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Annales Geophysicae An interactive open-access journal of the European Geosciences Union
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Volume 15, issue 11
Ann. Geophys., 15, 1447–1456, 1997
https://doi.org/10.1007/s00585-997-1447-6
© European Geosciences Union 1997
Ann. Geophys., 15, 1447–1456, 1997
https://doi.org/10.1007/s00585-997-1447-6
© European Geosciences Union 1997

  30 Nov 1997

30 Nov 1997

Wavelet analysis of turbulence in cirrus clouds

S. A. Smith* and P. R. Jonas S. A. Smith and P. R. Jonas
  • UMIST, PO Box 88, Manchester, M60 1QD, UK
  • *Currently at: Columbia University and NASA GISS, 2880 Broadway, New York, NY10025, USA

Abstract. Two flights of the UK Meteorological Office's Hercules aircraft through daytime frontal cirrus around Scotland have been analysed using wavelet analysis on the vertical velocity time-series from the horizontal runs. It is shown that wavelet analysis is a useful tool for analysing the turbulence data in cirrus clouds. It finds the largest scales involved in producing turbulence, as does Fourier analysis, such as the 2-km spectral peaks corresponding to convective activity during flight A283. Wavelet spectra have the added advantage that the position is shown, and so they identify smaller-scale, highly localised processes such as the production of turbulent kinetic energy by the breaking of Kelvin-Helmholtz waves due to the vertical shear in the horizontal wind. These may be lost in Fourier spectra obtained for long time-series, though they contribute something to the average spectral density at the appropriate scale. The main disadvantage of this technique is that only octave frequency bands are resolved.

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