Chan Duo, Wu Qigang
School of Atmospheric Sciences, Nanjing University, 163 Xianlin Ave., Nanjing, Jiangsu, China, 210023.
Sci Rep. 2015 Aug 28;5:13487. doi: 10.1038/srep13487.
Anthropogenic forcings have contributed to global and regional warming in the last few decades and likely affected terrestrial precipitation. Here we examine changes in major Köppen climate classes from gridded observed data and their uncertainties due to internal climate variability using control simulations from Coupled Model Intercomparison Project 5 (CMIP5). About 5.7% of the global total land area has shifted toward warmer and drier climate types from 1950-2010, and significant changes include expansion of arid and high-latitude continental climate zones, shrinkage in polar and midlatitude continental climates, poleward shifts in temperate, continental and polar climates, and increasing average elevation of tropical and polar climates. Using CMIP5 multi-model averaged historical simulations forced by observed anthropogenic and natural, or natural only, forcing components, we find that these changes of climate types since 1950 cannot be explained as natural variations but are driven by anthropogenic factors.
在过去几十年里,人为强迫导致了全球和区域变暖,并可能影响了陆地降水。在此,我们利用耦合模式比较计划第5阶段(CMIP5)的控制模拟,研究了基于网格化观测数据的主要柯本气候类型的变化及其由于内部气候变率导致的不确定性。从1950年至2010年,全球陆地总面积的约5.7%已转向更温暖和更干燥的气候类型,显著变化包括干旱和高纬度大陆气候区的扩张、极地和中纬度大陆气候的收缩、温带、大陆和极地气候的向极移动,以及热带和极地气候平均海拔的增加。利用CMIP5多模式平均历史模拟,这些模拟由观测到的人为和自然强迫成分,或仅自然强迫成分驱动,我们发现自1950年以来这些气候类型的变化不能解释为自然变化,而是由人为因素驱动的。