关于人类活动引起的气候变化的知识状况和不确定性

Jean-Claude Duplessy
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引用次数: 14

摘要

20世纪,地面平均气温上升了0.6±0.2°C,气温最高的时期出现在1980年以后。这一年的气温明显高于上个千年。与此同时,降雨和干旱、寒流和热浪的频率发生了变化,山地冰川退缩,海平面上升了~ 10厘米。这种变暖至少部分是由人类活动引起的,并将在未来几十年持续下去。其幅度将取决于温室气体和硫酸盐气溶胶排放的速率,即取决于能量情景。悬而未决的科学不确定性包括云的变化以及气候系统的物理部分与生物地球化学循环和生物圈之间的相互作用。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
État des connaissances et incertitudes sur le changement climatique induit par les activités humaines

During the 20th century, the mean temperature of the air at the ground level has increased by 0.6±0.2 °C and the warmest air temperatures occurred after 1980. These were significantly warmer than those of the last millennium. Simultaneously, rain and drought, cold and heat wave frequencies have changed, mountain glaciers retreated and the sea-level increased by ∼10 cm. This warming was at least in part induced by human activities and will continue during the next decades. Its amplitude will depend on the rate of greenhouse gas and sulphate aerosols emissions, i.e. on energetic scenarios. Pending scientific uncertainties include cloud variations and interactions between the physical parts of the climate system and the biogeochemical cycles and the biosphere.

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