2019
DOI: 10.1016/j.catena.2019.104082
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Evaluation and application of a SWAT model to assess the climate change impact on the hydrology of the Himalayan River Basin

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Cited by 227 publications
(123 citation statements)
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“…Nepal (2016) projected the water availability of the Dudh Koshi River basin (about 3710 km 2 ), a sub-basin of the Koshi River basin, considering the IPCC-SRES A1B scenario, using dynamically downscaled precipitation and temperature data with a spatial resolution of 50 km × 50 km. Likewise, Bhatta et al (2019) assessed climate change impacts on water availability in the Tamor River basin (about 4380 km 2 ), also a sub-basin of the Koshi River basin, using 50 km × 50 km spatial resolution data and RCPs 4.5 and 8.5. Bharati et al (2019) investigated water availability in the Koshi River basin (about 87,300 km 2 ) using weather data at a spatial resolution of 25 km × 25 km and RCPs 4.5 and 8.5.…”
Section: Introductionmentioning
confidence: 99%
“…Nepal (2016) projected the water availability of the Dudh Koshi River basin (about 3710 km 2 ), a sub-basin of the Koshi River basin, considering the IPCC-SRES A1B scenario, using dynamically downscaled precipitation and temperature data with a spatial resolution of 50 km × 50 km. Likewise, Bhatta et al (2019) assessed climate change impacts on water availability in the Tamor River basin (about 4380 km 2 ), also a sub-basin of the Koshi River basin, using 50 km × 50 km spatial resolution data and RCPs 4.5 and 8.5. Bharati et al (2019) investigated water availability in the Koshi River basin (about 87,300 km 2 ) using weather data at a spatial resolution of 25 km × 25 km and RCPs 4.5 and 8.5.…”
Section: Introductionmentioning
confidence: 99%
“…Some of the consequences of climate change, such as an increase in extreme floods and droughts, maybe unavoidable [3]. Therefore, quantifying the climate change impact on water availability is essential to watershed management as well as to the formulation of adaptation strategies to mitigate its negative impacts [4].…”
Section: Introductionmentioning
confidence: 99%
“…The rainy season output intensity of nitrogen and phosphorus pollutants was much higher than that in the dry season, mainly due to the severe mineralization process of litter in the rainy season. Therefore, in the rainy season, the polymorphism of nitrogen and phosphorus in the litter is more easily washed into the river by rainfall [43,44], and the rainy season also has more abundant precipitation than the dry season, resulting in more surface runoff [45]. Gu, et al [46] and Wilson [47] also proved that the phosphorus dynamics in soil was strongly influenced by climatic factors.…”
Section: The Response Of Forest Characteristics To Tn and Tpmentioning
confidence: 99%