Spatiotemporal soil moisture variations associated with hydro‐meteorological factors over the Yarlung Zangbo River basin in Southeast Tibetan Plateau

2019 ◽  
Vol 40 (1) ◽  
pp. 188-206 ◽  
Author(s):  
Xueying Li ◽  
Liu Liu ◽  
Hao Li ◽  
Shuping Wang ◽  
Jingxia Heng
Keyword(s):  
Soil Moisture ◽  
Tibetan Plateau ◽  
River Basin ◽  
Meteorological Factors ◽  
Yarlung Zangbo River ◽  
Southeast Tibetan Plateau

Characteristics of recent temperate glacier fluctuations in the Parlung Zangbo River basin, southeast Tibetan Plateau

2010 ◽  
Vol 55 (20) ◽  
pp. 2097-2102 ◽  
Author(s):  
Wei Yang ◽  
TanDong Yao ◽  
BaiQing Xu ◽  
LingLong Ma ◽  
ZhiHui Wang ◽  
...  
Keyword(s):  
Tibetan Plateau ◽  
River Basin ◽  
Glacier Fluctuations ◽  
Southeast Tibetan Plateau

scholarly journals Near-surface wind environment in the Yarlung Zangbo River basin, southern Tibetan Plateau

2021 ◽  
Author(s):  
Junhuai Yang ◽  
Dunsheng Xia ◽  
Shuyuan Wang ◽  
Weidong Wang ◽  
Xingyue Ma ◽  
...  
Keyword(s):  
Tibetan Plateau ◽  
River Basin ◽  
Surface Wind ◽  
Wind Environment ◽  
Near Surface ◽  
Yarlung Zangbo River ◽  
Southern Tibetan Plateau

scholarly journals Elevation-Dependent Vegetation Greening of the Yarlung Zangbo River Basin in the Southern Tibetan Plateau, 1999–2013

2015 ◽  
Vol 7 (12) ◽  
pp. 16672-16687 ◽  
Author(s):  
Haidong Li ◽  
Yingkui Li ◽  
Weishou Shen ◽  
Yanan Li ◽  
Jie Lin ◽  
...  
Keyword(s):  
Tibetan Plateau ◽  
River Basin ◽  
Yarlung Zangbo River ◽  
Southern Tibetan Plateau

scholarly journals Responses of Hydrological Processes under Different Shared Socioeconomic Pathway Scenarios in the Huaihe River Basin, China

Water ◽  
2021 ◽  
Vol 13 (8) ◽  
pp. 1053
Author(s):  
Yuan Yao ◽  
Wei Qu ◽  
Jingxuan Lu ◽  
Hui Cheng ◽  
Zhiguo Pang ◽  
...  
Keyword(s):  
Soil Moisture ◽  
River Basin ◽  
Climate Models ◽  
Global Climate Models ◽  
Hydrological Response ◽  
Huaihe River Basin ◽  
Huaihe River ◽  
Infiltration Capacity ◽  
Change Analysis ◽  
Average Annual Runoff

The Coupled Model Intercomparison Project Phase 6 (CMIP6) provides more scenarios and reliable climate change results for improving the accuracy of future hydrological parameter change analysis. This study uses five CMIP6 global climate models (GCMs) to drive the variable infiltration capacity (VIC) model, and then simulates the hydrological response of the upper and middle Huaihe River Basin (UMHRB) under future shared socioeconomic pathway scenarios (SSPs). The results show that the five-GCM ensemble improves the simulation accuracy compared to a single model. The climate over the UMHRB likely becomes warmer. The general trend of future precipitation is projected to increase, and the increased rates are higher in spring and winter than in summer and autumn. Changes in annual evapotranspiration are basically consistent with precipitation, but seasonal evapotranspiration shows different changes (0–18%). The average annual runoff will increase in a wavelike manner, and the change patterns of runoff follow that of seasonal precipitation. Changes in soil moisture are not obvious, and the annual soil moisture increases slightly. In the intrayear process, soil moisture decreases slightly in autumn. The research results will enhance a more realistic understanding of the future hydrological response of the UMHRB and assist decision-makers in developing watershed flood risk-management measures and water and soil conservation plans.

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