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Projected Changes in the Asian‐Australian Monsoon Region in 1.5°C and 2.0°C Global‐Warming Scenarios

机译:1.5°C和2.0°C全球升温情景下的亚澳季风区域的预计变化

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In light of the Paris Agreement, it is essential to identify regional impacts of half a degree additional global warming to inform climate adaptation and mitigation strategies. We investigate the effects of 1.5°C and 2.0°C global warming above preindustrial conditions, relative to present day (2006–2015), over the Asian‐Australian monsoon region (AAMR) using five models from the Half a degree Additional warming, Prognosis and Projected Impacts (HAPPI) project. There is considerable intermodel variability in projected changes to mean climate and extreme events in 2.0°C and 1.5°C scenarios. There is high confidence in projected increases to mean and extreme surface temperatures over AAMR, as well as more‐frequent persistent daily temperature extremes over East Asia, Australia, and northern India with an additional 0.5°C warming, which are likely to occur. Mean and extreme monsoon precipitation amplify over AAMR, except over Australia at 1.5°C where there is uncertainty in the sign of the change. Persistent daily extreme precipitation events are likely to become more frequent over parts of East Asia and India with an additional 0.5°C warming. There is lower confidence in projections of precipitation change than in projections of surface temperature change. These results highlight the benefits of limiting the global‐mean temperature change to 1.5°C above preindustrial, as the severity of the above effects increases with an extra 0.5°C warming.
机译:根据《巴黎协定》,必须确定全球变暖增加半度的区域影响,以为气候适应和减缓战略提供依据。我们使用来自半度额外变暖,预后的五个模型,调查了相对于今天(2006-2015)而言,工业化前条件下全球升温1.5°C和2.0°C对亚洲-澳大利亚季风区域(AAMR)的影响。和预计影响(HAPPI)项目。在2.0°C和1.5°C情景下,平均气候和极端事件的预计变化中,模型间存在很大差异。人们对AAMR的平均和极端地表温度预计升高以及在东亚,澳大利亚和印度北部频繁出现的每日持续极端温度抱有很高的信心,并有可能再升温0.5°C。除了在1.5°C的澳大利亚出现变化迹象不确定的澳大利亚以外,AAMR的平均和极端季风降水都会放大。在东亚和印度部分地区,持续的每日极端降水事件可能会变得更加频繁,而且气温还会升高0.5°C。降水变化的预测比表面温度变化的预测可信度低。这些结果凸显了将全球平均温度变化限制在比工业化前的温度高1.5°C的好处,因为随着温度升高0.5°C,上述影响的严重性会增加。

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