FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2002046153> ?p ?o ?g. }

• W2002046153 endingPage "1046" @default.
• W2002046153 startingPage "1035" @default.
• W2002046153 abstract "This study presented a quantitative climatology of atmospheric moisture affecting the Yangtze River Basin (YRB) region in boreal summer season, as well as the spatial evolution of atmospheric moisture passage towards the target regions. A three-dimensional Lagrangian particle dispersion model FLEXPART was driven by the National Centers for Environmental Prediction Final Operational Global Analysis data combined with a backtracking scheme, and the transport contributions to the moisture budget over the YRB region was identified through the continuous calculation of changes in specific humidity along the FLEXPART back trajectories of all air masses residing over this region for a period of six summers of year 2004–2009. The back trajectory analysis revealed four major moisture sources contributed to the YRB summer water vapour with different transport timescales: the East China Sea (17.5%), South China Sea (26.6%), Indian peninsula and the Bay of Bengal (20.5%) and Arabian Sea (13.6%). The properties of moisture sources and its transport processes are dominated by the Asian Summer Monsoon regimes. The Tibetan Plateau also acts as an effective barrier for the meridional moisture transport, leading to distinct moisture sinks at the southern slope. In contrast to the previous results, the tropical western Pacific only plays a minor role in the water vapour contributors. The importance of the four source areas varies over the summer: East and South China Sea sources persist throughout the summer, whereas the Indian peninsula, the Bay of Bengal and Arabian Sea sources reach the strongest moisture supply to the YRB region only in high summer (July), showing a close association with the March of Asian monsoon. The further evaluation shows that the inter-annual variability of precipitation over YRB is strongly related to the moisture sources in the Bay of Bengal and Arabian Sea. Copyright © 2012 Royal Meteorological Society" @default.
• W2002046153 created "2016-06-24" @default.
• W2002046153 creator A5012593462 @default.
• W2002046153 creator A5031192198 @default.
• W2002046153 creator A5071562362 @default.
• W2002046153 date "2012-04-16" @default.
• W2002046153 modified "2023-09-27" @default.
• W2002046153 title "Main moisture sources affecting lower Yangtze River Basin in boreal summers during 2004-2009" @default.
• W2002046153 cites W1749048564 @default.
• W2002046153 cites W1956875444 @default.
• W2002046153 cites W1969811424 @default.
• W2002046153 cites W1978457348 @default.
• W2002046153 cites W1984819644 @default.
• W2002046153 cites W1987371862 @default.
• W2002046153 cites W1988641306 @default.
• W2002046153 cites W1990429383 @default.
• W2002046153 cites W2015542569 @default.
• W2002046153 cites W2034326114 @default.
• W2002046153 cites W2039785873 @default.
• W2002046153 cites W2044505862 @default.
• W2002046153 cites W2045474363 @default.
• W2002046153 cites W2051776321 @default.
• W2002046153 cites W2066704063 @default.
• W2002046153 cites W2068725057 @default.
• W2002046153 cites W2073781242 @default.
• W2002046153 cites W2075535082 @default.
• W2002046153 cites W2081756291 @default.
• W2002046153 cites W2086894765 @default.
• W2002046153 cites W2094527983 @default.
• W2002046153 cites W2095133446 @default.
• W2002046153 cites W2099985906 @default.
• W2002046153 cites W2101076395 @default.
• W2002046153 cites W2108513177 @default.
• W2002046153 cites W2110198356 @default.
• W2002046153 cites W2114150302 @default.
• W2002046153 cites W2127632183 @default.
• W2002046153 cites W2132321424 @default.
• W2002046153 cites W2142401028 @default.
• W2002046153 cites W2148457324 @default.
• W2002046153 cites W2176800120 @default.
• W2002046153 cites W2176956584 @default.
• W2002046153 cites W2403488102 @default.
• W2002046153 cites W2514725356 @default.
• W2002046153 cites W2598647511 @default.
• W2002046153 doi "https://doi.org/10.1002/joc.3495" @default.
• W2002046153 hasPublicationYear "2012" @default.
• W2002046153 type Work @default.
• W2002046153 sameAs 2002046153 @default.
• W2002046153 citedByCount "45" @default.
• W2002046153 countsByYear W20020461532014 @default.
• W2002046153 countsByYear W20020461532015 @default.
• W2002046153 countsByYear W20020461532016 @default.
• W2002046153 countsByYear W20020461532017 @default.
• W2002046153 countsByYear W20020461532018 @default.
• W2002046153 countsByYear W20020461532019 @default.
• W2002046153 countsByYear W20020461532020 @default.
• W2002046153 countsByYear W20020461532021 @default.
• W2002046153 countsByYear W20020461532022 @default.
• W2002046153 countsByYear W20020461532023 @default.
• W2002046153 crossrefType "journal-article" @default.
• W2002046153 hasAuthorship W2002046153A5012593462 @default.
• W2002046153 hasAuthorship W2002046153A5031192198 @default.
• W2002046153 hasAuthorship W2002046153A5071562362 @default.
• W2002046153 hasConcept C100537666 @default.
• W2002046153 hasConcept C109007969 @default.
• W2002046153 hasConcept C111368507 @default.
• W2002046153 hasConcept C115880899 @default.
• W2002046153 hasConcept C123588078 @default.
• W2002046153 hasConcept C127313418 @default.
• W2002046153 hasConcept C136996986 @default.
• W2002046153 hasConcept C151730666 @default.
• W2002046153 hasConcept C153294291 @default.
• W2002046153 hasConcept C166957645 @default.
• W2002046153 hasConcept C176864760 @default.
• W2002046153 hasConcept C205649164 @default.
• W2002046153 hasConcept C2776914140 @default.
• W2002046153 hasConcept C2779345167 @default.
• W2002046153 hasConcept C2780789209 @default.
• W2002046153 hasConcept C39432304 @default.
• W2002046153 hasConcept C49204034 @default.
• W2002046153 hasConcept C91586092 @default.
• W2002046153 hasConceptScore W2002046153C100537666 @default.
• W2002046153 hasConceptScore W2002046153C109007969 @default.
• W2002046153 hasConceptScore W2002046153C111368507 @default.
• W2002046153 hasConceptScore W2002046153C115880899 @default.
• W2002046153 hasConceptScore W2002046153C123588078 @default.
• W2002046153 hasConceptScore W2002046153C127313418 @default.
• W2002046153 hasConceptScore W2002046153C136996986 @default.
• W2002046153 hasConceptScore W2002046153C151730666 @default.
• W2002046153 hasConceptScore W2002046153C153294291 @default.
• W2002046153 hasConceptScore W2002046153C166957645 @default.
• W2002046153 hasConceptScore W2002046153C176864760 @default.
• W2002046153 hasConceptScore W2002046153C205649164 @default.
• W2002046153 hasConceptScore W2002046153C2776914140 @default.
• W2002046153 hasConceptScore W2002046153C2779345167 @default.
• W2002046153 hasConceptScore W2002046153C2780789209 @default.
• W2002046153 hasConceptScore W2002046153C39432304 @default.
• W2002046153 hasConceptScore W2002046153C49204034 @default.

• next