Abstract
Climatic records of a long time series (eg, centuries) may be nonstationary. Thus, the stability of the variance (power) spectrum over a sequence of time periods is examined. Variance spectra of Hohenpeissenberg (FRG) annual mean air temperatures are compared using two methods, autocorrelation spectral analysis (ASA) and maximum entropy spectral analysis (MESA). These spectra are then compared with corresponding spectra based on Northern Hemisphere temperature reconstructions. The application of a moving (running, "dynamic') variance spectrum analysis shows that, in general, the signals found in the customary "integrated' spectrum vary as time varies, namely in their occurrence, significance and "bandwidth'. Similarly, coherence spectra can be computed in moving terms. As an example the Northern Hemisphere data are spectrally correlated with the corresponding central England and Philadelphia air temperature series. It is shown that the coherences are not stable in time, and that the spectral characteristics throw considerable doubt on the reliability of the reconstructed Northern Hemisphere temperature series prior to 1881. -from Author
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CITATION STYLE
Schonwiese, C. D. (1987). Moving spectral variance and coherence analysis and some applications on long air temperature series. Journal of Climate & Applied Meteorology, 26(12), 1723–1730. https://doi.org/10.1175/1520-0450(1987)026<1723:MSVACA>2.0.CO;2
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