{"title":"An Investigation on Microphysical Characteristics of Early-, Late-, and Post-Mei-yu Season Rainfall Over Taiwan","authors":"Balaji Kumar Seela, Jayalakshmi Janapati, Pay-Liam Lin, Chian-Yi Liu, Chuan-Chi Tu","doi":"10.1029/2024JD040847","DOIUrl":null,"url":null,"abstract":"<p>Over Taiwan, Mei-yu season (May and June), which is primarily linked to frontal systems, is the transition period between winter and summer. Using the Global Precipitation Measurement Mission dual-frequency precipitation radar (GPM DPR), the current study examined the rain and microphysical characteristics of the Mei-yu season in Taiwan. In order to examine the areal and intra-seasonal aspects, May and June months are divided into three sub-seasons: early-Mei-yu, late-Mei-yu, and post-Mei-yu. The three sub-seasons exhibited differences in rainfall and raindrop size distributions, with abundance of large drops in the post-Mei-yu. Additionally, there were noticeable variations in the raindrop size distributions among the south, central, north, and eastern parts of Taiwan, with more large drops in central Taiwan. To comprehend the microphysical progressions causing the regional and intra-seasonal fluctuations, CFADs (contoured frequency by altitude diagrams) of rain parameters are utilized. Compared to other two sub-seasons, the early-Mei-yu season exhibited weaker convection. Dominance of stratiform precipitation in late-Mei-yu season, and convective precipitation in post-Mei-yu season resulted in higher rainfall amounts in these two sub-seasons (more particularly in post-Mei-yu) than the early-Mei-yu season. Examination of warm rain microphysical processes (below 5 km height) among these sub-seasons revealed that the early-Mei-yu season is dominated with break-up process, late-Mei-yu season with breakup and coalescence balance, and post-Mei-yu with coalescence, size-sorting and evaporation processes.</p>","PeriodicalId":15986,"journal":{"name":"Journal of Geophysical Research: Atmospheres","volume":null,"pages":null},"PeriodicalIF":3.8000,"publicationDate":"2024-09-25","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"https://onlinelibrary.wiley.com/doi/epdf/10.1029/2024JD040847","citationCount":"0","resultStr":null,"platform":"Semanticscholar","paperid":null,"PeriodicalName":"Journal of Geophysical Research: Atmospheres","FirstCategoryId":"89","ListUrlMain":"https://onlinelibrary.wiley.com/doi/10.1029/2024JD040847","RegionNum":2,"RegionCategory":"地球科学","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":null,"EPubDate":"","PubModel":"","JCR":"Q2","JCRName":"METEOROLOGY & ATMOSPHERIC SCIENCES","Score":null,"Total":0}
引用次数: 0
Abstract
Over Taiwan, Mei-yu season (May and June), which is primarily linked to frontal systems, is the transition period between winter and summer. Using the Global Precipitation Measurement Mission dual-frequency precipitation radar (GPM DPR), the current study examined the rain and microphysical characteristics of the Mei-yu season in Taiwan. In order to examine the areal and intra-seasonal aspects, May and June months are divided into three sub-seasons: early-Mei-yu, late-Mei-yu, and post-Mei-yu. The three sub-seasons exhibited differences in rainfall and raindrop size distributions, with abundance of large drops in the post-Mei-yu. Additionally, there were noticeable variations in the raindrop size distributions among the south, central, north, and eastern parts of Taiwan, with more large drops in central Taiwan. To comprehend the microphysical progressions causing the regional and intra-seasonal fluctuations, CFADs (contoured frequency by altitude diagrams) of rain parameters are utilized. Compared to other two sub-seasons, the early-Mei-yu season exhibited weaker convection. Dominance of stratiform precipitation in late-Mei-yu season, and convective precipitation in post-Mei-yu season resulted in higher rainfall amounts in these two sub-seasons (more particularly in post-Mei-yu) than the early-Mei-yu season. Examination of warm rain microphysical processes (below 5 km height) among these sub-seasons revealed that the early-Mei-yu season is dominated with break-up process, late-Mei-yu season with breakup and coalescence balance, and post-Mei-yu with coalescence, size-sorting and evaporation processes.
期刊介绍:
JGR: Atmospheres publishes articles that advance and improve understanding of atmospheric properties and processes, including the interaction of the atmosphere with other components of the Earth system.