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Statistical Variability and Persistence Change in Daily Air Temperature Time Series from High Latitude Arctic Stations

机译:高纬度北极站每日气温时间序列的统计变化和持续变化

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In the last decades, Arctic communities have been reporting that weather conditions are becoming less predictable. Most scientific studies have not been able to consistently confirm such a trend. The question regarding the possible increase in weather variability was addressed here based on daily minimum and maximum surface air temperature time series from 15 high latitude Arctic stations from Canada, Norway, and the Russian Federation. A range of analysis methods were applied, distinguished mainly by the way in which they treat time scale. Statistical L-moments were determined for temporal windows of different lengths. While the picture provided by L-scale and L-kurtosis is not consistent with an increasing variability, L-skewness was found to change towards more positive values, reflecting an enhancement of warm spells. Haar wavelet analysis was applied both to the entire time series and to running windows. Persistence diagrams were generated based on running windows advancing through time and on local slopes of Haar analysis graphs; they offer a more nuanced view on variability by reflecting its change over time on a range of temporal scales. Local increases in variability could be identified in some cases, but no consistent change was detected in any of the stations over the studied temporal scales. The possibility for other intervals of temporal scale (e.g., days, hours, minutes) to potentially reveal a different situation cannot be ruled out. However, in the light of the results presented here, explanations for the discrepancy between variability perception and results of pattern analysis might have to be explored using an integrative approach to weather variables such as air temperature, cloud cover, precipitation, wind, etc.
机译:在过去的几十年中,北极社区一直在报告天气状况变得不可预测。大多数科学研究未能始终如一地证实这一趋势。这里基于来自加拿大,挪威和俄罗斯联邦的15个高纬度北极站的每日最低和最高地面气温时间序列,解决了有关天气变化性可能增加的问题。应用了一系列分析方法,主要通过它们处理时间刻度的方式来区分。确定不同长度的时间窗的统计L矩。尽管L尺度和L峰度所提供的图像与变异性的增加不一致,但发现L偏度朝着更正的值变化,反映出温暖的咒语的增强。 Haar小波分析既应用于整个时间序列,也应用于运行的窗口。持续性图是根据随时间前进的运行窗口以及Haar分析图的局部斜率生成的;通过在一定范围的时间尺度上反映随时间的变化,他们对变化具有更细微的了解。在某些情况下,可以确定局部变化的增加,但是在所研究的时间尺度上,任何一个测站均未检测到一致的变化。不能排除其他时间尺度上的时间间隔(例如,天,小时,分钟)可能揭示不同情况的可能性。但是,根据此处显示的结果,可能必须使用综合方法来研究诸如空气温度,云量,降水,风等天气变量的变异性感知与模式分析结果之间的差异。

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