Spatial and temporal variation of raindrop size distribution in Great Britain

Raindrop size distributions (DSDs) play a key role in revealing the underlying physical processes of rainfall. This study investigates the characteristics of the DSDs in Great Britain (GB) using data collected from eleven Thies laser precipitation monitors (LPMs) between 2017 and 2019. Around one million one-minute raindrop samples were fitted to a normalized gamma drop distribution model. This study examines the DSD characteristics from both temporal (seasons) and spatial (geography and topography) perspectives, considering different rain types(stratiform and convective) and rain rate clusters. The results indicate that the average mass-weighted mean diameter〈<i>D<sub>m</sub></i>〉 and the average normalized intercept parameter log<sub>10</sub>〈<i>N<sub>w</sub></i>〉 are influenced by geographical and atmospheric conditions. The 〈<i>D<sub>m</sub></i>〉 tends to be lower and log<sub>10</sub>〈<i>N<sub>w</sub></i>〉 is higher in the western and hilly regions, with the opposite pattern observed over the eastern plain of GB. Both parameters are strongly correlated with rain rate. Compared to subtropical/tropical regions, stratiform rain in GB exhibits smaller 〈<i>D<sub>m</sub></i>〉 and larger log<sub>10</sub>〈<i>N<sub>w</sub></i>〉,while the characteristics of convective rain align with the maritime-like cluster. Significant differences in 〈<i>D<sub>m</sub></i>〉are observed between stratiform (0.78–1.00 mm) and convective (1.30–1.74 mm) rain, with both showing a significant negative linear correlation with log10〈<i>N<sub>w</sub></i>〉. Moreover, extreme convective events show distinct seasonality, with larger <i>D<sub>m</sub></i> and lower log<sub>10</sub>(<i>N<sub>w</sub></i>) during the warm season. Furthermore, a bimodal distribution is observed for log<sub>10</sub>(<i>N<sub>w</sub></i>) in light rain events over western and hilly regions, highlighting the complexity of microphysical processes associated with small raindrops. The characteristics of DSDs observed in this study provide valuable insights for future investigations into GB’s precipitation formation and quantitative precipitation estimation using weather radar.

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Publication Details

Journal
Atmospheric Research
Published
2025-12-11
DOI
https://doi.org/10.1016/j.atmosres.2025.108699
Primary Topic
Precipitation Measurement and Analysis
Type
article
Field-Weighted Citation Impact
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article

Spatial and temporal variation of raindrop size distribution in Great Britain

Merhala Thurai, Shan Jiang, Miguel A. Rico‐Ramirez, Rafael Rosolem et al.
Atmospheric Research
Precipitation Measurement and Analysis
article

Spatial and temporal variation of raindrop size distribution in Great Britain

Merhala Thurai, Shan Jiang, Miguel A. Rico‐Ramirez, Rafael Rosolem, Dawei Han
article en

Abstract

Raindrop size distributions (DSDs) play a key role in revealing the underlying physical processes of rainfall. This study investigates the characteristics of the DSDs in Great Britain (GB) using data collected from eleven Thies laser precipitation monitors (LPMs) between 2017 and 2019. Around one million one-minute raindrop samples were fitted to a normalized gamma drop distribution model. This study examines the DSD characteristics from both temporal (seasons) and spatial (geography and topography) perspectives, considering different rain types(stratiform and convective) and rain rate clusters. The results indicate that the average mass-weighted mean diameter〈<i>D<sub>m</sub></i>〉 and the average normalized intercept parameter log<sub>10</sub>〈<i>N<sub>w</sub></i>〉 are influenced by geographical and atmospheric conditions. The 〈<i>D<sub>m</sub></i>〉 tends to be lower and log<sub>10</sub>〈<i>N<sub>w</sub></i>〉 is higher in the western and hilly regions, with the opposite pattern observed over the eastern plain of GB. Both parameters are strongly correlated with rain rate. Compared to subtropical/tropical regions, stratiform rain in GB exhibits smaller 〈<i>D<sub>m</sub></i>〉 and larger log<sub>10</sub>〈<i>N<sub>w</sub></i>〉,while the characteristics of convective rain align with the maritime-like cluster. Significant differences in 〈<i>D<sub>m</sub></i>〉are observed between stratiform (0.78–1.00 mm) and convective (1.30–1.74 mm) rain, with both showing a significant negative linear correlation with log10〈<i>N<sub>w</sub></i>〉. Moreover, extreme convective events show distinct seasonality, with larger <i>D<sub>m</sub></i> and lower log<sub>10</sub>(<i>N<sub>w</sub></i>) during the warm season. Furthermore, a bimodal distribution is observed for log<sub>10</sub>(<i>N<sub>w</sub></i>) in light rain events over western and hilly regions, highlighting the complexity of microphysical processes associated with small raindrops. The characteristics of DSDs observed in this study provide valuable insights for future investigations into GB’s precipitation formation and quantitative precipitation estimation using weather radar.

Atmospheric ResearchVol. 331
Openalex Percentile: Top 56%
Precipitation Measurement and Analysis
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