Upscale feedbacks associated with supercellular thunderstorms sampled during MPEX
Previously Published Material: American Meteorological Society's Conference on Severe Local Storms, November 2014, Madison, Wisconsin
Abstract ID#: 34565
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.
