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Chinese Academy of Sciences Institutional Repositories Grid
Diurnal variations of summer precipitation over the regions east to Tibetan Plateau

文献类型:期刊论文

作者Wu, Yang1; Huang, Anning1; Huang, Danqing1; Chen, Fei2; Yang, Ben1; Zhou, Yang3; Fang, Dexian4; Zhang, Lujun1; Wen, Lijuan5
刊名CLIMATE DYNAMICS
出版日期2018-12-01
卷号51期号:11-12页码:4287-4307
ISSN号0930-7575
DOI10.1007/s00382-017-4042-x
通讯作者Huang, Anning(anhuang@nju.edu.cn) ; Huang, Danqing(huangdq@nju.edu.cn)
英文摘要Based on the hourly gauge-satellite merged precipitation product with the horizontal resolution of 0.1 degrees latitude/longitude during 2008-2014, diurnal variations of the summer precipitation amount (PA), frequency (PF), and intensity (PI) with different duration time over the regions east to Tibetan Plateau have been systematically revealed in this study. Results indicate that the eight typical precipitation diurnal patterns identified by the cluster analysis display pronounced regional features among the plateaus, basins, plains, hilly and coastal areas. The precipitation diurnal cycles are significantly affected by the sub-grid terrain fluctuations. The PA, PF and PI of the total rainfall show much more pronounced double diurnal peaks with the sub-grid topography standard deviation (SD) decreased. Meanwhile, the diurnal peaks of PA and PF (PI) strengthen (weaken) with the sub-grid topography SD enhanced. Over the elevated mountain ranges, southeastern hilly and coastal regions, the PA and PF diurnal patterns of the total rainfall generally show predominant late-afternoon peaks, which are closely associated with the short-duration (3h) rainfall. Along the Tibetan Plateau to its downstream, the diurnal peaks of PA, PF and PI for the total rainfall all exhibit obvious eastward phase time delay mainly due to the diurnal evolutions of long-duration (>6h) rainfall. However, the 4-6h rainfall leads to the eastward phase time delay of the total rainfall along the Taihang Mountains to its downstream. Further mechanism analysis suggests that the midnight to morning diurnal evolution of the long-duration rainfall is closely associated with the diurnal variations of the upward branches of thermally driven mountain-plain solenoids and the water vapor transport associated with the accelerated nocturnal southwesterly winds. The late-afternoon peak of the short-duration PA over the southeastern hilly and coastal regions is ascribed to the strong local thermal convections due to the solar heating in afternoon, while the early-evening peak of the short-duration PA over the elevated mountain ranges is significantly contributed by the upward warm-moist wind from the surrounding low-lying basins or plains.
收录类别SCI ; ISTP
WOS关键词WARM-SEASON PRECIPITATION ; MEI-YU FRONT ; MOISTURE TRANSPORT ; DEEP CONVECTION ; RAINFALL ; CYCLE ; MONSOON ; CIRCULATION ; CHINA ; ASIA
WOS研究方向Meteorology & Atmospheric Sciences
WOS类目Meteorology & Atmospheric Sciences
语种英语
WOS记录号WOS:000451725600022
出版者SPRINGER
URI标识http://www.irgrid.ac.cn/handle/1471x/2558248
专题寒区旱区环境与工程研究所
通讯作者Huang, Anning; Huang, Danqing
作者单位1.Nanjing Univ, Sch Atmospher Sci, CMA NJU Joint Lab Climate Predict Studies, 163 Xianlin Ave, Nanjing 210046, Jiangsu, Peoples R China
2.Minist Environm Protect, Nanjing Inst Environm Sci, Nanjing 210042, Jiangsu, Peoples R China
3.Nanjing Univ Informat Sci & Technol, Minist Educ, Collaborat Innovat Ctr Forecast & Evaluat Meteoro, Key Lab Meteorol Disaster, Nanjing 210044, Jiangsu, Peoples R China
4.Chongqing Inst Meteorol & Sci, Chongqing 401147, Peoples R China
5.Chinese Acad Sci, Key Lab Land Surface Proc & Climate Change Cold &, Lanzhou 730000, Peoples R China
推荐引用方式
GB/T 7714
Wu, Yang,Huang, Anning,Huang, Danqing,et al. Diurnal variations of summer precipitation over the regions east to Tibetan Plateau[J]. CLIMATE DYNAMICS,2018,51(11-12):4287-4307.
APA Wu, Yang.,Huang, Anning.,Huang, Danqing.,Chen, Fei.,Yang, Ben.,...&Wen, Lijuan.(2018).Diurnal variations of summer precipitation over the regions east to Tibetan Plateau.CLIMATE DYNAMICS,51(11-12),4287-4307.
MLA Wu, Yang,et al."Diurnal variations of summer precipitation over the regions east to Tibetan Plateau".CLIMATE DYNAMICS 51.11-12(2018):4287-4307.

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来源:寒区旱区环境与工程研究所

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