首页> 外文期刊>Journal of Hydrology >Climate change impacts on water resources in the Upper Blue Nile (Abay) River Basin, Ethiopia
【24h】

Climate change impacts on water resources in the Upper Blue Nile (Abay) River Basin, Ethiopia

机译:气候变化对埃塞俄比亚的上蓝尼罗河(Abay)河流域水资源的影响

获取原文
获取原文并翻译 | 示例
           

摘要

This study assesses the impact of climate change on water resources in the Upper Blue Nile (Abay) River Basin using a regional climate model (RCM), COSMO Climate Limited-area Model (CCLM), coupled with a hydrological model, Soil and Water Assessment Tool (SWAT). The SWAT model was calibrated and validated using measured streamflow data from four gauging stations. Climate change projections showed increases in mean annual temperature and decrease in precipitation in most parts of the Basin. Such changes are expected to affect the hydrologic regime of the Basin; these were assessed by running the SWAT model with the past (1981-2010) and future (2010-2039, 2040-2069 and 2070-2099) climate scenarios. The results show an increase of potential evapotranspiration (PET) by up to 27% by the end of the 21st century under RCP8.5 compared to the baseline period. Surface runoff is projected to increase by up to 14%. However, the increase in surface runoff could not increase the total water yield of the Basin. Instead, the total water yield of the Basin is estimated to decrease by -1.7 to -6.5% and -10.7 to -22.7%, for simulations forced by RCP4.5 and RCP8.5 scenarios, respectively. By the end of the 21st century, the contribution of baseflow to the total water yield of the Basin is also projected to decline to 11.4% from 41.3% during the baseline period. The decrease in baseflow partly explains the decline in the total water yield of the Basin. Such changes in the hydrologic balance will have significant implications for water management in the Basin.
机译:本研究使用区域气候模型(RCM)、COSMO气候有限区模型(CCLM)以及水文模型、土壤和水评估工具(SWAT),评估了气候变化对上蓝尼罗河(Abay)流域水资源的影响。使用四个测量站的实测流量数据对SWAT模型进行了校准和验证。气候变化预测显示,该盆地大部分地区的年平均气温上升,降水量减少。预计这些变化将影响流域的水文状况;通过在过去(1981-2010年)和未来(2010-2039年、2040-2069年和2070-2099年)气候情景下运行SWAT模型来评估这些影响。结果表明,到21世纪末,在RCP8条件下,潜在蒸散量(PET)增加了27%。5与基线期相比。地表径流预计将增加14%。然而,地表径流的增加并不能增加流域的总产水量。相反,根据RCP4进行的模拟,预计该流域的总产水量将减少-1.7%至-6.5%,减少-10.7%至-22.7%。5和RCP8。分别有5种情况。到21世纪末,基流对流域总产水量的贡献预计也将从基线期间的41.3%降至11.4%。基流的减少部分解释了盆地总产水量的下降。水文平衡的这种变化将对流域的水资源管理产生重大影响。

著录项

相似文献

  • 外文文献
  • 中文文献
  • 专利
获取原文

客服邮箱:kefu@zhangqiaokeyan.com

京公网安备:11010802029741号 ICP备案号:京ICP备15016152号-6 六维联合信息科技 (北京) 有限公司©版权所有
  • 客服微信

  • 服务号