Mu'tah University, Karak, Jordan.
Environ Monit Assess. 2024 Sep 25;196(10):979. doi: 10.1007/s10661-024-13139-3.
Precipitation partitioning in arid and semiarid environments is not well understood due to scanty precipitation, its temporal distribution, and the lack/absence of adequate measurements of the hydrometeorological components. Simulation methods have the potential to bridge the data gap, thereby providing a window to estimate the water balance components. The present investigation evaluates the water balance components of a typical watershed situated in the southeastern Mediterranean for the period 1979 through 2019 using daily meteorological data and a grid spacing of 250 m. Generated runoff results were commensurate with corresponding values obtained using the SWAT model. Computed groundwater recharge is also compatible with recharge values calculated using the chloride mass balance method. Results show that average runoff and groundwater recharge for the entire period was ⁓24 mm a and 19 mm a, giving a precipitation ratio of 9.5% and 7.5%, respectively. Substantial interannual variability in the water balance components was observed during the study period which reflected the significant precipitation fluctuations typifying the Eastern Mediterranean. Results show that the period extending from 1998/1999 through 2018/2019 witnessed an 18% drop in annual precipitation, while surface runoff and groundwater recharge experienced a reduction of ⁓34% and ⁓67%, respectively. Although groundwater recharge is a complex function of numerous meteorological and geological factors, the NDVI can provide an excellent indicator of groundwater recharge in marginal Mediterranean environments. This is highly beneficial in areas where climate records are scanty or absent. The presented results emphasize the significant impacts of global warming and aridification on the future availability of water resources in the semiarid marginal climates in the Eastern Mediterranean and point out clearly that water resources in this area will become scarcer, leading to multiple security threats at national and regional levels.
由于降水量稀少、时间分布不均以及缺乏对水文气象要素的充分测量,干旱和半干旱环境中的降水分配情况还不太清楚。模拟方法有可能弥补数据空白,从而为估算水量平衡分量提供一个窗口。本研究使用逐日气象数据和 250m 的网格间距,评估了东南地中海一个典型流域的水量平衡分量,时间范围为 1979 年至 2019 年。生成的径流量结果与使用 SWAT 模型获得的相应值相符。计算得出的地下水补给量也与使用氯离子质量平衡法计算得出的补给量相符。结果表明,整个时期的平均径流量和地下水补给量分别为 ⁓24mm a 和 19mm a,降水比例分别为 9.5%和 7.5%。在研究期间,水量平衡分量表现出较大的年际变化,这反映了东地中海典型的显著降水波动。结果表明,1998/1999 年至 2018/2019 年期间,年降水量下降了 18%,而地表径流量和地下水补给量分别减少了 ⁓34%和 ⁓67%。尽管地下水补给是众多气象和地质因素的复杂函数,但 NDVI 可以很好地指示边缘地中海环境中的地下水补给。这在气候记录稀少或缺失的地区非常有益。所呈现的结果强调了全球变暖与干旱化对半干旱边缘地中海气候未来水资源可利用性的重大影响,并明确指出,该地区的水资源将变得更加稀缺,从而在国家和地区层面引发多种安全威胁。