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Modelling future no-analogue climate distributions: A world-wide phytoclimatic niche-based survey

机译:模拟未来的无模拟气候分布:基于植物生态位的全球调查

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摘要

By the end of the 21st century in some zones the accelerating climate change affecting this planet will create factorial combinations unknown at this time, which will give rise to climates unlike the present ones. This study presents a numerical and cartographic evaluation of these no-analogue climatic zones, whose consequences for existing ecosystems are quite unpredictable, using a method based on the convex hull in a climate hyperspace and 12 future climate projections for 2080. The percentage of the world surface that will foreseeably be occupied by no-analogue climates by 2080 ranges between 3.5% and 17.5%. The bulk of the no-analogue surface area will foreseeably be located in the Northern hemisphere (>80%), with more elevated risk in tropical and subtropical latitudes between 10 degrees latitude South and 30 degrees latitude North, preferentially in Africa, South America, the Arabian Peninsula, the Indian Peninsula, the Northwest of the Gulf of Mexico, Eastern China and Polynesia. Mean temperatures would appear to be the variables most influencing the process. This affects 32 of the 34 hotspots defined for the planet, especially tropical forests in South America and Asia. 6.8% of these conservation-critical surfaces are predicted as no-analogue areas. Population density is greater in the areas that will probably develop no-analogue climates in the future than in those that will not.
机译:到21世纪末,在某些地区,影响该星球的加速气候变化将产生此时未知的阶乘组合,这将引发与当前气候不同的气候。这项研究使用基于凸壳在气候超空间中的方法以及2080年的12个未来气候预测,对这些无模拟气候区进行了数值和制图评估,这些模拟区对现有生态系统的后果是不可预测的。可以预见,到2080年,无模拟气候所占据的地表范围将在3.5%至17.5%之间。可以预见,大部分非模拟区域都将位于北半球(> 80%),在南纬10度到北纬30度之间的热带和亚热带纬度地区(尤其是在非洲,南美,阿拉伯半岛,印度半岛,墨西哥湾西北部,中国东部和波利尼西亚。平均温度似乎是最影响过程的变量。这影响到为地球定义的34个热点中的32个,特别是南美和亚洲的热带森林。这些保护至关重要的表面的6.8%被预测为无模拟区域。未来可能会形成无模拟气候的地区的人口密度要比那些不会出现模拟气候的地区更高。

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