Goodarzi Mustafa, Abedi-Koupai Jahangir, Heidarpour Manouchehr
Department of Water Engineering, College of Agriculture, Isfahan University of Technology, Isfahan, Iran.
Ground Water. 2019 Mar;57(2):259-268. doi: 10.1111/gwat.12771. Epub 2018 May 11.
In this study, the impacts of climate change on crop water requirements and irrigation water requirements on the regional cropping pattern were evaluated using two climate change scenarios and combinations of 20 GCM models. Different models including CROPWAT, MODFLOW, and statistical models were used to evaluate the climate change impacts. The results showed that in the future period (2017 to 2046) the temperature in all months of the year will increase at all stations. The average annual precipitation decline in Isfahan, Tiran, Flavarjan, and Lenj stations for RCP 4.5 and RCP 8.5 scenarios are 18.6 and 27.6%, 15.2 and 18%, 22.5 and 31.5%, and 10.5 and 12.1%, respectively. The average increase in the evapotranspiration for RCP 4.5 and RCP 8.5 scenarios are about 2.5 and 4.1%, respectively. The irrigation water demands increases considerably and for some crops, on average 18%. Among the existing crops in the cropping pattern, barley, cumin, onion, wheat, and forage crops are more sensitive and their water demand will increase significantly. Results indicate that climate change could have a significant impact on water resources consumption. By considering irrigation efficiency in the region, climate change impacts will result in about 35 to 50 million m /year, over-extraction from the aquifer. This additional exploitation causes an extra drop of 0.4 to 0.8 m in groundwater table per year in the aquifer. Therefore, with regard to the critical condition of the aquifer, management and preventive measures to deal with climate change in the future is absolutely necessary.
在本研究中,利用两种气候变化情景和20个全球气候模型(GCM)的组合,评估了气候变化对区域种植模式下作物需水量和灌溉需水量的影响。使用了包括CROPWAT、MODFLOW和统计模型在内的不同模型来评估气候变化的影响。结果表明,在未来时期(2017年至2046年),所有站点全年各月的气温都将升高。在RCP 4.5和RCP 8.5情景下,伊斯法罕、蒂兰、弗拉瓦尔詹和伦吉站点的年平均降水量下降分别为18.6%和27.6%、15.2%和18%、22.5%和31.5%、10.5%和12.1%。在RCP 4.5和RCP 8.5情景下,蒸散量的平均增幅分别约为2.5%和4.1%。灌溉需水量大幅增加,一些作物的灌溉需水量平均增加18%。在种植模式中的现有作物中,大麦、孜然、洋葱、小麦和饲料作物更为敏感,其需水量将显著增加。结果表明,气候变化可能对水资源消耗产生重大影响。考虑到该地区的灌溉效率,气候变化的影响将导致每年从含水层超采约3500万至5000万立方米。这种额外的开采导致含水层地下水位每年额外下降0.4至0.8米。因此,鉴于含水层的危急状况,未来应对气候变化的管理和预防措施绝对必要。