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Assessing climate change impacts on water resources and crop yield: a case study of Varamin plain basin, Iran

机译:评估气候变化对水资源和作物产量的影响:以伊朗瓦拉明平原盆地为例

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This research evaluated climate change impacts on water resources using soil and water assessment tool (SWAT) models under representative concentration pathway scenarios (RCP 2.6, RCP 6, RCP 8.5). First, drought intensity was calculated using the standardized precipitation index (SPI) for the period 1987-2016. Then, the coefficients of precipitation as well as minimum and maximum temperature changes were simulated as SWAT model inputs. The results revealed that temperature will rise in future periods and the precipitation rate will be changed consequently. Then, changes in runoff during periods of 2011-2040, 2041-2070, and 2071-2100 were simulated by introducing downscaled results to SWAT model. The model was calibrated and validated by SWAT calibration and uncertainty procedures (SWAT-CUP). Nash-Sutcliffe (NS) coefficients (0.57 and 0.54) and R-2 determination coefficients (0.65 and 0.63) were obtained for calibration and validation periods, respectively. The results showed that runoff will rise in fall and spring while it will drop in winter and summer throughout future periods under all three scenarios. Such seasonal shifts in runoff levels result from climate change consequences in the forms of temperature rise, snowmelt, altered precipitation pattern, etc. Future-period evapotranspiration will rise under all three scenarios with a maximum increase in the period 2070-2100 under RCP 8.5 scenario. Additionally, rainfed crop yields will decline without considerable changes in irrigated and horticultural crop yields.
机译:这项研究在代表性浓度路径情景下(RCP 2.6,RCP 6,RCP 8.5)使用土壤和水评估工具(SWAT)模型评估了气候变化对水资源的影响。首先,使用标准降水指数(SPI)计算1987-2016年的干旱强度。然后,将降水系数以及最小和最大温度变化模拟为SWAT模型输入。结果表明,未来气温将升高,降水率将随之改变。然后,通过将缩水结果引入SWAT模型,模拟了2011-2040年,2041-2070年和2071-2100年期间的径流量变化。通过SWAT校准和不确定性程序(SWAT-CUP)对模型进行校准和验证。分别在校准和验证期间获得了纳什-舒克利夫(NS)系数(0.57和0.54)和R-2测定系数(0.65和0.63)。结果表明,在所有这三种情况下,径流都将在秋季和春季上升,而在整个冬季以后的冬季和夏季将下降。径流水平的这种季节性变化是由气候变化导致的,例如温度上升,融雪,降雨模式改变等。在这三种情况下,未来时期的蒸散量都将增加,在RCP 8.5情况下,2070-2100年期间的最大蒸发量将增加。 。此外,雨养作物单产将下降,而灌溉和园艺作物单产不会发生重大变化。

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