气候变化领域集成服务门户(CCPortal): Refined Characteristics of Moisture Cycling over the Inland River Basin Using the WRF Model and the Finer Box Model: A Case Study of the Heihe River Basin

CCPortal

DOI	10.3390/atmos12030399
	Refined Characteristics of Moisture Cycling over the Inland River Basin Using the WRF Model and the Finer Box Model: A Case Study of the Heihe River Basin
	Pan, Xiaoduo; Ma, Weiqiang; Zhang, Ying; Li, Hu
通讯作者	Pan, XD ; Ma, WQ (通讯作者)，Chinese Acad Sci, Inst Tibetan Plateau Res, Natl Tibetan Plateau Data Ctr, Key Lab Tibetan Environm Changes & Land Surface P, 16 Lincui Rd, Beijing 100101, Peoples R China.
发表日期	2021
EISSN	2073-4433
卷号	12 期号:3
英文摘要	The Heihe River Basin (HRB), located on the northeastern edge of the Tibetan Plateau, is the second-largest inland river basin in China, with an area of 140,000 km(2). The HRB is a coupling area of the westerlies, the Qinghai-Tibet Plateau monsoon and the Southeast monsoon circulation system, and is a relatively independent land-surface water-circulating system. The refined characteristics of moisture recycling over the HRB was described by using the Weather Research and Forecasting (WRF) model for a long-term simulation, and the finer box model for calculating the net water-vapor flux. The following conclusions were drawn from the results of this study: (1) The water vapor of the HRB was dominantly transported by the wind from the west and from the north, and the west one was much larger than the north one. The net vapor transported by the west wind was positive, and by the north wind was negative. (2) The precipitation over the HRB was triggered mainly by the vapor from the west, which arose from the lower vertical layer to higher one during transporting from west to east. The vapor from the north sank from a higher layer to a lower one, and crossed the south edge of the HRB. (3) The moisture-recycling ratio of evapotranspiration to precipitation over the HRB was much higher than the other regions, which may be due to the strong land-atmosphere interaction in the arid inland river basin.
英文关键词	land– atmosphere interaction; water vapor; weather research and forecasting model; precipitation; evapotranspiration; tuning layer
语种	英语
WOS研究方向	Environmental Sciences & Ecology ; Meteorology & Atmospheric Sciences
WOS类目	Environmental Sciences ; Meteorology & Atmospheric Sciences
WOS记录号	WOS:000635247500001
来源期刊	ATMOSPHERE
来源机构	中国科学院西北生态环境资源研究院
文献类型	期刊论文
条目标识符	http://gcip.llas.ac.cn/handle/2XKMVOVA/254681
作者单位	[Pan, Xiaoduo; Ma, Weiqiang; Li, Hu] Chinese Acad Sci, Inst Tibetan Plateau Res, Natl Tibetan Plateau Data Ctr, Key Lab Tibetan Environm Changes & Land Surface P, 16 Lincui Rd, Beijing 100101, Peoples R China; [Zhang, Ying] Chinese Acad Sci, Northwest Inst Ecoenvironm & Resources, Key Lab Remote Sensing Gansu Prov, Lanzhou 730000, Peoples R China; [Li, Hu] Univ Chinese Acad Sci, Grad Sch Beijing Sci & Technol, Beijing 100049, Peoples R China
推荐引用方式 GB/T 7714	Pan, Xiaoduo,Ma, Weiqiang,Zhang, Ying,et al. Refined Characteristics of Moisture Cycling over the Inland River Basin Using the WRF Model and the Finer Box Model: A Case Study of the Heihe River Basin[J]. 中国科学院西北生态环境资源研究院,2021,12(3).
APA	Pan, Xiaoduo,Ma, Weiqiang,Zhang, Ying,&Li, Hu.(2021).Refined Characteristics of Moisture Cycling over the Inland River Basin Using the WRF Model and the Finer Box Model: A Case Study of the Heihe River Basin.ATMOSPHERE,12(3).
MLA	Pan, Xiaoduo,et al."Refined Characteristics of Moisture Cycling over the Inland River Basin Using the WRF Model and the Finer Box Model: A Case Study of the Heihe River Basin".ATMOSPHERE 12.3(2021).