Modelling hydrologic impacts of semi-dynamic land use in the jedeb 8

Author(s):  
Seleshi Getahun Yalew
Keyword(s):  
Land Use ◽  
2012 ◽  
Vol 601 ◽  
pp. 186-189
Author(s):  
Xiao Hui Lu ◽  
Zhou Jun Li ◽  
Yang Wang

Distributed physically-based models have the predictive capacity to assess the effect of land use changes on groundwater dynamics across a range of scales. MIKESHE, which represents state-of-art of distributed hydrological model, is applied to the Skjern catchment. It is utilized to evaluate hydrologic impacts of land use changes in a watershed. Our overall objective was to quantitatively evaluate the effects of land use changes on watershed hydrology within the 1175 km2 Skjern catchment in Denmark. The results show that the soil is unsaturated and has bigger storage capacity. The groundwater recharge distribution has seasonal characters like the runoff, which mainly concentrated in winter and spring and decreased in summer and autumn.


2000 ◽  
Vol 26 (6) ◽  
pp. 643-658 ◽  
Author(s):  
Budhendra Bhaduri ◽  
Jon Harbor ◽  
Bernie Engel ◽  
Matt Grove

Anthropocene ◽  
2018 ◽  
Vol 22 ◽  
pp. 20-30 ◽  
Author(s):  
Anton Pijl ◽  
Claudia C. Brauer ◽  
Giulia Sofia ◽  
Adriaan J. Teuling ◽  
Paolo Tarolli
Keyword(s):  
Land Use ◽  

Water ◽  
2019 ◽  
Vol 11 (7) ◽  
pp. 1464 ◽  
Author(s):  
Regina Maria Bessa Santos ◽  
Luís Filipe Sanches Fernandes ◽  
Rui Manuel Vitor Cortes ◽  
Fernando António Leal Pacheco

The study area used for this study was the Sabor river basin (located in the Northeast of Portugal), which is composed mostly for agroforestry. The objectives were to analyze the spatiotemporal dynamics of hydrological services that occurred due to land use changes between 1990 and 2008 and to consider two scenarios for the year 2045. The scenarios were, firstly, afforestation projection, proposed by the Regional Plan for Forest Management, and secondly, wildfires that will affect 32% of the basin area. In this work, SWAT (Soil and Water Assessment Tool) was used to simulate the provision of hydrological services, namely water quantity, being calibrated for daily discharge. The calibration and validation showed a good agreement for discharge with coefficients of determination of 0.63 and 0.8 respectively. The land use changes and the afforestation scenario showed decreases in water yield, surface flow, and groundwater flow and increases in evapotranspiration and lateral flow. The wildfire scenario, contrary to the afforestation scenario, showed an increase in surface flow and a decrease in lateral flow. The Land Use and Land Cover (LULC) changes in 2000 and 2006 showed average decreases in the water yield of 91 and 52 mm·year−1, respectively. The decrease in water yield was greater in the afforestation scenario than in the wildfires scenario mainly in winter months. In the afforestation scenario, the large decrease varied between 28 hm3·year−1 in October and 62 hm3·year−1 in January, while in the wildfires scenario, the decrease was somewhat smaller, varying between 15 hm3·year−1 in October and 49 hm3·year−1 in January.


2006 ◽  
Vol 49 (2) ◽  
pp. 423-432 ◽  
Author(s):  
D. D. Bosch ◽  
D. G. Sullivan ◽  
J. M. Sheridan

2005 ◽  
Author(s):  
David D. Bosch ◽  
Dana G. Sullivan ◽  
Joseph M. Sheridan

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