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A model study of heat waves over North America: meteorological aspects and projections for the twenty-first century.

机译:北美热浪的模型研究:二十一世纪的气象方面和预测。

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The characteristics of summertime heat waves in North America are examined using reanalysis data and simulations by two general circulation models with horizontal resolution of 50 and 200 km. Several "key regions" with spatially coherent and high amplitude fluctuations in daily surface air temperature are identified. The typical synoptic features accompanying warm episodes in these regions are described. The averaged intensity, duration, and frequency of occurrence of the heat waves in various key regions, as simulated in the two models for twentieth-century climate, are in general agreement with the results based on reanalysis data. The impact of climate change on the heat wave characteristics in various key regions is assessed by contrasting model runs based on a scenario for the twenty-first century with those for the twentieth century. Both models indicate considerable increases in the duration and frequency of heat wave episodes, and in number of heat wave days per year, during the twenty-first century. The duration and frequency statistics of the heat waves in the mid-twenty-first century, as generated by the model with 50-km resolution, can be reproduced by adding the projected warming trend to the daily temperature data for the late twentieth century, and then recomputing these statistics. The detailed evolution of the averaged intensity, duration, and frequency of the heat waves through individual decades of the twentieth and twenty-first centuries, as simulated and projected by the model with 200-km resolution, indicates that the upward trend in these heat wave measures should become apparent in the early decades of the twenty-first century.
机译:使用重新分析数据和两个水平分辨率分别为50 km和200 km的一般环流模型对北美夏季热浪的特征进行了检验。识别出每日地面气温在空间上具有连贯性和高幅度波动的几个“关键区域”。描述了伴随这些地区温暖天气的典型天气特征。正如在两个世纪气候模型中所模拟的那样,在两个关键地区热浪在各个关键区域的平均强度,持续时间和发生频率与基于再分析数据的结果总体上是一致的。通过对比基于二十一世纪和二十世纪情景的模型运行,评估了气候变化对各个关键地区热浪特征的影响。两种模型都表明,在二十一世纪期间,热浪发作的持续时间和频率以及每年的热浪天数都显着增加。由分辨率为50 km的模型生成的二十一世纪中叶热浪的持续时间和频率统计数据可以通过将预计的变暖趋势添加到二十世纪后期的每日温度数据中来再现,并且然后重新计算这些统计信息。由200 km分辨率的模型模拟和预测的,在二十世纪和二十一世纪各个十年中热浪的平均强度,持续时间和频率的详细演变,表明这些热浪的上升趋势这些措施应该在二十一世纪初出现。

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