FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W3203397854> ?p ?o ?g. }

• W3203397854 endingPage "105871" @default.
• W3203397854 startingPage "105871" @default.
• W3203397854 abstract "Impacts of aerosol direct (ADE) and aerosol indirect (AIE) effects on an extreme rainfall event over Beijing on 19–21 July 2016 were analyzed by conducting four numerical experiments with the Weather Research and Forecasting model coupled with Chemistry (WRF-Chem). The analysis shows that the ADE and AIE change the distribution of the rainfall centers and concentrate rainfall in urban areas. The ADE-induced hourly rainfall intensity increases by about 1 mm h −1 , 10 mm h −1 , and 5 mm h −1 , whereas AIE-induced hourly rainfall intensity decreases by about 1.4 mm h −1 , 10 mm h −1 , and 3 mm h −1 in Beijing, central and eastern part of Beijing during 1200–1800 BJT on 19 July, respectively. The ADE has a slight impact (variation <0.3 mm h −1 ) on the hourly rainfall intensity, whereas the AIE increases the hourly rainfall intensity by about 1 mm h −1 in Beijing; the ADE and AIE increase the hourly rainfall intensity by about 12 mm h −1 and 20 mm h −1 in central part of Beijing while decrease by about 10 mm h −1 and 21 mm h −1 in eastern part of Beijing during 1200–1800 BJT on 20 July, respectively. The ADE destabilizes the atmosphere due to the increase in atmospheric diabatic heating, leading to an increase in rainfall in Beijing during 1200–1800 BJT on 19 July. The nucleation of more aerosols to cloud droplets, which decreases the size of the droplets and inhibits collision, decreasing the amount of rainfall. The impact of the ADE on rainfall is weakened due to the wet deposition caused by rainfall decreasing the aerosol concentration during 1200–1800 BJT on 20 July. The AIE increases the number of collisions and therefore increases the amount of rainfall. The difference in vertical speed is responsible for the difference in the local hourly rainfall intensity for central and eastern part of Beijing during 1200–1800 BJT on 20 July. • The impacts of direct and indirect aerosol effects on an extreme heavy rainfall in Beijing are revealed in detail. • Pollution, meteorology, and thermo-dynamical of this rainfall event on 19–21 July 2016 were revealed by WRF-Chem. • Relative effects of direct and indirect aerosol effects on rainfall were investigated. • Differences in aerosol effects on vertical speed and collision are the main reasons for the differences in rainfall." @default.
• W3203397854 created "2021-10-11" @default.
• W3203397854 creator A5006291503 @default.
• W3203397854 creator A5049056995 @default.
• W3203397854 creator A5056596548 @default.
• W3203397854 creator A5069133820 @default.
• W3203397854 date "2021-12-01" @default.
• W3203397854 modified "2023-09-26" @default.
• W3203397854 title "Numerical analysis of aerosol direct and indirect effects on an extreme rainfall event over Beijing in July 2016" @default.
• W3203397854 cites W1508498710 @default.
• W3203397854 cites W1513871976 @default.
• W3203397854 cites W1900594609 @default.
• W3203397854 cites W1969480794 @default.
• W3203397854 cites W1972989419 @default.
• W3203397854 cites W1993064731 @default.
• W3203397854 cites W2001229805 @default.
• W3203397854 cites W2001678051 @default.
• W3203397854 cites W2002570697 @default.
• W3203397854 cites W2003304723 @default.
• W3203397854 cites W2008177083 @default.
• W3203397854 cites W2008474208 @default.
• W3203397854 cites W2010640017 @default.
• W3203397854 cites W2014840824 @default.
• W3203397854 cites W2015698815 @default.
• W3203397854 cites W2027425310 @default.
• W3203397854 cites W2031675844 @default.
• W3203397854 cites W2036516380 @default.
• W3203397854 cites W2057641318 @default.
• W3203397854 cites W2064188955 @default.
• W3203397854 cites W2067318157 @default.
• W3203397854 cites W2067911916 @default.
• W3203397854 cites W2069460427 @default.
• W3203397854 cites W2075278499 @default.
• W3203397854 cites W2083985768 @default.
• W3203397854 cites W2087485762 @default.
• W3203397854 cites W2087990474 @default.
• W3203397854 cites W2090830020 @default.
• W3203397854 cites W2093381698 @default.
• W3203397854 cites W2094433086 @default.
• W3203397854 cites W2095029195 @default.
• W3203397854 cites W2101394945 @default.
• W3203397854 cites W2105923053 @default.
• W3203397854 cites W2121690346 @default.
• W3203397854 cites W2140805694 @default.
• W3203397854 cites W2142794782 @default.
• W3203397854 cites W2143802999 @default.
• W3203397854 cites W2153988972 @default.
• W3203397854 cites W2173852084 @default.
• W3203397854 cites W2179666172 @default.
• W3203397854 cites W2321241648 @default.
• W3203397854 cites W2460319032 @default.
• W3203397854 cites W2516137856 @default.
• W3203397854 cites W2521751573 @default.
• W3203397854 cites W2561345901 @default.
• W3203397854 cites W2773079125 @default.
• W3203397854 cites W2783166613 @default.
• W3203397854 cites W2799815913 @default.
• W3203397854 cites W2895143048 @default.
• W3203397854 cites W2923060256 @default.
• W3203397854 cites W2959256296 @default.
• W3203397854 cites W2970752774 @default.
• W3203397854 cites W2981977949 @default.
• W3203397854 cites W2982150552 @default.
• W3203397854 cites W2986418128 @default.
• W3203397854 cites W3013886998 @default.
• W3203397854 cites W3025949386 @default.
• W3203397854 cites W3042222091 @default.
• W3203397854 cites W3155726744 @default.
• W3203397854 cites W3198868306 @default.
• W3203397854 doi "https://doi.org/10.1016/j.atmosres.2021.105871" @default.
• W3203397854 hasPublicationYear "2021" @default.
• W3203397854 type Work @default.
• W3203397854 sameAs 3203397854 @default.
• W3203397854 citedByCount "5" @default.
• W3203397854 countsByYear W32033978542022 @default.
• W3203397854 countsByYear W32033978542023 @default.
• W3203397854 crossrefType "journal-article" @default.
• W3203397854 hasAuthorship W3203397854A5006291503 @default.
• W3203397854 hasAuthorship W3203397854A5049056995 @default.
• W3203397854 hasAuthorship W3203397854A5056596548 @default.
• W3203397854 hasAuthorship W3203397854A5069133820 @default.
• W3203397854 hasConcept C121332964 @default.
• W3203397854 hasConcept C127313418 @default.
• W3203397854 hasConcept C153294291 @default.
• W3203397854 hasConcept C166957645 @default.
• W3203397854 hasConcept C191935318 @default.
• W3203397854 hasConcept C205649164 @default.
• W3203397854 hasConcept C2778304055 @default.
• W3203397854 hasConcept C2779345167 @default.
• W3203397854 hasConcept C2779662365 @default.
• W3203397854 hasConcept C39432304 @default.
• W3203397854 hasConcept C49204034 @default.
• W3203397854 hasConcept C62520636 @default.
• W3203397854 hasConcept C91586092 @default.
• W3203397854 hasConceptScore W3203397854C121332964 @default.
• W3203397854 hasConceptScore W3203397854C127313418 @default.
• W3203397854 hasConceptScore W3203397854C153294291 @default.
• W3203397854 hasConceptScore W3203397854C166957645 @default.

• next