Normalized Hail Particle Size Distributions from the T-28 Storm-Penetrating Aircraft

Author:

Field Paul R.1,Heymsfield Andrew J.2,Detwiler Andrew G.3,Wilkinson Jonathan M.4

Affiliation:

1. Met Office, Exeter, and Institute for Climate and Atmospheric Science, University of Leeds, Leeds, United Kingdom

2. National Center for Atmospheric Research, Boulder, Colorado

3. Department of Physics, and Atmospheric and Environmental Sciences Program, South Dakota School of Mines and Technology, Rapid City, South Dakota

4. Met Office, Exeter, United Kingdom

Abstract

AbstractHail and graupel are linked to lightning production and are important components of cloud evolution. Hail can also cause significant damage when it precipitates to the surface. The accurate prediction of the amount and location of hail and graupel and the effects on the other hydrometeor species depends upon the size distribution assumed. Here, we use ~310 km of in situ observations from flights of the South Dakota School of Mines and Technology T-28 storm-penetrating aircraft to constrain the representation of the particle size distribution (PSD) of hail. The maximum ~1-km hail water content encountered was 9 g m−3. Optical probe PSD measurements are normalized using two-moment normalization relations to obtain an underlying exponential shape. By linking the two normalizing moments through a power law, a parameterization of the hail PSD is provided based on the hail water content only. Preliminary numerical weather simulations indicate that the new parameterization produces increased radar reflectivity relative to commonly used PSD representations.

Funder

National Science Foundation

Publisher

American Meteorological Society

Subject

Atmospheric Science

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3. Some measurements of snow pellet bulk-densities;Braham;J. Appl. Meteor.,1963

4. Toward a global climatology of severe hailstorms as estimated by satellite passive microwave imagers;Cecil;J. Climate,2012

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