Estimation of the ecological water requirement for natural vegetation in the Ergune River basin in Northeastern China from 2001 to 2014

2018 ◽  
Vol 92 ◽  
pp. 141-150 ◽  
Author(s):  
Dengkai Chi ◽  
Hong Wang ◽  
Xiaobing Li ◽  
Honghai Liu ◽  
Xiaohui Li
2013 ◽  
Vol 864-867 ◽  
pp. 2595-2598
Author(s):  
Qin Li ◽  
An Ming Bao ◽  
Xi Chen ◽  
Hai Jun Sun ◽  
Gui Bin Pang

Data of natural vegetation coverage in the Central Asia and Xinjiang of Chinese in 2005 was obtained by statistical analysis on MODIS Land cover data, then the ecological water requirement (EWR) of natural vegetation was brought out which based on the evapotranspirtation (ET) retrieval using SEBS model and natural vegetation areas. Results showed that the total EWR of wood land and grass land during the 2005 growing season was 70.10×108m3 and 3251.91×108m3,respectively. It is applicable for reference in the project of regenerating ecology and rationally redistributing water resources in arid areas.


2020 ◽  
Vol 41 (1) ◽  
pp. 423-438 ◽  
Author(s):  
Keyuan Zhong ◽  
Fenli Zheng ◽  
Xunchang Zhang ◽  
Chao Qin ◽  
Ximeng Xu ◽  
...  

2019 ◽  
Vol 46 (3) ◽  
pp. 176
Author(s):  
Camila Calazans Da Silva Luz ◽  
Alexander Webber Perlandim Ramos ◽  
Gessica De Jesus Oliveira Silva

The disorderly use of land is currently one of the main causes of environmental problems. From this perspective, the objective of this study was to determine the natural and environmental vulnerability of the Jauru river basin in the Brazilian state of Mato Grosso. This goal was made from the perspective that the results generated contribute to environmental planning and management, considering that the Jauru river is tributary of the Paraguay river, responsible for the flooding of the Pantanal plain and, that possible impacts caused by the basin may compromise the dynamic equilibrium of the Pantanal's flood pulse. The model of assessment of natural and environmental vulnerability was adopted, with the identification of the following environmental characteristics: geology, slope, agricultural aptitude and vegetation cover and land use. Data were related through Geographic Information Systems to generate natural and environmental vulnerability maps. It was verified, through the data obtained, that in both vulnerabilities studied there was a predominance of the middle class, mainly resulting from the presence of fragile soils. Also, the predominance of the classes of agricultural aptitude found in the basin, as well as the suppression of the natural vegetation to expand the pasture areas. It was concluded that the areas covered by natural vegetation and/or pastures, in the Jauru river basin, present average natural vulnerability and state of medium to high environmental vulnerability, evidencing that livestock, the main activity regional economic development, has been developed in disagreement with environmental aptitude, contributing to the elevation of the state of environmental vulnerability in the basin.


2012 ◽  
Vol 43 (1-2) ◽  
pp. 73-90 ◽  
Author(s):  
Fei Yuan ◽  
Liliang Ren ◽  
Zhongbo Yu ◽  
Yonghua Zhu ◽  
Jing Xu ◽  
...  

Vegetation and land-surface hydrology are intrinsically linked under long-term climate change. This paper aims to evaluate the dynamics of potential natural vegetation arising from 21st century climate change and its possible impact on the water budget of the Hanjiang River basin in China. Based on predictions of the Intergovernmental Panel on Climate Change Special Report on Emissions Scenarios (IPCC-SRES) A1 scenario from the PRECIS (Providing Regional Climates for Impact Studies) regional climate model, changes in plant functional types (PFTs) and leaf area index (LAI) were simulated via the Lund-Potsdam-Jena dynamic global vegetation model. Subsequently, predicted PFTs and LAIs were employed in the Xinanjiang vegetation-hydrology model for rainfall–runoff simulations. Results reveal that future long-term changes in precipitation, air temperature and atmospheric CO2 concentration would remarkably affect the spatiotemporal distribution of PFTs and LAIs. These climate-driven vegetation changes would further influence regional water balance. With the decrease in forest cover in the 21st century, plant transpiration and evaporative loss of intercepted canopy water will tend to fall while soil evaporation may rise considerably. As a result, total evapotranspiration may increase moderately with a slight increase in annual runoff depth. This indicates that, for long-term hydrological prediction, climate-induced changes in terrestrial vegetation cannot be neglected as the terrestrial biosphere plays an important role in land-surface hydrological responses.


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