Abstract In this study we analyze natural complex signals employing the Hilbert-Huang spectral analysis. Specifically, low wind meandering meteorological data are decomposed in turbulent and non turbulent components. These non turbulent movements, responsible by the absence of a preferential direction of the horizontal wind, provoke negative lobes in the meandering autocorrelation functions. The meandering characteristic time scales (meandering periods) are determined from the spectral peak provided by the Hilbert-Huang marginal spectrum. The magnitudes of the temperature and horizontal wind meandering period obtained agree with the results found from the best fit of the heuristic meandering autocorrelation functions. Therefore, the new method represents a new procedure to evaluate meandering periods that does not employs mathematical expressions to represent observed meandering autocorrelation functions.

Employing the Hilbert-Huang Transform to analyse observed natural complex signals: Calm wind meandering cases

Luca Mortarini;Domenico Anfossi;
2016

Abstract

Abstract In this study we analyze natural complex signals employing the Hilbert-Huang spectral analysis. Specifically, low wind meandering meteorological data are decomposed in turbulent and non turbulent components. These non turbulent movements, responsible by the absence of a preferential direction of the horizontal wind, provoke negative lobes in the meandering autocorrelation functions. The meandering characteristic time scales (meandering periods) are determined from the spectral peak provided by the Hilbert-Huang marginal spectrum. The magnitudes of the temperature and horizontal wind meandering period obtained agree with the results found from the best fit of the heuristic meandering autocorrelation functions. Therefore, the new method represents a new procedure to evaluate meandering periods that does not employs mathematical expressions to represent observed meandering autocorrelation functions.
2016
Istituto di Scienze dell'Atmosfera e del Clima - ISAC
Stable boundary layer
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/20.500.14243/319674
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