Abstract

Abstract. Simultaneous observations of rainfall collected by a tipping bucket rain gauge (TBRG), a weighing rain gauge (WRG), an optical rain gauge (ORG), a present weather detector (PWD), a Joss–Waldvogel disdrometer (JWD), and a 2-D video disdrometer (2DVD) during January to October 2012 were analyzed to evaluate how accurately they measure rainfall and drop size distributions (DSDs). For the long-term observations, there were different discrepancies in rain amounts from six instruments on the order of 0% to 27.7%. The TBRG, WRG, and ORG have a good agreement, while the PWD and 2DVD record higher and the JWD lower rain rates when R > 20 mm h−1, the ORG agrees well with JWD and 2DVD, while the TBRG records higher and the WRG lower rain rates when R > 20 mm h−1. Compared with the TBRG and WRG, optical and impact instruments can measure the rain rate accurately in the light rain. The overall DSDs of JWD and 2DVD agree well with each other, except for the small raindrops (D < 1 mm). JWD can measure more moderate-size raindrops (0.3 mm < D < 1.5 mm) than 2DVD, but 2DVD can measure more small-size raindrops (D < 0.3 mm). 2DVD has a larger measurement range; more overall raindrops can be measured by 2DVD than by JWD in different rain rate regimes. But small raindrops might be underestimated by 2DVD when R > 15 mm h−1. The small raindrops tend to be omitted in the more large-size raindrops due to the shadow effect of light. Therefore, the measurement accuracy of small raindrops in the heavy rainfall from 2DVD should be handled carefully.

Highlights

  • Amounts from six instruments on the order of 0 % to 27.7 %. been widely used in the cloud modeling and climate stud

  • It can be found that the tipping bucket rain gauge (TBRG), weighing rain gauge (WRG), and optical rain gauge (ORG) have a good agreement when rain rate is more than 20 mm h−1, whereas Joss–Waldvogel disdrometer (JWD) records lower rain rate, while present weather detector (PWD) and 2DVD record higher rain rates

  • In order to evaluate the accuracy of rainfall measurements from different instruments based on different principles, we analyzed the rainfall observations from a tipping bucket rain gauge, a weighing bucket rain gauge, an optical rain gauge, a present weather detector, a Joss–Waldvogel disdrometer, and a 2-D video disdrometer

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Summary

Rain gauge

The tipping bucket rain gauge (TBRG for short) is a siphoncontrolled tipping bucket rain gauge (RIMCO 7499 series). The accuracy of the rain rate is related to the precision of the water accumulation measurement, the rate at which rainwater drains from the catchment basin into the measurement chamber, and the sampling interval (Nystuen, 1999). Rainfall measurement is invalid during the collecting pan drains when the collecting pan fills with water. Both the TBRG and WRG are equipped with an optional heater, whereas the TBRG and WRG were not heated because the environment temperature was higher than 20 ◦C in this study. The optical rain gauge (ORG for short) measures the scintillation of infrared light produced by the liquid water drops falling between a light source and a receiver (Nystuen et al, 1996). Compared with the other gauges, the ORG overestimates rain rate when there are more small-size drops, and underestimates rain rate when there are more large-size drops, while it might be biased high during higher winds (Nystuen, 1999)

Present weather detector
Joss–Waldvogel disdrometer
General analysis
Event analysis
JWD 2DVD
Conclusions
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