Lelieveld J, Hadjinicolaou P, Kostopoulou E, Chenoweth J, El Maayar M, Giannakopoulos C, Hannides C, Lange M A, Tanarhte M, Tyrlis E, Xoplaki E
The Cyprus Institute, P.O. Box 27456, 1645 Nicosia, Cyprus ; Max Planck Institute for Chemistry, 55020 Mainz, Germany ; King Saud University, Riyadh, 11451 Saudi Arabia.
The Cyprus Institute, P.O. Box 27456, 1645 Nicosia, Cyprus.
Clim Change. 2012;114(3-4):667-687. doi: 10.1007/s10584-012-0418-4. Epub 2012 Mar 7.
The Eastern Mediterranean and the Middle East (EMME) are likely to be greatly affected by climate change, associated with increases in the frequency and intensity of droughts and hot weather conditions. Since the region is diverse and extreme climate conditions already common, the impacts will be disproportional. We have analyzed long-term meteorological datasets along with regional climate model projections for the 21st century, based on the intermediate IPCC SRES scenario A1B. This suggests a continual, gradual and relatively strong warming of about 3.5-7°C between the 1961-1990 reference period and the period 2070-2099. Daytime maximum temperatures appear to increase most rapidly in the northern part of the region, i.e. the Balkan Peninsula and Turkey. Hot summer conditions that rarely occurred in the reference period may become the norm by the middle and the end of the 21st century. Projected precipitation changes are quite variable. Annual precipitation is expected to decrease in the southern Europe - Turkey region and the Levant, whereas in the Arabian Gulf area it may increase. In the former region rainfall is actually expected to increase in winter, while decreasing in spring and summer, with a substantial increase of the number of days without rainfall. Anticipated regional impacts of climate change include heat stress, associated with poor air quality in the urban environment, and increasing scarcity of fresh water in the Levant.
东地中海和中东地区(EMME)很可能受到气候变化的严重影响,这与干旱和炎热天气状况的频率及强度增加有关。由于该地区情况多样,极端气候条件已然常见,其影响将是不均衡的。我们基于政府间气候变化专门委员会(IPCC)特别报告排放情景(SRES)A1B中等方案,分析了长期气象数据集以及21世纪的区域气候模型预测。这表明在1961 - 1990年参考期与2070 - 2099年期间,气温将持续、逐渐且相对强劲地上升约3.5 - 7°C。该地区北部,即巴尔干半岛和土耳其,白天最高气温似乎上升最为迅速。参考期内极少出现的炎热夏季状况,到21世纪中叶及末期可能会成为常态。预计降水变化差异很大。南欧 - 土耳其地区和黎凡特地区的年降水量预计将减少,而阿拉伯湾地区的降水量可能增加。在前一地区,实际上预计冬季降水量会增加,而春季和夏季降水量会减少,无降雨天数将大幅增加。预计气候变化对该地区的影响包括热应激,这与城市环境中空气质量差有关,以及黎凡特地区淡水日益短缺。