FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2315204672> ?p ?o ?g. }

• W2315204672 endingPage "560" @default.
• W2315204672 startingPage "540" @default.
• W2315204672 abstract "This study investigates influencing weather systems for and the effect of Tibetan Plateau (TP)’s surface heating on the heavy rainfall over southern China in June 2010, focusing on the four persistent heavy rainfall events during 14–24 June 2010. The major weather systems include the South Asian high, midlatitude trough and ridge, western Pacific subtropical high in the middle troposphere, and shear lines and eastward-moving vortices in the lower troposphere. An ensemble of convection-permitting simulations (CTL) is carried out with the WRF model for these rainfall events, which successfully reproduce the observed evolution of precipitation and weather systems. Another ensemble of simulations (SEN) with the surface albedo over the TP and its southern slope changed artificially to one, i.e., the surface does not absorb any solar heating, otherwise it is identical to CTL, is also performed. Comparison between CTL and SEN suggests that the surface sensible heating of TP in CTL significantly affects the temperature distributions over the plateau and its surroundings, and the thermal wind adjustment consequently changes atmospheric circulations and properties of the synoptic systems, leading to intensified precipitation over southern China. Specifically, at 200 hPa, anticyclonic and cyclonic anomalies form over the western and eastern plateau, respectively, which enhances the southward cold air intrusion along the eastern TP and the divergence over southern China; at 500 hPa, the ridge over the northern plateau and the trough over eastern China are strengthened, the southwesterly flows along the northwestern side of the subtropical high are intensified, and the positive vorticity propagation from the plateau to its downstream is also enhanced significantly; at 850 hPa, the low-pressure vortices strongly develop and move eastward while the southwesterly low-level jet over southern China strengthens in CTL, leading to increased water vapor convergence and upward motion over the precipitation region." @default.
• W2315204672 created "2016-06-24" @default.
• W2315204672 creator A5019695571 @default.
• W2315204672 creator A5081938339 @default.
• W2315204672 creator A5086499138 @default.
• W2315204672 date "2014-08-01" @default.
• W2315204672 modified "2023-09-29" @default.
• W2315204672 title "The persistent heavy rainfall over southern China in June 2010: Evolution of synoptic systems and the effects of the Tibetan Plateau heating" @default.
• W2315204672 cites W1482636228 @default.
• W2315204672 cites W1903603028 @default.
• W2315204672 cites W1979531930 @default.
• W2315204672 cites W1984136939 @default.
• W2315204672 cites W1984160355 @default.
• W2315204672 cites W2000666236 @default.
• W2315204672 cites W2013445189 @default.
• W2315204672 cites W2015062319 @default.
• W2315204672 cites W2020472321 @default.
• W2315204672 cites W2028550342 @default.
• W2315204672 cites W2032521431 @default.
• W2315204672 cites W2076757012 @default.
• W2315204672 cites W2077038911 @default.
• W2315204672 cites W2083339292 @default.
• W2315204672 cites W2101394945 @default.
• W2315204672 cites W2104484944 @default.
• W2315204672 cites W2114883075 @default.
• W2315204672 cites W2121745948 @default.
• W2315204672 cites W2176267398 @default.
• W2315204672 cites W2178057317 @default.
• W2315204672 cites W2179912439 @default.
• W2315204672 cites W2180576529 @default.
• W2315204672 cites W2180799588 @default.
• W2315204672 cites W2211235357 @default.
• W2315204672 cites W2229169132 @default.
• W2315204672 cites W2323981757 @default.
• W2315204672 doi "https://doi.org/10.1007/s13351-014-3284-3" @default.
• W2315204672 hasPublicationYear "2014" @default.
• W2315204672 type Work @default.
• W2315204672 sameAs 2315204672 @default.
• W2315204672 citedByCount "18" @default.
• W2315204672 countsByYear W23152046722017 @default.
• W2315204672 countsByYear W23152046722018 @default.
• W2315204672 countsByYear W23152046722019 @default.
• W2315204672 countsByYear W23152046722020 @default.
• W2315204672 countsByYear W23152046722021 @default.
• W2315204672 countsByYear W23152046722022 @default.
• W2315204672 crossrefType "journal-article" @default.
• W2315204672 hasAuthorship W2315204672A5019695571 @default.
• W2315204672 hasAuthorship W2315204672A5081938339 @default.
• W2315204672 hasAuthorship W2315204672A5086499138 @default.
• W2315204672 hasBestOaLocation W23152046722 @default.
• W2315204672 hasConcept C107054158 @default.
• W2315204672 hasConcept C119947313 @default.
• W2315204672 hasConcept C121332964 @default.
• W2315204672 hasConcept C127313418 @default.
• W2315204672 hasConcept C133204551 @default.
• W2315204672 hasConcept C134306372 @default.
• W2315204672 hasConcept C139719470 @default.
• W2315204672 hasConcept C151730666 @default.
• W2315204672 hasConcept C153294291 @default.
• W2315204672 hasConcept C160945548 @default.
• W2315204672 hasConcept C162164538 @default.
• W2315204672 hasConcept C162324750 @default.
• W2315204672 hasConcept C18101618 @default.
• W2315204672 hasConcept C205649164 @default.
• W2315204672 hasConcept C2780030769 @default.
• W2315204672 hasConcept C32239851 @default.
• W2315204672 hasConcept C32277403 @default.
• W2315204672 hasConcept C33923547 @default.
• W2315204672 hasConcept C49204034 @default.
• W2315204672 hasConcept C67320510 @default.
• W2315204672 hasConcept C9075549 @default.
• W2315204672 hasConcept C91586092 @default.
• W2315204672 hasConcept C97355855 @default.
• W2315204672 hasConceptScore W2315204672C107054158 @default.
• W2315204672 hasConceptScore W2315204672C119947313 @default.
• W2315204672 hasConceptScore W2315204672C121332964 @default.
• W2315204672 hasConceptScore W2315204672C127313418 @default.
• W2315204672 hasConceptScore W2315204672C133204551 @default.
• W2315204672 hasConceptScore W2315204672C134306372 @default.
• W2315204672 hasConceptScore W2315204672C139719470 @default.
• W2315204672 hasConceptScore W2315204672C151730666 @default.
• W2315204672 hasConceptScore W2315204672C153294291 @default.
• W2315204672 hasConceptScore W2315204672C160945548 @default.
• W2315204672 hasConceptScore W2315204672C162164538 @default.
• W2315204672 hasConceptScore W2315204672C162324750 @default.
• W2315204672 hasConceptScore W2315204672C18101618 @default.
• W2315204672 hasConceptScore W2315204672C205649164 @default.
• W2315204672 hasConceptScore W2315204672C2780030769 @default.
• W2315204672 hasConceptScore W2315204672C32239851 @default.
• W2315204672 hasConceptScore W2315204672C32277403 @default.
• W2315204672 hasConceptScore W2315204672C33923547 @default.
• W2315204672 hasConceptScore W2315204672C49204034 @default.
• W2315204672 hasConceptScore W2315204672C67320510 @default.
• W2315204672 hasConceptScore W2315204672C9075549 @default.
• W2315204672 hasConceptScore W2315204672C91586092 @default.
• W2315204672 hasConceptScore W2315204672C97355855 @default.
• W2315204672 hasIssue "4" @default.
• W2315204672 hasLocation W23152046721 @default.

• next