the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Vertical profiles of raindrop size distribution parameters of summer rainfall in the eastern Tibetan Plateau: retrieval method and characteristics
Abstract. The eastern Tibetan Plateau has a high elevation, with a cold and dry atmospheric background. The features of the raindrop size distributions (DSD) in this region have notable differences from those in the plains. The general empirical relationships for retrieving parameters of precipitation from radar observations are not applicable in the eastern Tibetan Plateau. In this study, we developed a new method based on optimal estimation theory to retrieve the vertical profiles of N0 and Dm from a Ka-band zenith-pointing Doppler radar. Validation by a field campaign during the summer of 2024 indicate that the average bias in the log10(N0) and Dm derived from the PARSIVEL2 disdrometer and the retrieved values is 0.12 and -0.1 mm, demonstrating the effectiveness of the retrieved DSD parameters in this region. Based on the retrieved vertical profiles of DSD parameters, some unique characteristics are found. The heavy precipitation (the maximum value in the reflectivity profile exceeding 30 dBZ) exhibits a higher particle number concentration above 2 km and larger raindrop size in the bottom of the rainfall on average. The mean values of Dm above 2 km are approximately 0.5 mm, for heavy precipitation, the value increase as the raindrops fall, reaching a peak at around 0.5 km. Precipitation that occurs after the nighttime cooling usually has higher particle concentrations and smaller particle sizes. Based on the above research, empirical relationships for the quantitative precipitation estimates (QPE) and attenuation correction using Ka-band radar in the eastern Tibetan Plateau are established.
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Status: open (until 04 Nov 2025)
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RC1: 'Comment on egusphere-2025-2523', Kwo-Sen Kuo, 14 Aug 2025
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AC1: 'Reply on RC1', Pingyi Dong, 19 Aug 2025
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The comment was uploaded in the form of a supplement: https://egusphere.copernicus.org/preprints/2025/egusphere-2025-2523/egusphere-2025-2523-AC1-supplement.pdf
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RC2: 'Reply on AC1', Kwo-Sen Kuo, 05 Sep 2025
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My concerns have been satisfactorily addressed. I would accept the manuscript for publication.
However, I notice that the Preprint has not been updated. For example, Figure 5 still has blue on black.
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EMBED THE SNIPPET BELOW IN YOUR SITEEnable collaborative features and customize widget:Citation: https://doi.org/10.5194/egusphere-2025-2523-RC2 -
AC2: 'Reply on RC2', Pingyi Dong, 15 Sep 2025
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We sincerely appreciate the time and effort you devoted to reviewing our manuscript. At present, the figure has not been modified in the submitted version, as it is still under discussion, and the revised manuscript can not be uploaded as  supplement.  We will ensure that the figure is revised accordingly in the final version.Citation: https://doi.org/
10.5194/egusphere-2025-2523-AC2
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AC2: 'Reply on RC2', Pingyi Dong, 15 Sep 2025
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RC2: 'Reply on AC1', Kwo-Sen Kuo, 05 Sep 2025
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AC1: 'Reply on RC1', Pingyi Dong, 19 Aug 2025
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penney1007/Article_Vertical-profiles-of.: code Pingyi Dong https://doi.org/10.5281/zenodo.15827786
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The manuscript is of good scientific quality and is clearly and well written, except for some minor issues, which include, but are not limited to:
Please see the attached PDF for more comprehensive and detailed comments and suggestions.
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