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首页> 外文期刊>Journal of Climate >Trend singular value decomposition analysis and its application to the global ocean surface latent heat flux and SST anomalies.
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Trend singular value decomposition analysis and its application to the global ocean surface latent heat flux and SST anomalies.

机译:趋势奇异值分解分析及其在全球海洋表面潜热通量和海表温度异常中的应用。

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Given the complexity of trends in the actual climate system, distinguishing between different trends and different trend modes is important for climate research. This study introduces a new method called "trend singular value decomposition (TSVD) analysis", which is designed for systematically extracting coupled trend modes, albeit small, by performing an eigenanalysis of the inverse-rank covariance matrix between two fields. Applications to simple time series models and annual mean surface latent heat flux (LHF) and SST data for 1958-2006 are presented and discussed. Results show that the TSVD analysis can capture different coherent trends into different leading modes. The first TSVD mode between the global LHF and SST anomalies, similar to the first conventional SVD mode, generally represents a large-scale increasing LHF trend induced by a warming SST trend; whereas, interestingly, unlike the second SVD mode that is mainly associated with the familiar ENSO, the second TSVD mode is mainly associated with the Pacific decadal oscillation (PDO). TSVD analysis casts the (global) long-term and (Pacific) decadal trends into the leading two modes, respectively. Compared to SVD analysis, the advantages of the TSVD analysis in detecting coupled low-frequency modes are even more evident in the tropical Pacific (TP), where the coherent trend signals (i.e., the long-term trends and the decadal trends) are smaller than the ENSO-related signals. Thus, TSVD analysis performs better than SVD analysis when focusing on trends rather than on maximum covariance patterns, particularly on relatively small coherent trend patterns, such as the coupled long-term trends and decadal trends in the TP.Digital Object Identifier http://dx.doi.org/10.1175/2010JCLI3743.1
机译:考虑到实际气候系统中趋势的复杂性,区分不同趋势和不同趋势模式对于气候研究非常重要。这项研究引入了一种称为“趋势奇异值分解(TSVD)分析”的新方法,该方法旨在通过对两个场之间的逆秩协方差矩阵进行特征分析来系统地提取耦合趋势模式(尽管很小)。介绍并讨论了1958-2006年的简单时间序列模型以及年平均表面潜热通量(LHF)和SST数据的应用。结果表明,TSVD分析可以将不同的相关趋势捕获到不同的主导模式中。类似于第一个传统的SVD模式,全局LHF和SST异常之间的第一个TSVD模式通常代表由SST变暖引起的大规模LHF趋势增加。相反,有趣的是,与主要与熟悉的ENSO相关的第二SVD模式不同,第二TSVD模式主要与太平洋年代际振荡(PDO)相关。 TSVD分析将(全球)长期和(太平洋)年代际趋势分别转换为两种主导模式。与SVD分析相比,TSVD分析在检测耦合低频模式方面的优势在热带太平洋(TP)中更为明显,那里的相关趋势信号(即长期趋势和年代际趋势)较小而不是ENSO相关信号。因此,当重点关注趋势而不是最大协方差模式时,TSVD分析的性能要优于SVD分析,尤其是在相对较小的相干趋势模式(例如TP中长期趋势和年代际趋势的耦合)上。 dx.doi.org/10.1175/2010JCLI3743.1

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