Investigation of stability characteristics of thundersnow events utilizing the growth rate parameter.
Singer, Marc
Stability characteristics of thunder snow events across the central
United States were examined in order to provide more insight into how
the environment becomes destabilized over a relatively short period of
time. For this purpose, calculations of a growth rate parameter
([[sigma].sup.2]) are performed for seven archived case studies during
the 2003-04 winter season utilizing numerical weather model output from
the 40-km RUC. Results from this stability tendency revealed that the
doubling time for the convection was upon the order of 2.4 hours, which
was consistent with the typical timescale for moist slantwise convection
released from conditional symmetric instability. In addition, the
development of mesoscale snowbands was correctly predicted with the
associated computed values for [[sigma].sup.2] easily surpassing the 0.2
h-2 criterion. One rather intense case study will be provided in order
to illustrate the usefulness of this method in an operational
environment, with a term-by-term diagnosis of the mathematical
expression also presented.
* Melick, C.J., L.L. Smith, P.S. Market and B.P. Pettegrew.
Department of Soil, Environmental, and Atmospheric Sciences, University
of Missouri-Columbia.