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1.5 degrees, 2 degrees, and 3 degrees global warming: visualizing European regions affected by multiple changes

机译:1.5度,2度和3度全球变暖:可视化受多次变化影响的欧洲地区

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Assessing multiple climatic and non-climatic variables affecting one region at the same time is a crucial aspect to support climate adaptation action. This publication presents a method to display relevant measures of any three adaptation relevant parameters (or optionally their projected future changes) at once on a map by allocating them to multiple transparency levels of the three primary colors of additive color mixing (red, green, and blue). The overlay of information allows the combined assessment of the regional exposures. The method is demonstrated by two examples based on an ensemble of regional climate projections analyzed for 1.5 degrees C, 2 degrees C, and 3 degrees C global warming periods. The first example shows the increasing number of people at risk for summer climate extremes under 1.5 degrees C, 2 degrees C, and 3 degrees C global warming by combining projected increases in tropical nights and summer intense precipitation days with today's population density. Under 3 degrees C global warming, many heavily populated areas across Europe are affected by both heat stress and summer precipitation extremes, whereas under 1.5 degrees C global warming, heat stress regions are restricted to southern Europe and the large settlements along the Eastern Mediterranean coast. A second example combines daily mean and minimum and maximum summer temperatures and highlights the regional expansion and the increasing robustness of projected mean summer warming with rising global warming levels, as well as the regional day to night differences of the warming signal.
机译:同时评估影响一个区域的多气候和非气候变量是支持气候适应行动的关键方面。该出版物通过将它们的三个原色混合(红色,绿色,以及红色,绿色,以及红色,绿色,以及红色,绿色和)的多种透明度水平分配给多种透明度水平,提出了一种在地图上显示任何三个适应相关参数(或可选的未来变化)的方法。蓝色)。信息的覆盖层允许协会评估区域风险。该方法是基于分析1.5℃,2摄氏度和3摄氏度的全球变暖周期的区域气候投影的集合的两个实例。第一个例子显示了越来越多的人,夏季气候极端的风险有1.5摄氏度下,2摄氏度和3摄氏度全球变暖,通过组合热带夜晚和夏季激烈的降水日,随着当今人口密度的夏季激烈的降水日。在3摄氏度下,全球变暖下,欧洲各地的许多人口稠密的地区都受到热应力和夏季降水极端的影响,而在1.5摄氏度下,南欧的南欧和东地中海沿岸的大型住区受到热压力和夏季降水。第二个例子结合了每日平均值和最低和最大夏季气温,并突出了区域扩张,并在全球变暖水平上升的区域升温以及夜间差异的温暖信号的区域日差异,突出了区域扩张和增加的鲁棒性。

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