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    Thermal Effects of the Surface Heat Flux on Cloud Systems over the Tibetan Plateau in Boreal Summer

    Source: Journal of Climate:;2019:;volume 032:;issue 015::page 4699
    Author:
    Chen, Jinghua
    ,
    Wu, Xiaoqing
    ,
    Yin, Yan
    ,
    Lu, Chunsong
    ,
    Xiao, Hui
    ,
    Huang, Qian
    ,
    Deng, Liping
    DOI: 10.1175/JCLI-D-18-0604.1
    Publisher: American Meteorological Society
    Abstract: ABSTRACTThe influence of surface heat fluxes on the generation and development of cloud and precipitation and its relative importance to the large-scale circulation patterns are investigated via cloud-resolving model (CRM) simulations over the Tibetan Plateau (TP) during boreal summer. Over the lowland (e.g., along the middle and lower reaches of the Yangtze River), the dynamical and thermal properties of the atmosphere take more responsibility than the surface heat fluxes for the triggering of heavy rainfall events. However, the surface thermal driving force is a necessary criterion for the triggering of heavy rainfall in the eastern and western TP (ETP and WTP). Strong surface heat fluxes can trigger shallow convections in the TP. Furthermore, moisture that is mainly transported from the southern tropical ocean has a greater influence on the heavy rainfall events of the WTP than those of the ETP. Cloud microphysical processes are substantially less active and heavy rainfall cannot be produced when surface heat fluxes are weakened by half in magnitude over the TP. In addition, surface heating effects are largely responsible for the high occurrence frequency of convection during the afternoon, and the cloud tops of convective systems show a positive relationship with the intensity of surface heat fluxes.
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      Thermal Effects of the Surface Heat Flux on Cloud Systems over the Tibetan Plateau in Boreal Summer

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    http://yetl.yabesh.ir/yetl1/handle/yetl/4263156
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    contributor authorChen, Jinghua
    contributor authorWu, Xiaoqing
    contributor authorYin, Yan
    contributor authorLu, Chunsong
    contributor authorXiao, Hui
    contributor authorHuang, Qian
    contributor authorDeng, Liping
    date accessioned2019-10-05T06:42:19Z
    date available2019-10-05T06:42:19Z
    date copyright5/14/2019 12:00:00 AM
    date issued2019
    identifier otherJCLI-D-18-0604.1.pdf
    identifier urihttp://yetl.yabesh.ir/yetl1/handle/yetl/4263156
    description abstractABSTRACTThe influence of surface heat fluxes on the generation and development of cloud and precipitation and its relative importance to the large-scale circulation patterns are investigated via cloud-resolving model (CRM) simulations over the Tibetan Plateau (TP) during boreal summer. Over the lowland (e.g., along the middle and lower reaches of the Yangtze River), the dynamical and thermal properties of the atmosphere take more responsibility than the surface heat fluxes for the triggering of heavy rainfall events. However, the surface thermal driving force is a necessary criterion for the triggering of heavy rainfall in the eastern and western TP (ETP and WTP). Strong surface heat fluxes can trigger shallow convections in the TP. Furthermore, moisture that is mainly transported from the southern tropical ocean has a greater influence on the heavy rainfall events of the WTP than those of the ETP. Cloud microphysical processes are substantially less active and heavy rainfall cannot be produced when surface heat fluxes are weakened by half in magnitude over the TP. In addition, surface heating effects are largely responsible for the high occurrence frequency of convection during the afternoon, and the cloud tops of convective systems show a positive relationship with the intensity of surface heat fluxes.
    publisherAmerican Meteorological Society
    titleThermal Effects of the Surface Heat Flux on Cloud Systems over the Tibetan Plateau in Boreal Summer
    typeJournal Paper
    journal volume32
    journal issue15
    journal titleJournal of Climate
    identifier doi10.1175/JCLI-D-18-0604.1
    journal fristpage4699
    journal lastpage4714
    treeJournal of Climate:;2019:;volume 032:;issue 015
    contenttypeFulltext
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    DSpace software copyright © 2002-2015  DuraSpace
    نرم افزار کتابخانه دیجیتال "دی اسپیس" فارسی شده توسط یابش برای کتابخانه های ایرانی | تماس با یابش
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