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首页> 外文期刊>Journal of Geophysical Research, D. Atmospheres: JGR >Regional differentiation in multidecadal connections between Indian monsoon rainfall and solar activity
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Regional differentiation in multidecadal connections between Indian monsoon rainfall and solar activity

机译:印度季风降雨与太阳活动之间的年代际联系的区域差异

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摘要

The wavelet cross spectra of the yearly sunspot index and homogeneous-zone Indian monsoon rainfall time series are examined over the 120 a period 1871–1990 using Morlet continuous wavelets. The cross spectra of sunspot numbers with synthetic noise ensembles, including those matching the spectrum and probability distribution function of the rainfall time series, are used as reference to assess the significance of the cross spectrum between sunspot numbers and rainfall; their differences are studied using standard statistical tests. It is found particularly revealing to consider the two test periods 1878–1913 and 1933–1964, each comprising three complete solar cycles, which between them exhibit maximum contrast in solar activity since the beginning of accurate rainfall data collection in India [1871]. It is shown that the cumulative distribution of the 9–13 a band averaged cross power between sunspots and rainfall, derived from yearly values over either test period, differs from that between sunspots and spectrally matched noise in the same period at confidence levels of 99.5% or higher by the χ 2 test. Further, the cross power of the sunspot index with rainfall, averaged over either test period, exceeds that with synthetic noise at z test confidence levels exceeding 99.99% over scale bands covering the 11.6 a sunspot cycle. The results further show variations across the different homogeneous rainfall zones of India, northeast India exhibiting a dramatically different phase relationship compared to the western regions of the country. The strong connections demonstrated here between Indian rainfall and solar activity are found to be organized approximately along quasi-longitudinal bands tilting eastward at their northern end. This suggests that higher solar activity causes intensification of the Walker and Hadley circulations; the mechanisms that may be responsible and the evidence from models are briefly discussed.
机译:利用Morlet连续小波对120个1871–1990年期间的太阳黑子指数和均质带印度季风降雨时间序列的小波交叉谱进行了检查。具有合成噪声集合的黑子数互谱,包括与降雨时间序列的频谱和概率分布函数匹配的那些,被用作评估黑子数与降雨之间的互谱意义的参考;使用标准统计检验研究它们之间的差异。发现特别揭示了考虑两个测试期1878–1913和1933–1964,每个测试期包括三个完整的太阳周期,自印度开始准确的降雨数据收集以来,它们之间就表现出太阳活动的最大反差[1871]。结果表明,在任何一个测试期内,从太阳黑子和降雨之间的9-13波段平均交叉功率的累积分布,根据同一时期的年值得出,不同于同一时期黑子和频谱匹配噪声之间的累积分布,置信度为99.5%。或通过χ2检验更高。此外,在任一测试期间内,黑子指数与降雨的交叉功率均超过了在覆盖11.6个黑子周期的尺度范围内,z检验置信度水平上的合成噪声超过99.99%时的综合噪声。结果进一步表明,在印度不同的均匀降雨带之间存在差异,与印度西部地区相比,印度东北部呈现出显着不同的相位关系。此处发现印度降雨与太阳活动之间的强联系大致沿着其北端向东倾斜的准纵向带组织。这表明较高的太阳活动导致沃克和哈德利环流的加剧。简要讨论了可能负责任的机制以及来自模型的证据。

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