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首页> 外文期刊>International Journal of Climatology: A Journal of the Royal Meteorological Society >Adjusting inhomogeneous daily temperature variability using wavelet analysis
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Adjusting inhomogeneous daily temperature variability using wavelet analysis

机译:使用小波分析调整每日温度的不均匀性

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A wavelet-analysis-based homogenization method (WHM) is developed for detecting and adjusting biases of variability in a daily climate observation series, which are influential in the estimation of climate extremes and relevant trends in the time series. WHM is applied to the Central England daily mean temperature series (CET, 1772-2010) and the daily mean temperature series at Henan station in mountainous western China (HNT, 1960-2008) in order to demonstrate the usefulness of the new technique. The changes of methods for calculating daily mean temperature for CET in 1878 caused significantly reduced daily variability (DV) in the subsequent sub-series of CET. The relocation of the Chinese station in 1981 to a higher mountainous site resulted in not only enhanced DV but also in weather (weekly) time-scale variability (WV) in the subsequent sub-series of HNT. The adjustments based on WHM in the present cases improve the estimates of the long-term trends of climate extremes such as hot days, cold days, heat waves, and cold surges. A few widely applied methods of homogenization such as multiple analysis of series for homogenization (MASH), higher-order moment (HOM), RHtestsV3 with quantile-matching (QM) adjustments and two-phase regression (TPR) are also applied to HNT for comparison. TPR is not aimed at improving the homogeneity of variability in the time series; MASH does not improve daily variability either; HOM improves it in a small way; and with RHtestsV3 with QM adjustments it is considerably improved, but biases remain. In contrast, WHM improves the homogeneity of the short-term variability in the time series, resulting in reasonable assessments of climate extremes and trends in the daily observations.
机译:开发了一种基于小波分析的均化方法(WHM),用于检测和调整每日气候观测序列中的变异性偏差,这对估计气候极端事件和时间序列中的相关趋势有影响。 WHM被应用于英格兰中部的每日平均温度序列(CET,1772-2010)和中国西部山区河南站的每日平均温度序列(HNT,1960-2008),以证明该新技术的实用性。 1878年,计算CET日平均温度的方法发生了变化,从而在随后的CET子系列中大大降低了日变化(DV)。 1981年,中国台站迁至更高的山区,不仅导致DV增强,而且在随后的HNT子系列中也导致了天气(每周)时标变化(WV)。在当前情况下,基于WHM的调整改进了对极端气候(如炎热天,寒冷天,热浪和寒冷浪潮)的长期趋势的估计。均化的几种广泛应用的方法,例如均化级数的多重分析(MASH),高阶矩(HOM),具有分位数匹配(QM)调整的RHtestsV3和两相回归(TPR),也适用于比较。 TPR并非旨在改善时间序列中变异性的均一性; MASH也不能改善每日变化。 HOM在很小的程度上对其进行了改进;并通过带有QM调整的RHtestsV3进行了很大的改进,但是仍然存在偏差。相比之下,WHM可以提高时间序列中短期变化的均匀性,从而可以合理评估每日观测的极端气候和趋势。

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