NCAS Climate and Department of Meteorology, University of Reading, Reading, UK.
Philos Trans A Math Phys Eng Sci. 2010 Nov 28;368(1931):5173-84. doi: 10.1098/rsta.2010.0199.
Anthropogenic changes in precipitation pose a serious threat to society-particularly in regions such as the Middle East that already face serious water shortages. However, climate model projections of regional precipitation remain highly uncertain. Moreover, standard resolution climate models have particular difficulty representing precipitation in the Middle East, which is modulated by complex topography, inland water bodies and proximity to the Mediterranean Sea. Here we compare precipitation changes over the twenty-first century against both millennial variability during the Holocene and interannual variability in the present day. In order to assess the climate model and to make consistent comparisons, this study uses new regional climate model simulations of the past, present and future in conjunction with proxy and historical observations. We show that the pattern of precipitation change within Europe and the Middle East projected by the end of the twenty-first century has some similarities to that which occurred during the Holocene. In both cases, a poleward shift of the North Atlantic storm track and a weakening of the Mediterranean storm track appear to cause decreased winter rainfall in southern Europe and the Middle East and increased rainfall further north. In contrast, on an interannual time scale, anomalously dry seasons in the Middle East are associated with a strengthening and focusing of the storm track in the north Mediterranean and hence wet conditions throughout southern Europe.
人为因素引起的降水变化对社会构成了严重威胁——特别是在中东等已经面临严重水资源短缺的地区。然而,气候模式对区域降水的预测仍然存在很大的不确定性。此外,标准分辨率气候模式在代表中东降水方面特别困难,因为中东的降水受到复杂地形、内陆水体和靠近地中海的影响。在这里,我们将二十一世纪的降水变化与全新世的千年变率和现代的年际变率进行了比较。为了评估气候模型并进行一致的比较,本研究使用了过去、现在和未来的新区域气候模型模拟,并结合代理和历史观测结果。我们表明,二十一世纪末预计欧洲和中东的降水变化模式与全新世期间发生的变化模式有一些相似之处。在这两种情况下,北大西洋风暴轨迹的北移和地中海风暴轨迹的减弱似乎导致了南欧和中东冬季降雨量的减少,以及更北地区降雨量的增加。相比之下,在年际时间尺度上,中东异常干燥的季节与北地中海风暴轨迹的加强和集中有关,从而导致南欧整个地区的潮湿条件。