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首页> 外文期刊>Earth System Dynamics Discussions >Changes in extremely hot days under stabilized 1.5 and 2.0?°C global warming scenarios as simulated by the HAPPI multi-model ensemble
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Changes in extremely hot days under stabilized 1.5 and 2.0?°C global warming scenarios as simulated by the HAPPI multi-model ensemble

机译:由HAPPI多模型合奏模拟,在稳定的1.5和2.0°C全球变暖情景下,极热天的变化

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摘要

The half a degree additional warming, prognosis and projected impacts (HAPPI) experimental protocol provides a multi-model database to compare the effects of stabilizing anthropogenic global warming of 1.5?°C over preindustrial levels to 2.0?°C over these levels. The HAPPI experiment is based upon large ensembles of global atmospheric models forced by sea surface temperature and sea ice concentrations plausible for these stabilization levels. This paper examines changes in extremes of high temperatures averaged over three consecutive days. Changes in this measure of extreme temperature are also compared to changes in hot season temperatures. We find that over land this measure of extreme high temperature increases from about 0.5 to 1.5?°C over present-day values in the 1.5?°C stabilization scenario, depending on location and model. We further find an additional 0.25 to 1.0?°C increase in extreme high temperatures over land in the 2.0?°C stabilization scenario. Results from the HAPPI models are consistent with similar results from the one available fully coupled climate model. However, a complicating factor in interpreting extreme temperature changes across the HAPPI models is their diversity of aerosol forcing changes.
机译:半度附加变暖,预后和预计影响(HAPPI)实验方案提供了一个多模型数据库,用于比较将人为造成的全球变暖稳定在工业化前水平的1.5?C至这些水平上的2.0?C的影响。 HAPPI实验是基于由海面温度和可能对这些稳定水平合理的海冰浓度推动的全球大气模型的大集合。本文研究了连续三天平均出现的极端高温变化。还将极端温度测量值的变化与炎热季节温度的变化进行比较。我们发现,在陆地上,这种极端高温措施在1.5?C的稳定情景下,比目前的值从约0.5升高到1.5?C,具体取决于位置和型号。我们还发现,在2.0?C稳定情景下,陆地上的极端高温还会使温度再升高0.25至1.0?C。 HAPPI模型的结果与一种可用的完全耦合气候模型的相似结果一致。但是,解释HAPPI模型中极端温度变化的一个复杂因素是其气溶胶强迫变化的多样性。

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