Lohmann, Gerrit

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StatisticCovariance (cross, auto)g(D) = E (( x (t) - x ) ( y (t + D) – y ))e.g. coral e.g. meteorol. dataCorrelation (cross, auto)rxy =                measures the tendency of x (t) and y (t) to covaryg(D)normalizedSpectrum (cross, auto)(spectral density)G(w) =S   g (D) e-2piDD=-measures variance88Climate Modes from Proxy DataComposite Map of SST [°C] and 925 hPa wind [m/s]         for 1948 -1995, January - February  mechanistic understanding

Dynamical interpretation of paleoclimate data: Corals and atmospheric circulation

https://epic.awi.de/id/eprint/56732/1/Coral_slide_Lohmann_2022.pdf

Dynamical interpretation of paleoclimate data: Corals and atmospheric circulation

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