Extended Abstract (108K)7A.2
Some Effects of the Stochastic Structure of Rain on Remote Sensing Observations Part 2: Z-R Relations and Raindrop Size Distributions
A. R. Jameson, RJH Scientific, Inc., Arlington, VA; and A. B. Kostinski
It is shown in recent work that physically-based, linear relations between the radar reflectivity factor, Z, and the rainfall rate, R, (as well as between other parameters) apply in statistically homogeneous rain. This conclusion is proven theoretically after developing a ‘generalized' Z-R relation based upon the physical consideration of R and Z as random variables. This relation explicitly incorporates details of the drop microphysics as well as the variability in measurements of Z and R. In statistically homogeneous rain, this generalized expression shows that the coefficient relating Z and R is a constant resulting in a linear Z-R relation. A physical explanation is also given based upon the observation that the statistical homogeneity of the rain requires that the mean flux and mean number concentration at each drop size remain fixed. Consequently, the pdf of D, p(D), is ‘steady' so that the ratio R/Z is constant. In such rain the drop size distribution has an intrinsic physical interpretation independent of the measurement process. Furthermore, convergence toward this distribution is fastest in ‘steady' rain, discussed in Part 1.
In statistically inhomogeneous rain, however, the coefficient relating Z and R varies in an unknown fashion so that one must resort to statistical fits, often power laws, in order to relate the two quantities empirically over widely varying conditions. The ‘justification' for non-linear power law Z-R relations is not physical, but rather statistical in that they provide convenient parametric fits for estimating mean R from measured mean Z in statistically inhomogeneous rain. Accordingly, the interpretations of drop size distributions in statistically inhomogeneous rain now depend upon the measurement process. Furthermore, in statistically inhomogeneous rain, different remote sensing instruments, even if pointed at the same target, will see different total drop size distributions simply because the beam-widths are not the same. This will affect all algorithms which assume that different instruments are viewing the same set of drops.
Finally, examples suggest that such generalized relations between two variables defined by such sums are potentially useful over a wide range of remote sensing problems and over a wide range of scales. Application of such relations, however, requires the extraction from the non-Rayleigh signal statistics, common to almost all radar and radiometer observations, of the component of the variances due to the distribution of mean values.
Session 7A, Quantitative Rainfall—Microphysics I (Parallel with Session 7B)
Saturday, 21 July 2001, 4:00 PM-6:00 PM
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