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Comment on 'Influence of the Southern Oscillation on tropospheric temperature' by J. D. McLean, C. R. de Freitas, and R. M. Carter

机译:评“南方涛动对对流层的影响”   温度“由J. D. mcLean,C。R. de Freitas和R. m. Carter撰写

摘要

We demonstrate an alternative correlation between the El Ni\~no SouthernOscillation (ENSO) and global temperature variation to that shown by McLean etal. [2009]. We show 50% of the variation in RATPAC-A tropospheric temperature(and 54% of HadCRUT3) is explained by a novel cumulative Southern OscillationIndex (cSOI) term in a simple linear regression. We review evidence fromphysical and statistical research in support of the hypothesis thataccumulation of the effects of ENSO can produce natural multi-decadal warmingtrends. Although it is not possible to reliably determine the relativecontribution of anthropogenic forcing and SOI accumulation from multipleregression models due to collinearity, these analyses suggest that anaccumulation ratio cSOI/SOI of $4.8\pm1.5%$ and up to $9\pm2%$ is sufficientfor ENSO to play a large part in the global mean temperature trend since 1960.
机译:我们证明了厄尔尼诺或南方涛动(ENSO)与全球温度变化之间的另一种相关性,与麦克莱恩等人所显示的相关。 [2009]。我们显示,RATPAC-A对流层温度的50%的变化(和HadCRUT3的54%)由简单的线性回归中的新型累积南方涛动指数(cSOI)术语解释。我们回顾了来自物理和统计研究的证据,以支持以下假设,即ENSO的影响累积会产生自然的多年代际变暖趋势。尽管由于共线性不可能从多元回归模型可靠地确定人为强迫和SOI积累的相对贡献,但这些分析表明,累积比率cSOI / SOI为$ 4.8 \ pm1.5%$,最高为$ 9 \ pm2%$自1960年以来,ENSO在全球平均气温趋势中扮演着重要角色。

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