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In this study, we analyze extreme storms in Tropical and Subtropical East Asia, a moisture\u2010rich environment with complex terrain and oceanic regions. The Tropical Rainfall Measuring Mission's Precipitation Radar is utilized to characterize the frequency and rainfall intensity of four extreme storm types. Extreme storms producing heavy precipitation are categorized into four types: deep convective cores (DCCs), deepwide convective cores (DWCCs), wide convective cores (WCCs), and broad stratiforms regions (BSRs). DCCs and DWCCs occur more frequently and produce stronger rain intensities over land compared to those over ocean. However, WCCs and BSRs occur more frequently over oceans, especially in association with the Meiyu front season and climatological progression in the northern subregions. Although the Convective Cores show higher rain intensities than the BSRs, they show lower volumetric rain rate due to their comparatively smaller horizontal area. An ingredients\u2010based framework is applied to find key similarities across the different heavy rainfall\u2010producing storms near Taiwan using ERA5 reanalysis. The analysis shows that the broader systems (i.e., WCCs and BSRs) are associated with larger in area and longer timescales of vertical moisture flux and low\u2010level wind shear that support the development of the horizontally large, organized storms. Smaller DCCs do not show strong vertical moisture flux on the spatial scales resolved by the reanalysis, suggesting their more local nature and less meso\u2010 or synoptic scale support.<\/jats:p>","DOI":"10.1029\/2022jd036863","type":"journal-article","created":{"date-parts":[[2022,11,29]],"date-time":"2022-11-29T08:30:23Z","timestamp":1669710623000},"update-policy":"https:\/\/doi.org\/10.1002\/crossmark_policy","source":"Crossref","is-referenced-by-count":4,"title":["A Climatology of Extreme Convective Storms in Tropical and Subtropical East Asia and Their Ingredients for Heavy Rainfall as Seen by TRMM"],"prefix":"10.1029","volume":"127","author":[{"ORCID":"https:\/\/orcid.org\/0000-0002-1221-9670","authenticated-orcid":false,"given":"Warittha","family":"Panasawatwong","sequence":"first","affiliation":[{"name":"Department of Atmospheric Science Colorado State University  Fort Collins CO USA"}],"role":[{"vocabulary":"crossref","role":"author"}]},{"ORCID":"https:\/\/orcid.org\/0000-0003-1321-0974","authenticated-orcid":false,"given":"Kristen L.","family":"Rasmussen","sequence":"additional","affiliation":[{"name":"Department of Atmospheric Science Colorado State University  Fort Collins CO USA"}],"role":[{"vocabulary":"crossref","role":"author"}]},{"ORCID":"https:\/\/orcid.org\/0000-0002-0496-331X","authenticated-orcid":false,"given":"Michael M.","family":"Bell","sequence":"additional","affiliation":[{"name":"Department of Atmospheric Science Colorado State University  Fort Collins CO USA"}],"role":[{"vocabulary":"crossref","role":"author"}]}],"member":"13","published-online":{"date-parts":[[2022,12,25]]},"reference":[{"key":"e_1_2_8_2_1","doi-asserted-by":"publisher","DOI":"10.2467\/mripapers1950.24.2_157"},{"key":"e_1_2_8_3_1","doi-asserted-by":"publisher","DOI":"10.1175\/2007JAMC1611.1"},{"key":"e_1_2_8_4_1","doi-asserted-by":"publisher","DOI":"10.1109\/IGARSS.1997.608993"},{"key":"e_1_2_8_5_1","doi-asserted-by":"publisher","DOI":"10.1175\/JHM-D-19-0192.1"},{"key":"e_1_2_8_6_1","doi-asserted-by":"publisher","DOI":"10.1175\/JTECH-D-15-0234.1"},{"key":"e_1_2_8_7_1","doi-asserted-by":"publisher","DOI":"10.1175\/JCLI-3257.1"},{"key":"e_1_2_8_8_1","doi-asserted-by":"publisher","DOI":"10.1175\/1520-0493(2003)131<1323:trcot>2.0.co;2"},{"key":"e_1_2_8_9_1","doi-asserted-by":"publisher","DOI":"10.1175\/WAF1033.1"},{"key":"e_1_2_8_10_1","doi-asserted-by":"publisher","DOI":"10.1175\/1520-0469(1996)053\u23291380:MVODCI\u232a2.0.CO;2"},{"key":"e_1_2_8_11_1","unstructured":"Copernicus Climate Change Service (C3S). 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