Authors: Herbert Weidner
Signale unbekannter Herkunft kann man in den Gravitationsdaten der SG nur entdecken, nachdem die störenden Gezeitenoszillationen beseitigt sind. Das Verfahren der inversen FFT-Filterung kann im Gegensatz zu den üblichen Hochpassfiltern die riesigen Unterschiede der Amplituden ohne Zusatzrauschen verarbeiten. Das Verfahren wird ausführlich beschrieben. (Signals of unknown origin can be detected in the SG gravity data only after the interfering tidal oscillations are removed. The inverse FFT filtering method, unlike the usual high-pass filters, can handle the huge differences in amplitudes without additional noise. The procedure is described in detail.)
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