School of Human and Environmental Sciences, University of Reading, 2 Earley Gate, Whiteknights, Reading, UK.
Philos Trans A Math Phys Eng Sci. 2010 Nov 28;368(1931):5151-72. doi: 10.1098/rsta.2010.0207.
This paper is concerned with the quantification of the likely effect of anthropogenic climate change on the water resources of Jordan by the end of the twenty-first century. Specifically, a suite of hydrological models are used in conjunction with modelled outcomes from a regional climate model, HadRM3, and a weather generator to determine how future flows in the upper River Jordan and in the Wadi Faynan may change. The results indicate that groundwater will play an important role in the water security of the country as irrigation demands increase. Given future projections of reduced winter rainfall and increased near-surface air temperatures, the already low groundwater recharge will decrease further. Interestingly, the modelled discharge at the Wadi Faynan indicates that extreme flood flows will increase in magnitude, despite a decrease in the mean annual rainfall. Simulations projected no increase in flood magnitude in the upper River Jordan. Discussion focuses on the utility of the modelling framework, the problems of making quantitative forecasts and the implications of reduced water availability in Jordan.
本文旨在量化人为气候变化对 21 世纪末约旦水资源可能产生的影响。具体来说,本研究使用了一系列水文模型,结合区域气候模型 HadRM3 的模拟结果和天气生成器,以确定上约旦河和瓦迪法耶南未来的流量可能会发生怎样的变化。研究结果表明,随着灌溉需求的增加,地下水将在该国的水安全中发挥重要作用。考虑到未来冬季降雨量减少和近地表气温升高的预测,已经很低的地下水补给量将进一步减少。有趣的是,模拟的瓦迪法耶南流量表明,尽管年平均降雨量减少,但极端洪水流量的规模将进一步增加。模拟预测在上约旦河的洪水规模不会增加。讨论集中在建模框架的实用性、定量预测的问题以及约旦水资源减少的影响。