Downscaling simulation of groundwater storage in the Tarim River basin in northwest China based on GRACE data

2021 ◽  
pp. 103042
Author(s):  
Jingping Zuo ◽  
Jianhua Xu ◽  
Yaning Chen ◽  
Weihong Li
Keyword(s):  
River Basin ◽  
Northwest China ◽  
Tarim River ◽  
Tarim River Basin ◽  
Groundwater Storage ◽  
The Tarim River ◽  
Grace Data ◽  
The Tarim River Basin

How is the risk of hydrological drought in the Tarim River Basin, Northwest China?

2019 ◽  
Vol 693 ◽  
pp. 133555 ◽  
Author(s):  
Peng Yang ◽  
Jun Xia ◽  
Yongyong Zhang ◽  
Chesheng Zhan ◽  
Shangxin Sun
Keyword(s):  
River Basin ◽  
Northwest China ◽  
Hydrological Drought ◽  
Tarim River ◽  
Tarim River Basin ◽  
The Tarim River ◽  
The Tarim River Basin

scholarly journals Estimation of Actual Evapotranspiration by the Complementary Theory-Based Advection–Aridity Model in the Tarim River Basin, China

2018 ◽  
Vol 19 (2) ◽  
pp. 289-303 ◽  
Author(s):  
Dongnan Jian ◽  
Xiucang Li ◽  
Hemin Sun ◽  
Hui Tao ◽  
Tong Jiang ◽  
...  
Keyword(s):  
River Basin ◽  
Potential Evapotranspiration ◽  
Temporal Trends ◽  
Northwest China ◽  
Actual Evapotranspiration ◽  
Tarim River ◽  
Tarim River Basin ◽  
Complementary Relationship ◽  
The Tarim River ◽  
The Tarim River Basin

AbstractIn this study, the complementary relationship between actual evapotranspiration (ETa) and potential evapotranspiration (ETp) was verified in the Tarim River basin (TRB) in northwest China. The advection–aridity (AA) model that is based on the complementary relationship (CR) was used to calculate ETa. Spatial and temporal trends in the estimated annual ETa and the factors that influenced ETa were investigated. The multiyear average ETa in the TRB for the period from 1961 to 2014 was 178.5 mm. There was an overall significant increasing trend (at a rate of 10.6 mm decade−1) in ETa from 1961 to 2014; ETa increased at a rate of 22.9 mm decade−1 from 1961 to 1996 and decreased at a rate of 33.9 mm decade−1 from 1996 to 2014. Seasonally, ETa was strongest in summer, followed by spring and autumn. The spatial distributions of the annual and seasonal ETa were mostly consistent, with higher ETa values in the northeast, northwest, and southwest of the TRB, and lower ETa values in the mostly desert lands in the central and southeastern areas. While the energy budget (indicated by net radiation Rn) had little influence on ETa over time, the advection budget (indicated by the drying power of the air Ea) played an important role, explainable by Bouchet’s complementary relationship. In the Aksu River basin (ARB), ETa has increased because of an increase in the surface water supply (SWS). The change in ETa between 1996 and 1998 may have been caused by changes in the SWS and the advection budget during the same time period.

scholarly journals Glacier retreat as a result of climate warming and increased precipitation in the Tarim river basin, northwest China

2006 ◽  
Vol 43 ◽  
pp. 91-96 ◽  
Author(s):  
Shiyin Liu ◽  
Yongjian Ding ◽  
Donghui Shangguan ◽  
Yong Zhang ◽  
Jing Li ◽  
...  
Keyword(s):  
River Basin ◽  
Northwest China ◽  
Tarim River ◽  
Tarim River Basin ◽  
Positive Anomaly ◽  
Stream Discharge ◽  
The Tarim River ◽  
High Resolution Satellite Images ◽  
The Tarim River Basin ◽  
The Impact

AbstractThe Tarim river basin, a river system formed by the convergence of nine tributaries, is the most heavily glacierized watershed in arid northwest China. In the basin, there are 11 665 glaciers with a total area of 19 878 km2 and a volume of 2313 km3. Glaciers in the basin play a significant role in the water resource system. It is estimated that they provide about 133 x 108 m3 of meltwater annually, contributing 39% of the total river runoff. Under the influence of global warming, northwest China has experienced a generally warmer and drier climate since the mid-19th century. However, a so-called ‘warm and wet transition’ has occurred since the late 1980s, evidenced by an increase in both precipitation and stream discharge in the Xinjiang Autonomous Region and neighboring regions. This paper describes how glaciers in the Tarim river basin have responded to such warming and increased precipitation, and the impact of these glacier changes. We analyzed the variations of more than 3000 glaciers since the 1960s using topographical maps, high-resolution satellite images and aerial photographs of the river basin. Our results indicate that glaciers in the basin have been mostly in retreat in the past 40 years, and ice wastage has significantly influenced water resources in the Tarim river basin. Estimation by a degree-day meltwater model shows the positive anomaly in stream runoff of the Tailan river can be partly attributed to the increase in glacier runoff (amounting to one-third of the stream discharge), and a rough estimation using observed average ablation on the termini of 15 glaciers in China verifies that the mass loss calculated by a glacier area-volume relation is reasonable.

Development of Environmental Information System for the Tarim River Basin

2010 ◽  
Vol 26 (3) ◽  
pp. 347-353
Author(s):  
Jian-kang SHI ◽  
An-ming BAO ◽  
Hai-long LIU ◽  
Xian-wei FENG ◽  
Wei-sheng WANG ◽  
...  
Keyword(s):  
Information System ◽  
River Basin ◽  
Environmental Information ◽  
Tarim River ◽  
Tarim River Basin ◽  
The Tarim River ◽  
Environmental Information System ◽  
The Tarim River Basin

scholarly journals Temporal clustering of floods and impacts of climate indices in the Tarim River basin, China

2016 ◽  
Vol 147 ◽  
pp. 12-24 ◽  
Author(s):  
Xihui Gu ◽  
Qiang Zhang ◽  
Vijay P Singh ◽  
Yongqin David Chen ◽  
Peijun Shi
Keyword(s):  
River Basin ◽  
Tarim River ◽  
Climate Indices ◽  
Tarim River Basin ◽  
Temporal Clustering ◽  
The Tarim River ◽  
The Tarim River Basin
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