Spectra and correlations of climate data from days to decades

The correlations of several daily surface meteorological parameters such as maximum, minimum, and mean temperature, diurnal temperature range, pressur e, precipitation, and relative air humidity are analyzed by partly compleme ntary methods being effective on different timescales: power spectral analy sis, second- and higher-degree detrended fluctuation analysis, Hurst analys is, and the direct estimation of the autocorrelation in the time domain. Da ta from American continental and maritime and European low-elevation and mo untain stations are used to see possible site dependencies. For all station types and locations, all meteorological parameters show correlations from the shortest to the longest statistically reliable timescales of about thre e decades. The correlations partly show a clear power law scaling with site -dependent exponents. Mainly, the short-time behavior of the correlations d epends on the station type and differs considerably among the various meteo rological parameters. In particular, the detrended fluctuation and the Hurs t analyses reveal a possible power low behavior for long timescales which i s less well resolved or even may remain unrecognized by the classical power spectral analysis and from the autocorrelation. The long-time behavior of the American temperatures is governed by power laws. The corresponding expo nents coincide for all temperatures except for the daily temperature range with different values for the maritime and the continental stations. From t he European temperatures those from low-elevation stations also scale quite well, whereas temperatures from mountain stations do not.