干旱区生态环境知识资源中心(Arid): Spatiotemporal distribution and variation of wind erosion over the Tibetan Plateau based on a coupled land-surface wind-erosion model

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DOI	10.1016/j.aeolia.2021.100699
	Spatiotemporal distribution and variation of wind erosion over the Tibetan Plateau based on a coupled land-surface wind-erosion model
	Jiang, Yingsha; Gao, Yanhong; He, Cenlin; Liu, Benli; Pan, Yongjie; Li, Xia
通讯作者	Gao, YH (corresponding author), Fudan Univ, Dept Atmospher & Ocean Sci, 2005 Songhu Rd, Shanghai 200438, Peoples R China. ; Gao, YH (corresponding author), Fudan Univ, Inst Atmospher Sci, 2005 Songhu Rd, Shanghai 200438, Peoples R China.
来源期刊	AEOLIAN RESEARCH
ISSN	1875-9637
EISSN	2212-1684
出版年	2021
卷号	50
英文摘要	Wind erosion has notable impacts on ecology, water supply and regional climate, but its distributions and longterm changes are still poorly quantified for the Tibetan Plateau (TP). This study develops a coupled land-surface wind-erosion model (HRLDAS-WEPS) in two dimensions horizontally to analyze wind-erosion distributions and its temporal variations under the climate change in 1979?2015 over the entire TP. Two model enhancements are also used, including the application of MODIS vegetation datasets and the optimization of snow-cover parameterizations. Evaluation results indicate that the enhanced coupled model can generally represent the winderosion distributions over the TP, being mainly located in the arid and semi-arid areas and occurring in winter and spring, as compared with station observations and satellite datasets. In 1979?2015, wind erosion has a significant (P < 0.01) decreasing trend of -0.54 kg m- 2 yr- 1 for annual total soil loss averaged over the arid and semi-arid areas of the TP, which is mainly due to the significant (P < 0.01) declining wind speed and increasing soil moisture. The severest wind-erosion reduction is located to the northwest of the 200 mm precipitation line and the Qaidam Basin. Furthermore, a significant turning point of wind-erosion variation is found in 1992. Specifically, wind erosion over the TP decreases from 1979 to 1991 (-1.26 kg m- 2 yr- 1), and then stays at a low level with a slight increase (0.08 kg m- 2 yr- 1) since 1993. This is probably due to the abrupt change of wind speed over the TP in 1991.
英文关键词	Wind-erosion modeling HRLDAS WEPS Tibetan Plateau Temporal variation
类型	Article
语种	英语
收录类别	SCI-E
WOS记录号	WOS:000647794600001
WOS关键词	SNOW-COVER ; CLIMATE-CHANGE ; PREDICTION SYSTEM ; NORTHERN CHINA ; AEOLIAN DUST ; RIVER-BASIN ; SIMULATIONS ; SOIL ; VARIABILITY ; SPEED
WOS类目	Geography, Physical
WOS研究方向	Physical Geography
资源类型	期刊论文
条目标识符	http://119.78.100.177/qdio/handle/2XILL650/349287
作者单位	[Jiang, Yingsha; Pan, Yongjie; Li, Xia] Chinese Acad Sci, Northwest Inst Ecoenvironm & Resources, Key Lab Land Surface Proc & Climate Change Cold &, Lanzhou, Peoples R China; [Gao, Yanhong] Fudan Univ, Dept Atmospher & Ocean Sci, 2005 Songhu Rd, Shanghai 200438, Peoples R China; [Gao, Yanhong] Fudan Univ, Inst Atmospher Sci, 2005 Songhu Rd, Shanghai 200438, Peoples R China; [He, Cenlin] Natl Ctr Atmospher Res, Res Applicat Lab, POB 3000, Boulder, CO 80307 USA; [Liu, Benli] Chinese Acad Sci, Northwest Inst Ecoenvironm & Resources, Key Lab Desert & Desertificat, Lanzhou, Peoples R China
推荐引用方式 GB/T 7714	Jiang, Yingsha,Gao, Yanhong,He, Cenlin,et al. Spatiotemporal distribution and variation of wind erosion over the Tibetan Plateau based on a coupled land-surface wind-erosion model[J],2021,50.
APA	Jiang, Yingsha,Gao, Yanhong,He, Cenlin,Liu, Benli,Pan, Yongjie,&Li, Xia.(2021).Spatiotemporal distribution and variation of wind erosion over the Tibetan Plateau based on a coupled land-surface wind-erosion model.AEOLIAN RESEARCH,50.
MLA	Jiang, Yingsha,et al."Spatiotemporal distribution and variation of wind erosion over the Tibetan Plateau based on a coupled land-surface wind-erosion model".AEOLIAN RESEARCH 50(2021).