Department of Environmental Earth System Science, Stanford University, Stanford, CA 94305, USA.
Science. 2013 Aug 2;341(6145):486-92. doi: 10.1126/science.1237123.
Terrestrial ecosystems have encountered substantial warming over the past century, with temperatures increasing about twice as rapidly over land as over the oceans. Here, we review the likelihood of continued changes in terrestrial climate, including analyses of the Coupled Model Intercomparison Project global climate model ensemble. Inertia toward continued emissions creates potential 21st-century global warming that is comparable in magnitude to that of the largest global changes in the past 65 million years but is orders of magnitude more rapid. The rate of warming implies a velocity of climate change and required range shifts of up to several kilometers per year, raising the prospect of daunting challenges for ecosystems, especially in the context of extensive land use and degradation, changes in frequency and severity of extreme events, and interactions with other stresses.
在过去的一个世纪里,陆地生态系统已经经历了大幅度的变暖,陆地的升温速度大约是海洋的两倍。在这里,我们回顾了陆地气候持续变化的可能性,包括对耦合模式比较计划全球气候模型集合的分析。持续排放的惯性造成了潜在的 21 世纪全球变暖,其规模与过去 6500 万年中最大的全球变化相当,但速度要快几个数量级。变暖的速度意味着气候变化的速度和所需的气候带移动速度高达每年数公里,这给生态系统带来了严峻的挑战,特别是在广泛的土地利用和退化、极端事件的频率和严重程度变化以及与其他压力相互作用的背景下。