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首页> 外文期刊>Journal of Geophysical Research, D. Atmospheres: JGR >What influence will future solar activity changes over the 21st century have on projected global near-surface temperature changes?
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What influence will future solar activity changes over the 21st century have on projected global near-surface temperature changes?

机译:影响未来的太阳活动变化在21世纪预计全球近地表温度变化?

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During the 20th century, solar activity increased in magnitude to a so-called grand maximum. It is probable that this high level of solar activity is at or near its end.It is of great interest whether any future reduction in solar activity could have a significant impact on climate that could partially offset the projected anthropogenic warming. Observations and reconstructions of solar activity over the last 9000 years are used as a constraint on possible future variations to produce probability distributions of total solar irradiance over the next 100 years. Using this information, with a simple climate model, we present results of the potential implications for future projections of climate on decadal to multidecadal timescales. Using one of the most recent reconstructions of historic total solar irradiance, the likely reduction in the warming by 2100 is found to be between 0.06 and 0.1 K, a very small fraction of the projected anthropogenic warming. However, if past total solar irradiance variations are larger and climate models substantially underestimate the response to solar variations, then there is a potential for a reduction in solar activity to mitigate a small proportion of the future warming, a scenario we cannot totally rule out. While the Sun is not expected to provide substantial delays in the time to reach critical temperature thresholds, any small delays it might provide are likely to be greater for lower anthropogenic emissions scenarios than for higher-emissions scenarios.
机译:在20世纪,太阳活动增加所谓的宏大的最大大小。可能这高水平的太阳活动在或即将结束。是否未来的太阳活动的减少可能会对气候产生重大影响可以部分抵消预期人为气候变暖。太阳活动在过去的重建9000年作为限制是可能的未来的变化产生的概率太阳总辐照度的分布下一个100年。简单的气候模型,我们现在的结果对未来的预测潜在的影响气候年代际数十年时间尺度。使用的一个最近的重建历史太阳总辐照度,可能减少到2100年全球变暖是发现在0.06和0.1之间K,一个很小的一部分预计人为气候变暖。过去的太阳辐照总量变化更大和气候模型大大低估太阳能的响应变化,然后有一个潜在的对太阳活动的减少减轻未来的一小部分变暖,一个场景,我们不能完全排除。虽然太阳是不会提供的大量的延迟时间达到临界温度阈值,任何小的延迟可能提供较低的可能会更大人为排放的场景比更高的排放情况。

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