FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W3115443326> ?p ?o ?g. }

• W3115443326 endingPage "52" @default.
• W3115443326 startingPage "52" @default.
• W3115443326 abstract "Based on severe weather reports, surface precipitation observations, surface routine observations, and the European Center for Medium-Range Weather Forecasts ERA5 reanalysis dataset during the warm seasons (May–September) of 2011–2018 over North China, this paper analyzes the statistical characteristics and environmental conditions of three types of severe convective events. Results are compared between events with different altitudes (i.e., mountains and plains), severities (i.e., ordinary and significant), and months. Hail and thunderstorm high winds (THWs) are more common over the mountains whereas short-duration heavy rainfall (SDHR) is more frequent over the plains. The occurrence frequency of severe convective events exhibits distinct monthly and diurnal variations. Analyses of the environmental parameters provide reference for the potential forecasting of severe convective events over this region. Specifically, the 850–500 hPa temperature lapse rate (LR85), pseudo-equivalent potential temperature at 500 hPa (thetase500), and precipitable water (PW) are skillful in distinguishing hail and THW environments from SDHR environments, and thetase500 is useful in discriminating between hail and THW environments. The convective environments over the plains are characterized by significantly higher (lower) PW (LR85) compared with mountains. The skill of these parameters in forecasting the severity of the convective hazards is limited. Probability distributions in the two parameters space indicate that the occurrence of significant hail requires both higher most unstable convective available potential energy (MUCAPE) and stronger 0–6 km bulk wind shear (SHR6) compared with ordinary hail. Compared with ordinary THWs, the significant THWs over the mountains depend more on the SHR6 whereas those over the plains rely more on the MUCAPE. The significant SDHR events over the plains tend to occur under a variety of instability conditions. The thermodynamic parameters (i.e., MUCAPE, thetase500, and downdraft convective available potential energy), and PW are significantly higher in July–August, whereas the LR85 and vertical wind shear are apparently higher in May, June and September." @default.
• W3115443326 created "2021-01-05" @default.
• W3115443326 creator A5026592652 @default.
• W3115443326 creator A5043942714 @default.
• W3115443326 creator A5052926185 @default.
• W3115443326 creator A5058088408 @default.
• W3115443326 creator A5058516510 @default.
• W3115443326 creator A5072790059 @default.
• W3115443326 creator A5078344087 @default.
• W3115443326 date "2020-12-31" @default.
• W3115443326 modified "2023-09-27" @default.
• W3115443326 title "Statistical Characteristics and Environmental Conditions of the Warm-Season Severe Convective Events over North China" @default.
• W3115443326 cites W1582896676 @default.
• W3115443326 cites W1662482809 @default.
• W3115443326 cites W1750477509 @default.
• W3115443326 cites W1970343002 @default.
• W3115443326 cites W1981924456 @default.
• W3115443326 cites W1984559227 @default.
• W3115443326 cites W1990295591 @default.
• W3115443326 cites W1995480410 @default.
• W3115443326 cites W2008793633 @default.
• W3115443326 cites W2014690889 @default.
• W3115443326 cites W2017761002 @default.
• W3115443326 cites W2050297422 @default.
• W3115443326 cites W2052998290 @default.
• W3115443326 cites W2059206665 @default.
• W3115443326 cites W2060430093 @default.
• W3115443326 cites W2067184637 @default.
• W3115443326 cites W2068282327 @default.
• W3115443326 cites W2070787619 @default.
• W3115443326 cites W2075479617 @default.
• W3115443326 cites W2079246256 @default.
• W3115443326 cites W2087490323 @default.
• W3115443326 cites W2087654094 @default.
• W3115443326 cites W2112823219 @default.
• W3115443326 cites W2131760093 @default.
• W3115443326 cites W2135570495 @default.
• W3115443326 cites W2141504340 @default.
• W3115443326 cites W2148847360 @default.
• W3115443326 cites W2149218990 @default.
• W3115443326 cites W2158466588 @default.
• W3115443326 cites W2173268569 @default.
• W3115443326 cites W2322041505 @default.
• W3115443326 cites W2529854520 @default.
• W3115443326 cites W2558593184 @default.
• W3115443326 cites W2574994921 @default.
• W3115443326 cites W2577888971 @default.
• W3115443326 cites W2592042806 @default.
• W3115443326 cites W2611057193 @default.
• W3115443326 cites W2761307268 @default.
• W3115443326 cites W2787062637 @default.
• W3115443326 cites W2788212566 @default.
• W3115443326 cites W2896467450 @default.
• W3115443326 cites W2899939650 @default.
• W3115443326 cites W937396684 @default.
• W3115443326 doi "https://doi.org/10.3390/atmos12010052" @default.
• W3115443326 hasPublicationYear "2020" @default.
• W3115443326 type Work @default.
• W3115443326 sameAs 3115443326 @default.
• W3115443326 citedByCount "3" @default.
• W3115443326 countsByYear W31154433262021 @default.
• W3115443326 countsByYear W31154433262022 @default.
• W3115443326 countsByYear W31154433262023 @default.
• W3115443326 crossrefType "journal-article" @default.
• W3115443326 hasAuthorship W3115443326A5026592652 @default.
• W3115443326 hasAuthorship W3115443326A5043942714 @default.
• W3115443326 hasAuthorship W3115443326A5052926185 @default.
• W3115443326 hasAuthorship W3115443326A5058088408 @default.
• W3115443326 hasAuthorship W3115443326A5058516510 @default.
• W3115443326 hasAuthorship W3115443326A5072790059 @default.
• W3115443326 hasAuthorship W3115443326A5078344087 @default.
• W3115443326 hasBestOaLocation W31154433261 @default.
• W3115443326 hasConcept C105306849 @default.
• W3115443326 hasConcept C107054158 @default.
• W3115443326 hasConcept C10899652 @default.
• W3115443326 hasConcept C127313418 @default.
• W3115443326 hasConcept C135558025 @default.
• W3115443326 hasConcept C153294291 @default.
• W3115443326 hasConcept C156008332 @default.
• W3115443326 hasConcept C161067210 @default.
• W3115443326 hasConcept C187460315 @default.
• W3115443326 hasConcept C192932206 @default.
• W3115443326 hasConcept C205649164 @default.
• W3115443326 hasConcept C39432304 @default.
• W3115443326 hasConcept C49204034 @default.
• W3115443326 hasConcept C61939431 @default.
• W3115443326 hasConcept C80316258 @default.
• W3115443326 hasConcept C89298926 @default.
• W3115443326 hasConcept C91586092 @default.
• W3115443326 hasConceptScore W3115443326C105306849 @default.
• W3115443326 hasConceptScore W3115443326C107054158 @default.
• W3115443326 hasConceptScore W3115443326C10899652 @default.
• W3115443326 hasConceptScore W3115443326C127313418 @default.
• W3115443326 hasConceptScore W3115443326C135558025 @default.
• W3115443326 hasConceptScore W3115443326C153294291 @default.
• W3115443326 hasConceptScore W3115443326C156008332 @default.
• W3115443326 hasConceptScore W3115443326C161067210 @default.
• W3115443326 hasConceptScore W3115443326C187460315 @default.

• next