Monday, 16 September 2013: 9:30 AM
Colorado Ballroom (Peak 4&5, 3rd Floor) (Beaver Run Resort and Conference Center)
Christopher R. Williams, CIRES/Univ. of Colorado, Boulder, CO
The raindrop size distribution (DSD) can be described as a Gamma function with three parameters (e.g., N
w, D
m and µ). Previous studies have shown that these three parameters are correlated. But there is controversy in the research literature over why the three parameters are correlated. Some studies suggest that the correlation is a statistical artifact due to correlation between the raindrop spectrum moments. Other studies suggest that the correlation is not a statistical artifact and have developed slope-shape (µ-Λ) relationships so that the three parameter Gamma function can be described as a constrained two parameter function.
Analysis of vertical profiles of DSD estimates and surface disdrometer observations from the Mid-Continental Convective Cloud Experiment (MC3E) and other field campaigns suggests a relationship between the mass-weighted mean diameter (Dm) and the mass spectrum standard deviation (σm). This relationship is not a statistical artifact due to correlations between spectrum moments and suggests a physical relationship between the two DSD parameters.
There are mathematical relationships that relate σm , Dm and µ. These relationships imply that data can be analyzed in σm Dm space and then converted into µ Dm space (if needed) avoiding the statistical artifact controversy of directly estimating µ from spectrum moments. The DSD parameter retrievals and the relationships between retrieved DSD parameters will be presented at the conference.
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