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dc.contributor.authorShen, Chong
dc.contributor.authorChen, Xiaoyang
dc.contributor.authorDai, Wei
dc.contributor.authorLi, Xiaohui
dc.contributor.authorWu, Jie
dc.contributor.authorFan, Qi
dc.contributor.authorWang, Xuemei
dc.contributor.authorZhu, Liye
dc.contributor.authorChan, Pakwai
dc.contributor.authorHang, Jian
dc.contributor.authorFan, Shaojia
dc.contributor.authorLi, Weibiao
dc.date.accessioned2019-10-05T06:49:06Z
dc.date.available2019-10-05T06:49:06Z
dc.date.copyright4/5/2019 12:00:00 AM
dc.date.issued2019
dc.identifier.otherJAMC-D-18-0114.1.pdf
dc.identifier.urihttp://yetl.yabesh.ir/yetl1/handle/yetl/4263511
dc.description.abstractAbstractOn urban scales, the detailed characteristics of land-use information and building properties are vital to improving the meteorological model. The WRF Model with high-spatial-resolution urban fraction (UF) and urban morphology (UM) is used to study the impacts of these urban canopy parameters (UCPs) on dynamical and thermal meteorological fields in two representative seasons in Guangzhou. The results of two seasons are similar and as follows. 1) The impacts of updated UF and UM are obvious on wind speed but minor on temperature and humidity. In the urban environment, the results with updated UF and UM are more consistent with observations compared with the default UCPs, which means the performance of the model has been improved. 2) The dynamical factors associated with wind speed are analyzed. Turbulent kinetic energy (TKE) is significantly affected by UM but little by UF. And both UF and UM are found to influence friction velocity U*. The UM and greater UF attained larger U*. 3) In addition, the thermal fields are analyzed. The UM and increased UF induce higher surface skin temperature (TSK) and ground heat flux in the daytime, indicating that more heat is transported from the surface to the soil. At night, more heat is transported from the soil to the surface, producing higher TSK. For sensible heat flux (HFX), greater UF induces larger HFX during the daytime. But the effects of UM are complex, which makes HFX decrease during the daytime and increase at night. Finally, larger UF attains lower latent heat in the daytime.
dc.publisherAmerican Meteorological Society
dc.titleImpacts of High-Resolution Urban Canopy Parameters within the WRF Model on Dynamical and Thermal Fields over Guangzhou, China
dc.typeJournal Paper
dc.journal.volume58
dc.journal.issue5
dc.journal.titleJournal of Applied Meteorology and Climatology
dc.identifier.doi10.1175/JAMC-D-18-0114.1
dc.journal.fristpage1155
dc.journal.lastpage1176
dc.treeJournal of Applied Meteorology and Climatology:;2019:;volume 058:;issue 005
dc.contenttypeFulltext


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