DTR methodology can improve the accuracy of
temperature measurement in the upper air within the framework of the
traceability to the International System of Units.