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• W4280526263 endingPage "106248" @default.
• W4280526263 startingPage "106248" @default.
• W4280526263 abstract "The nation-wide feature of raindrop size distribution (hereafter referred to as DSD) remains largely unknown across China. We here analyzed the DSD using high-resolution disdrometer measurements collected throughout China during the warm season (May through August) of 2020. Overall, pronounced unimodal structures were found for the monthly mean DSD, while little differences were revealed in the monthly variation of DSD. Spatially, the regions with a high value of mass-weighted mean diameter Dm generally witnessed a low value of intercept parameter Nw. The DSD parameters were further investigated by six regions of interest: Northeast China Plain (ECP), North China Plain (NCP), Yangtze River Delta (YRD), Pearl River Delta (PRD), Sichuan Basin (SCB), and Qinghai-Tibet Plateau (QTP). Specially, Dm (log10Nw) over ECP, NCP, YRD, PRD and SCB was found to have a larger (smaller) value than the surrounding areas, whereas the Dm (log10Nw) in the QTP had a smaller (larger) value. Furthermore, explicit analyses were performed in attempt to better understand the influential factors accounting for the regional disparity of DSD by two categories: stratiform and convective precipitation. Dm, log10Nw, spectral width and peak concentration all showed larger values in the convective precipitation than those in the stratiform precipitation. Interestingly, the Dm-log10Nw pairs for convective precipitation resembled roughly the “maritime” cluster, indicating a maritime nature of convective precipitation throughout the warm season in China. The PRD had the largest Dm and the smallest log10Nw, while the QTP had the smallest Dm and the largest log10Nw in the stratiform precipitation. In addition, several widely used empirical equations of Z-R relations tended to underestimate R compared with our actual fitting. The impacts of environmental variables were further studied, including convection available potential energy (CAPE), surface temperature, wind shear and vertically integrated moisture flux divergence (MFD). The dependence of DSD on environmental variable was revealed to varying degrees. It is noteworthy that larger CAPE but lower MFD was found to be accompanied with heavy rain produced by convective precipitation than by stratiform precipitation. The invaluable DSD dataset hereby will lay a solid foundation for potentially improved quantitative precipitation estimation from weather radar in the future in China." @default.
• W4280526263 created "2022-05-22" @default.
• W4280526263 creator A5007568345 @default.
• W4280526263 creator A5051167681 @default.
• W4280526263 creator A5052883326 @default.
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• W4280526263 creator A5065442126 @default.
• W4280526263 creator A5068048071 @default.
• W4280526263 creator A5072279396 @default.
• W4280526263 creator A5080280687 @default.
• W4280526263 date "2022-09-01" @default.
• W4280526263 modified "2023-09-24" @default.
• W4280526263 title "Investigation of raindrop size distribution and its potential influential factors during warm season over China" @default.
• W4280526263 cites W1532223261 @default.
• W4280526263 cites W1661303466 @default.
• W4280526263 cites W1794098459 @default.
• W4280526263 cites W1949065959 @default.
• W4280526263 cites W1964801436 @default.
• W4280526263 cites W1973744481 @default.
• W4280526263 cites W1974167811 @default.
• W4280526263 cites W1977070284 @default.
• W4280526263 cites W1980267524 @default.
• W4280526263 cites W1992955350 @default.
• W4280526263 cites W1993617157 @default.
• W4280526263 cites W1996367659 @default.
• W4280526263 cites W2000257837 @default.
• W4280526263 cites W2001063609 @default.
• W4280526263 cites W2002712953 @default.
• W4280526263 cites W2005469587 @default.
• W4280526263 cites W2018566469 @default.
• W4280526263 cites W2018633042 @default.
• W4280526263 cites W2018898343 @default.
• W4280526263 cites W2020975129 @default.
• W4280526263 cites W2030293362 @default.
• W4280526263 cites W2031675844 @default.
• W4280526263 cites W2034803461 @default.
• W4280526263 cites W2034956393 @default.
• W4280526263 cites W2040037974 @default.
• W4280526263 cites W2051249177 @default.
• W4280526263 cites W2052926657 @default.
• W4280526263 cites W2055218499 @default.
• W4280526263 cites W2073247318 @default.
• W4280526263 cites W2076057452 @default.
• W4280526263 cites W2081654416 @default.
• W4280526263 cites W2086021208 @default.
• W4280526263 cites W2088041715 @default.
• W4280526263 cites W2094764088 @default.
• W4280526263 cites W2097055177 @default.
• W4280526263 cites W2121849293 @default.
• W4280526263 cites W2142140026 @default.
• W4280526263 cites W2144022504 @default.
• W4280526263 cites W2147205509 @default.
• W4280526263 cites W2152068641 @default.
• W4280526263 cites W2153839935 @default.
• W4280526263 cites W2155586300 @default.
• W4280526263 cites W2171905601 @default.
• W4280526263 cites W2173031829 @default.
• W4280526263 cites W2174157742 @default.
• W4280526263 cites W2177746725 @default.
• W4280526263 cites W2178415932 @default.
• W4280526263 cites W2253691383 @default.
• W4280526263 cites W2274487689 @default.
• W4280526263 cites W2313040768 @default.
• W4280526263 cites W2319636845 @default.
• W4280526263 cites W2500077203 @default.
• W4280526263 cites W2531306006 @default.
• W4280526263 cites W2610090103 @default.
• W4280526263 cites W2617654664 @default.
• W4280526263 cites W2763577999 @default.
• W4280526263 cites W2766944531 @default.
• W4280526263 cites W2797513361 @default.
• W4280526263 cites W2801611053 @default.
• W4280526263 cites W2803028566 @default.
• W4280526263 cites W2804468468 @default.
• W4280526263 cites W2805754236 @default.
• W4280526263 cites W2896599334 @default.
• W4280526263 cites W2898198235 @default.
• W4280526263 cites W2904755549 @default.
• W4280526263 cites W2906353386 @default.
• W4280526263 cites W2908620319 @default.
• W4280526263 cites W2911535408 @default.
• W4280526263 cites W2913904793 @default.
• W4280526263 cites W2917300546 @default.
• W4280526263 cites W2921221695 @default.
• W4280526263 cites W2926090895 @default.
• W4280526263 cites W2947226607 @default.
• W4280526263 cites W2951808367 @default.
• W4280526263 cites W2985293211 @default.
• W4280526263 cites W2997941124 @default.
• W4280526263 cites W3000098254 @default.
• W4280526263 cites W3002988727 @default.
• W4280526263 cites W3012910817 @default.
• W4280526263 cites W3025949386 @default.
• W4280526263 cites W3034407757 @default.
• W4280526263 cites W3081825248 @default.
• W4280526263 cites W3082840893 @default.
• W4280526263 cites W3083608462 @default.
• W4280526263 cites W3093250210 @default.

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