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Assessing Climate Change Impact on Water Balance Components of a River Basin Using SWAT Model

机译:利用SWAT模型评估气候变化对流域水平衡成分的影响

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Climate change is one of the most important global environmental challenges, which affects the entire earth system in terms of negative impacts on food production, water supply, health, livelihood, energy, etc. The intent of the present study was to assess the impact of climate change on the water balance components of a data-starved Upper Baitarani River basin of Eastern India using ArcSWAT model. The ArcSWAT model was calibrated using SUFI-2 technique. The daily observed streamflow data from 1998 to 2003 were employed for calibration and those for 2004–2005 for validation. The calibration results were found to be satisfactory with the Nash-Sutcliffe efficiency (NSE) and mean absolute error (MAE) of 0.88 and 9.70 m3/s for the daily time step, respectively. Also, the model was validated successfully for simulating daily streamflow (NSE = 0.80 and MAE = 10.33 m3/s). The calibrated and validated model was then used to evaluate basin response to the anticipated climate changes by the end of the 21st century. Twelve independent as well as twenty eight combined area-specific climatic scenarios were considered in this study to evaluate the impact of climate change on the hydrology of the basin. The analysis of model results for the 12 Independent Climatic Scenarios indicated a reduction in the surface runoff ranging from 2.5 to 11 % by changing the temperature from 1 to 5 °C, whereas the increase in rainfall by 2.5 to 15 % suggested an increase in surface runoff by 6.67 to 43.42 % from the baseline condition. In case of 28 Combined Scenarios compared to the baseline condition, the changes in surface runoff would vary from −4.55 to 37.53 %, the groundwater recharge would change from −8.7 to 23.15 % and the evapotranspiration would increase from 4.05 to 11.88 %. It is concluded that future changes in the climatic condition by the end of the 21st century are most likely to produce significant impacts on the streamflow in the study area. The findings of this study and those of follow-up studies in this direction will be useful for guiding suitable adaptation measures for sustainable water management in the basin in the face of impending climate change.
机译:气候变化是全球最重要的环境挑战之一,它对食品生产,供水,健康,生计,能源等方面的负面影响影响了整个地球系统。本研究的目的是评估气候变化的影响。使用ArcSWAT模型的印度东部数据匮乏的上塔拉塔拉尼河流域水平衡要素上的气候变化。使用SUFI-2技术对ArcSWAT模型进行了校准。使用1998年至2003年的每日观测流量数据进行校准,并使用2004-2005年的每日观测数据进行验证。每天时间步长的纳什-萨特克利夫效率(NSE)和平均绝对误差(MAE)分别为0.88和9.70 m3 / s,发现校准结果令人满意。此外,该模型已成功验证以模拟日流量(NSE = 0.80和MAE = 10.33m3 / s)。然后,使用经过校准和验证的模型来评估流域对21世纪末预期气候变化的响应。在这项研究中考虑了十二个独立的以及二十八个组合的特定地区气候情景,以评估气候变化对流域水文学的影响。对12种独立气候情景的模型结果分析表明,通过将温度从1°C更改为5°C,地表径流减少了2.5%至11%,而降雨增加了2.5%至15%,表明地表径流增加了与基准条件相比,径流减少了6.67%至43.42%。与基准条件相比,如果有28种组合方案,地表径流的变化将从-4.55%改变到37.53%,地下水补给量将从−8.7改变到23.15%,蒸散量将从4.05%增加到11.88%。结论是,到21世纪末,未来气候条件的变化最有可能对研究区的水流产生重大影响。这项研究的结果和后续研究的结果将有助于指导面临气候变化的流域可持续水资源管理的适当适应措施。

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