Upscale feedbacks associated with supercellular thunderstorms sampled during MPEX

Robert Jeffrey Trapp, University of Illinois Urbana-Champaign, Department of Climate, Meteorology, and Atmospheric Sciences, Urbana, United States, Joseph Woznicki, Dept Earth & Atmospheric Scien, West Lafayette, IN, United States and Michael E Baldwin, Purdue University, West Lafayette, IN, United States

Contact First Author: Robert Jeffrey Trapp; jtrapp@illinois.edu

Previously Published Material: American Meteorological Society's Conference on Severe Local Storms, November 2014, Madison, Wisconsin

Abstract ID#: 34565

 

English Abstract:
Deep convective storms are well known to modify the 3D temperature, moisture, and wind distributions of their local environment via adiabatic and diabatic processes. There are still uncertainties, however, about the duration and areal extent of such modifications as a function of the mode of convection, including supercellular thunderstorms. These uncertainties served to motivate one of the research foci of Mesoscale Predictability Experiment (MPEX), which specifically regarded convective upscaling and its feed back to the convective-scale dynamics and predictability. Using balloon-borne GPS radiosondes, such upscale feedbacks were sampled during the MPEX field phase, which was conducted 15 May through 15 June 2013 within the Great Plains region of the United States.

Analyses of the MPEX soundings collected in the immediate environment of supercellular thunderstorms are indicating that the sampled supercells produced a significant, persistent upscale feedback mostly near the ground, in the form of a surface-based cold pool. This was realized as a marked reduction of environmental convective available potential energy, and as a slight modification of the vertical wind shear. Thus, as confirmed using complementary idealized model simulations, the strength, areal extent, and depth of the cold pool were critical to the upscale feedback, which highly influenced how rapidly the local atmosphere could return to its pre-convective state.

Significant feedbacks aloft tended to be transient, moving with the storm rather than trailing in the wake or otherwise extending well beyond the storm’s confines. For example, the most significant modifications to the vertical wind shear owed to storm-induced (e.g., mesocyclonic) enhancements of the midlevel winds. Similarly, the mid-level lapse rates were modified mostly within translating updraft regions.

Other MPEX cases, especially those involving non-supercellular convection, are being analyzed in tandem with model simulations to explore the veracity and implications of these findings.