Significance of the Coupled Term in the Doppler Weather Radar Spectrum Width Equation

Author:

Fang Ming1,Doviak Richard J.2,Albrecht Bruce A.1

Affiliation:

1. Rosenstiel School of Marine and Atmospheric Science, The University of Miami, Miami, Florida

2. National Severe Storms Laboratory, Norman, Oklahoma

Abstract

AbstractThere is an additional zero mean random variable term that couples mean wind shear and turbulence in the Doppler radar spectrum width equation. This random variable, labeled the “coupled term,” has been neglected heretofore in the literature. Herein, the variance of the squared spectrum width ascribed to this coupled term is determined from data collected with a Weather Surveillance Radar-1988 Doppler (WSR-88D) in two snowstorms; it can exceed 1 m4 s−4. Thus, this coupled term can be a significant contributor to the variance of the spectrum width and must be considered when using spectrum width to deduce turbulence.

Publisher

American Meteorological Society

Subject

Atmospheric Science,Ocean Engineering

Reference17 articles.

1. The Theory of Homogeneous Turbulence;Batchelor,1960

2. Doppler Radar and Weather Observations;Doviak,2006

3. Theoretical and practical considerations in using spectrum width data;Doviak,2008

4. Spectral analysis of detailed vertical wind speed profiles;Endlich;J. Atmos. Sci.,1969

5. The spectrum width equations for Doppler weather radar and the coupling of spectral broadening terms;Fang,2008

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