1991
DOI: 10.1007/bf00876893
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A note on the spatial structure of the covariability of observed Northern Hemisphere surface air temperatures

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Cited by 3 publications
(2 citation statements)
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“…2. By spectrally decomposing 100 randomly generated surrogate rainfall data matrices, we choose the fifth largest eigenvalue for each mode to represent the 95% significance level (Overland and Presendorfer 1982;Elsner and Tsonis 1991). This significance level, which is based on the assumption of white noise, is shown as the dashed line in Fig.…”
Section: Regionalizationmentioning
confidence: 99%
“…2. By spectrally decomposing 100 randomly generated surrogate rainfall data matrices, we choose the fifth largest eigenvalue for each mode to represent the 95% significance level (Overland and Presendorfer 1982;Elsner and Tsonis 1991). This significance level, which is based on the assumption of white noise, is shown as the dashed line in Fig.…”
Section: Regionalizationmentioning
confidence: 99%
“…Then, as was done with the original data, the spectrum of surrogate eigenvalues is determined (Asw) from the matrix Csm = Rsm -Wsw. Repeating the entire procedure 100 times gives us a distribution of surrogate eigenvalues, and the magnitude of the fifth largest eigenvalue for each mode is chosen as the 95 percent significance level (Overland and Presendorfer, 1982;Elsner and Tsonis, 1991).…”
Section: Upper Bound On the Number Of Factorsmentioning
confidence: 99%