Comparison of summer raindrop size distribution characteristics in the western and central Tianshan Mountains of China

Abstract The microphysical processes of cloud and precipitation in the Tianshan Mountains still remain unclear due to the complex terrain and the lack of ground‐based observational data. In this study, the characteristics of summer raindrop size distribution (RSD) in the western and central Tianshan...

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Main Authors: Yufei Jiang, Lianmei Yang, Yong Zeng, Zepeng Tong, Jiangang Li, Fan Liu, Jinru Zhang, Jin Liu
Format: Article
Language:English
Published: Wiley 2022-05-01
Series:Meteorological Applications
Subjects:
Online Access:https://doi.org/10.1002/met.2067
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author Yufei Jiang
Lianmei Yang
Yong Zeng
Zepeng Tong
Jiangang Li
Fan Liu
Jinru Zhang
Jin Liu
author_facet Yufei Jiang
Lianmei Yang
Yong Zeng
Zepeng Tong
Jiangang Li
Fan Liu
Jinru Zhang
Jin Liu
author_sort Yufei Jiang
collection DOAJ
description Abstract The microphysical processes of cloud and precipitation in the Tianshan Mountains still remain unclear due to the complex terrain and the lack of ground‐based observational data. In this study, the characteristics of summer raindrop size distribution (RSD) in the western and central Tianshan Mountains of China were investigated in 2020 and 2021. According to the average raindrop spectra, the RSD characteristics exhibit significant differences that the concentration of medium and large particles is relatively higher at Zhaosu than that at Tianchi. Weak precipitation prevails in the Tianshan Mountains most of the time, yet moderate rainfall and heavy rainfall have a great impact on the accumulated rainfall amount. For each rainfall rate class, raindrops of diameter less than 0.75mm have a lower concentration and raindrops of diameter greater than 3 mm have a higher concentration at Zhaosu as compared to those at Tianchi. Compared with Tianchi, Zhaosu has a larger mass‐weighted mean diameter (Dm) and a lower normalized intercept parameter (log10Nw). Compared with the classical convective spectrum, the RSDs at both Zhaosu and Tianchi are similar to the continental convective cluster. The relationships between the shape and slope (μ–Λ), and radar reflectivity and rainfall rate (Z–R) exhibit a significant difference in the western and central Tianshan Mountains of China.
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spelling doaj.art-50d3fb99247b4365b1f9476fc7c32c322022-12-22T03:32:48ZengWileyMeteorological Applications1350-48271469-80802022-05-01293n/an/a10.1002/met.2067Comparison of summer raindrop size distribution characteristics in the western and central Tianshan Mountains of ChinaYufei Jiang0Lianmei Yang1Yong Zeng2Zepeng Tong3Jiangang Li4Fan Liu5Jinru Zhang6Jin Liu7Institute of Desert Meteorology China Meteorological Administration Urumqi ChinaInstitute of Desert Meteorology China Meteorological Administration Urumqi ChinaInstitute of Desert Meteorology China Meteorological Administration Urumqi ChinaInstitute of Desert Meteorology China Meteorological Administration Urumqi ChinaInstitute of Desert Meteorology China Meteorological Administration Urumqi ChinaInstitute of Desert Meteorology China Meteorological Administration Urumqi ChinaInstitute of Desert Meteorology China Meteorological Administration Urumqi ChinaInstitute of Desert Meteorology China Meteorological Administration Urumqi ChinaAbstract The microphysical processes of cloud and precipitation in the Tianshan Mountains still remain unclear due to the complex terrain and the lack of ground‐based observational data. In this study, the characteristics of summer raindrop size distribution (RSD) in the western and central Tianshan Mountains of China were investigated in 2020 and 2021. According to the average raindrop spectra, the RSD characteristics exhibit significant differences that the concentration of medium and large particles is relatively higher at Zhaosu than that at Tianchi. Weak precipitation prevails in the Tianshan Mountains most of the time, yet moderate rainfall and heavy rainfall have a great impact on the accumulated rainfall amount. For each rainfall rate class, raindrops of diameter less than 0.75mm have a lower concentration and raindrops of diameter greater than 3 mm have a higher concentration at Zhaosu as compared to those at Tianchi. Compared with Tianchi, Zhaosu has a larger mass‐weighted mean diameter (Dm) and a lower normalized intercept parameter (log10Nw). Compared with the classical convective spectrum, the RSDs at both Zhaosu and Tianchi are similar to the continental convective cluster. The relationships between the shape and slope (μ–Λ), and radar reflectivity and rainfall rate (Z–R) exhibit a significant difference in the western and central Tianshan Mountains of China.https://doi.org/10.1002/met.2067microphysical characteristicsraindrop size distributionrainfall rateTianshan Mountains
spellingShingle Yufei Jiang
Lianmei Yang
Yong Zeng
Zepeng Tong
Jiangang Li
Fan Liu
Jinru Zhang
Jin Liu
Comparison of summer raindrop size distribution characteristics in the western and central Tianshan Mountains of China
Meteorological Applications
microphysical characteristics
raindrop size distribution
rainfall rate
Tianshan Mountains
title Comparison of summer raindrop size distribution characteristics in the western and central Tianshan Mountains of China
title_full Comparison of summer raindrop size distribution characteristics in the western and central Tianshan Mountains of China
title_fullStr Comparison of summer raindrop size distribution characteristics in the western and central Tianshan Mountains of China
title_full_unstemmed Comparison of summer raindrop size distribution characteristics in the western and central Tianshan Mountains of China
title_short Comparison of summer raindrop size distribution characteristics in the western and central Tianshan Mountains of China
title_sort comparison of summer raindrop size distribution characteristics in the western and central tianshan mountains of china
topic microphysical characteristics
raindrop size distribution
rainfall rate
Tianshan Mountains
url https://doi.org/10.1002/met.2067
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