Preprints
https://doi.org/10.5194/egusphere-2026-5816
https://doi.org/10.5194/egusphere-2026-5816
16 Oct 2026
 | 16 Oct 2026
Status: this preprint is open for discussion and under review for Atmospheric Measurement Techniques (AMT).

A Ka/W-band dual-frequency millimeter-wave radar–thermal infrared radiometer system for cloud and precipitation observations over the Tibetan Plateau: design, performance evaluation, and preliminary observations

Yongheng Bi, Yinan Wang, Rui Qi, Linjun Pan, Ming Li, Yufang Tian, Wei Zhao, Juan Huo, and Daren Lyu

Abstract. Continuous observations of cloud and precipitation structure are important for characterizing atmospheric processes over the Tibetan Plateau, where long-term measurements remain challenging to obtain. We present a Ka/W-band dualfrequency millimeter-wave radar–thermal infrared radiometer system (KaW-TIR), developed by the Institute of Atmospheric Physics, Chinese Academy of Sciences, and Sun Create Electronics Co., Ltd., and deployed at the Yangbajing Atmospheric Observatory in Tibet. The system integrates all-solid-state frequency-modulated continuous-wave (FMCW) radars, sharedaperture dual-frequency Cassegrain antennas, separate transmit and receive assemblies, and a thermal infrared channel on a common scanning platform. A common time reference supports synchronized observations with approximately aligned viewing directions. We evaluated system performance using internal monitoring, UAV-suspended metal-sphere calibration, weak cold-cloud consistency analysis, and long-term observation statistics. The metal-sphere calibration yielded mean apparent reflectivity biases of −0.75 dB for the Ka band and +0.32 dB for the W band, which were used to correct the corresponding radar constants. Selected weak cold-cloud samples had a median Ka–W dual-wavelength ratio of 0.34 dB. In the routine observing mode, the nominal range resolution is 30 m, and the product update interval is approximately 0.92 s. At 10 km above radar level, the observed statistical detection boundaries are approximately −44.43 dBZ for the Ka band and −43.20 dBZ for the W band. A representative case illustrates concurrent radar-observed cloud and precipitation structure and thermal infrared brightness temperature. These results demonstrate the KaW-TIR system's capability for continuous, synchronous observations of cloud and precipitation at a high-altitude site on the Tibetan Plateau.

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Yongheng Bi, Yinan Wang, Rui Qi, Linjun Pan, Ming Li, Yufang Tian, Wei Zhao, Juan Huo, and Daren Lyu

Status: open (until 21 Nov 2026)

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Yongheng Bi, Yinan Wang, Rui Qi, Linjun Pan, Ming Li, Yufang Tian, Wei Zhao, Juan Huo, and Daren Lyu
Yongheng Bi, Yinan Wang, Rui Qi, Linjun Pan, Ming Li, Yufang Tian, Wei Zhao, Juan Huo, and Daren Lyu
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Latest update: 16 Oct 2026
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Short summary
Clouds over the Tibetan Plateau are difficult to observe continuously, yet they strongly influence weather, water, and climate. We developed and tested a ground-based system combining two cloud radars with a thermal infrared radiometer. Long-term observations show reliable operation and high sensitivity to weak clouds, while synchronized measurements provide complementary views of cloud structure and thermal emission. The system supports studies of clouds and precipitation over the plateau.
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