The multifractal properties of a set of precipitation intensity fields measured during the Global Atmospheric Research Program (GARP) Atlantic Tropical Experiment ( GATE) are studied, and it is shown that one cannot reject the null hypothesis that the fields are generated by a nonlinear transformation of a linear Gaussian process. These results indicate that the choice of representing rainfall fields in terms of multifractal cascades or as a nonlinear transformation of a linear Gaussian process should be based on physical motivations and not solely on the outcome of data analysis.

Revisiting multifractality in rainfall fields / Ferraris, L; Gabellani, S; Parodi, U; von Hardenberg, J; Provenzale, A. - In: JOURNAL OF HYDROMETEOROLOGY. - ISSN 1525-755X. - 4:3(2003), pp. 544-551. [10.1175/1525-7541(2003)004<0544:RMIRF>2.0.CO;2]

Revisiting multifractality in rainfall fields

von Hardenberg, J;
2003

Abstract

The multifractal properties of a set of precipitation intensity fields measured during the Global Atmospheric Research Program (GARP) Atlantic Tropical Experiment ( GATE) are studied, and it is shown that one cannot reject the null hypothesis that the fields are generated by a nonlinear transformation of a linear Gaussian process. These results indicate that the choice of representing rainfall fields in terms of multifractal cascades or as a nonlinear transformation of a linear Gaussian process should be based on physical motivations and not solely on the outcome of data analysis.
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/11583/2814914