Matches in SemOpenAlex for { <https://semopenalex.org/work/W4308341479> ?p ?o ?g. }
- W4308341479 endingPage "3049" @default.
- W4308341479 startingPage "3031" @default.
- W4308341479 abstract "Abstract This study investigates the organizational modes of convective storms and associated severe weather in spring and summer (March–August) of 2015–19 over southern China. These storms are classified into three major organizational structures (cellular, linear, and nonlinear), including 10 dominant morphologies. In general, cellular systems are most frequent, followed by linear systems. Convective storms are common in spring, increasing markedly from April to June, and peak in June. Convective storm cases are usually longer lived in spring, while shorter lived in summer. They also present pronounced diurnal variations, with a primary peak in the afternoon and several secondary peaks during the night to the morning. Approximately 79.7% of initial convection clearly exhibits a dominant eastward movement, with a faster moving speed in spring. Convective storms frequently evolve among organizational modes during their life spans. Linear systems produce the most severe weather observations, in which convective lines with trailing stratiform rain are most prolific. Bow echoes are most efficient in producing severe weather events among all systems, despite their rare occurrences. In spring, lines with parallel stratiform rain are abundant producers of severe wind events, ranking the second highest probability. In summer, embedded lines produce the second largest proportion of intense rainfall events, whereas lines with leading stratiform rain are most efficient in generating extremely intense rainfall and thus pose a distinct flooding threat. Broken lines produce the largest proportion of severe weather events among cellular storms. In contrast, nonlinear systems possess the weakest capability to produce severe weather events. Significance Statement Under the influence of the East Asian summer monsoon, severe weather events produced by convective storms occur frequently in China, leading to serious natural disasters. Numerous studies have demonstrated that the morphologies of convective storms are helpful to improve our understanding and prediction of convective storms. However, fewer attempts have been made to examine the convective morphologies over southern China. We aim to reveal the general features of convective organizational modes (e.g., frequencies, durations, variations, etc.) and determine which particular types of severe weather are more or less likely to be associated with particular convective morphologies. These results are of benefit to local forecasters for better anticipating the storm types and issuing warnings for related hazardous weather." @default.
- W4308341479 created "2022-11-11" @default.
- W4308341479 creator A5004466460 @default.
- W4308341479 creator A5012435102 @default.
- W4308341479 creator A5021817568 @default.
- W4308341479 creator A5050831222 @default.
- W4308341479 creator A5057228969 @default.
- W4308341479 creator A5065140987 @default.
- W4308341479 creator A5079157593 @default.
- W4308341479 date "2022-11-01" @default.
- W4308341479 modified "2023-10-02" @default.
- W4308341479 title "Organizational Modes of Spring and Summer Convective Storms and Associated Severe Weather over Southern China during 2015–19" @default.
- W4308341479 cites W1967757502 @default.
- W4308341479 cites W1975839751 @default.
- W4308341479 cites W1984663247 @default.
- W4308341479 cites W1989067258 @default.
- W4308341479 cites W1990695224 @default.
- W4308341479 cites W2014690889 @default.
- W4308341479 cites W2017200583 @default.
- W4308341479 cites W2032331143 @default.
- W4308341479 cites W2039373026 @default.
- W4308341479 cites W2053843082 @default.
- W4308341479 cites W2055141084 @default.
- W4308341479 cites W2070235302 @default.
- W4308341479 cites W2073683120 @default.
- W4308341479 cites W2087490323 @default.
- W4308341479 cites W2098677536 @default.
- W4308341479 cites W2112556913 @default.
- W4308341479 cites W2123987184 @default.
- W4308341479 cites W2124323707 @default.
- W4308341479 cites W2124639193 @default.
- W4308341479 cites W2130721901 @default.
- W4308341479 cites W2133851322 @default.
- W4308341479 cites W2138682651 @default.
- W4308341479 cites W2144540674 @default.
- W4308341479 cites W2152881735 @default.
- W4308341479 cites W2160097385 @default.
- W4308341479 cites W2164786439 @default.
- W4308341479 cites W2172312359 @default.
- W4308341479 cites W2174313875 @default.
- W4308341479 cites W2175161202 @default.
- W4308341479 cites W2177102455 @default.
- W4308341479 cites W2180592573 @default.
- W4308341479 cites W2374042435 @default.
- W4308341479 cites W2611057193 @default.
- W4308341479 cites W2788212566 @default.
- W4308341479 cites W2797710567 @default.
- W4308341479 cites W2888504372 @default.
- W4308341479 cites W2894721921 @default.
- W4308341479 cites W2904022256 @default.
- W4308341479 cites W2974341751 @default.
- W4308341479 cites W2986809921 @default.
- W4308341479 cites W2990792844 @default.
- W4308341479 cites W3016097621 @default.
- W4308341479 cites W3033409372 @default.
- W4308341479 cites W3039889760 @default.
- W4308341479 cites W3107518062 @default.
- W4308341479 cites W3111200916 @default.
- W4308341479 cites W4200130150 @default.
- W4308341479 cites W4230250764 @default.
- W4308341479 cites W4376848726 @default.
- W4308341479 doi "https://doi.org/10.1175/mwr-d-22-0061.1" @default.
- W4308341479 hasPublicationYear "2022" @default.
- W4308341479 type Work @default.
- W4308341479 citedByCount "1" @default.
- W4308341479 countsByYear W43083414792023 @default.
- W4308341479 crossrefType "journal-article" @default.
- W4308341479 hasAuthorship W4308341479A5004466460 @default.
- W4308341479 hasAuthorship W4308341479A5012435102 @default.
- W4308341479 hasAuthorship W4308341479A5021817568 @default.
- W4308341479 hasAuthorship W4308341479A5050831222 @default.
- W4308341479 hasAuthorship W4308341479A5057228969 @default.
- W4308341479 hasAuthorship W4308341479A5065140987 @default.
- W4308341479 hasAuthorship W4308341479A5079157593 @default.
- W4308341479 hasConcept C105306849 @default.
- W4308341479 hasConcept C10899652 @default.
- W4308341479 hasConcept C127313418 @default.
- W4308341479 hasConcept C153294291 @default.
- W4308341479 hasConcept C187460315 @default.
- W4308341479 hasConcept C190930322 @default.
- W4308341479 hasConcept C192932206 @default.
- W4308341479 hasConcept C196937547 @default.
- W4308341479 hasConcept C205649164 @default.
- W4308341479 hasConcept C29141058 @default.
- W4308341479 hasConcept C39432304 @default.
- W4308341479 hasConcept C49204034 @default.
- W4308341479 hasConcept C91586092 @default.
- W4308341479 hasConceptScore W4308341479C105306849 @default.
- W4308341479 hasConceptScore W4308341479C10899652 @default.
- W4308341479 hasConceptScore W4308341479C127313418 @default.
- W4308341479 hasConceptScore W4308341479C153294291 @default.
- W4308341479 hasConceptScore W4308341479C187460315 @default.
- W4308341479 hasConceptScore W4308341479C190930322 @default.
- W4308341479 hasConceptScore W4308341479C192932206 @default.
- W4308341479 hasConceptScore W4308341479C196937547 @default.
- W4308341479 hasConceptScore W4308341479C205649164 @default.
- W4308341479 hasConceptScore W4308341479C29141058 @default.
- W4308341479 hasConceptScore W4308341479C39432304 @default.