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Validation of a stochastic temperature generator focusing on extremes, and an example of use for climate change

机译:以极端为重点的随机温度发生器的验证,以及用于气候变化的示例

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ABSTRACT: We present a stochastic seasonal functional heteroscedastic auto-regressive model developed to simulate daily (minimum, maximum, or mean) temperature time series coherent with observed time series and designed to reliably reproduce extreme values through a careful study of extremes and the fact that the tails of the distribution are bounded. The model was first validated using different daily minimum and maximum weather station time series over Eurasia and the US in different climatic regions. The model was able to produce coherent results both for the bulk of the distribution and for its extremes and was able to produce higher or lower extreme values than observed. A possible use in the climate change context was then tested. We fit the model over the first part of a long temperature time series and then used it to simulate a large number of possible trajectories for the second part when temperature increased. Two approaches were tested to do so, one based on a simple mean change in mean and variance and the other in considering the full seasonalities and trends estimated over the observed second part of the time series. Both approaches yielded good results, both for the bulk and for the extremes of the temperature distribution over the second part of the period. However, the second approach allowed us to take interannual variability changes into account, which leads to more realistic results when this occurs. Our results support the use of this tool for statistical downscaling, enabling the reliable reproduction of temperature extremes.
机译:摘要:我们提出了一种随机的季节性功能异方差自回归模型,用于模拟与观察到的时间序列相一致的每日(最小,最大或平均)温度时间序列,旨在通过仔细研究极端值和事实来可靠地再现极端值。分布的尾部是有界的。该模型首先使用欧亚大陆和美国不同气候区域的不同每日最小和最大气象站时间序列进行了验证。该模型能够为大部分分布及其极端产生一致的结果,并且能够产生比所观察到的更高或更低的极值。然后测试了在气候变化背景下的可能用途。我们在较长的温度时间序列的第一部分上拟合模型,然后使用该模型为第二部分在温度升高时模拟大量可能的轨迹。测试了两种方法来执行此操作,一种方法是基于均值和方差的简单均值变化,另一种方法是考虑在观察到的时间序列第二部分中估计的整个季节性和趋势。两种方法都产生了良好的结果,无论是对于第二阶段的大部分还是极端的温度分布。但是,第二种方法使我们能够考虑年际变化,当这种情况发生时,可以得出更实际的结果。我们的结果支持使用此工具进行统计缩小,从而能够可靠地再现极端温度。

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