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Title: Effects of vertical wind shear on the cumulus transport of momentum: Observations and parameterization

Journal Article · · Journal of the Atmospheric Sciences; (United States)
;  [1]
  1. Univ. of California, Los Angeles, Los Angeles, CA (United States)

Dynamical effects of organized cumulus convection on its environment with vertical wind shear are studied. Analyses of the wind field and momentum budget residual for mesoscale convective systems observed during Severe Environmental Storms and Mesoscale Experiment (SESAME) and Preliminary Regional Experiment for Storm-Central (PRE-STORM) reveal systematic differences in the vertical transport of horizontal momentum between mesoscale convective complex (MCC) and squall line cases. In the MCC, a distinct minimum in wind speed appears over the area of intense convection and the momentum budget residual acts to decelerate the environmental wind and to reduce the upper-level vertical shear. Therefore, the inferred vertical transport of momentum in the MCC is downgradient in the upper layer. On the other hand, in the squall line, there is no wind speed minimum and the upper-level vertical shear of the line-normal component of the environmental wind increases as convection develops. Thus, the vertical transport of momentum normal to the squall line is upgradient in the upper layer, although the transport of momentum parallel to the line is downgradient. The effects of cumulus convection on the environmental flow are through the subsidence of environmental air that compensates the cloud mass flux, the detrainment of momentum from clouds, and the convective-scale horizontal pressure gradient force acting on the environment. A cumulus momentum parameterization including the convective-scale pressure gradient force is formu lated.

OSTI ID:
6710227
Journal Information:
Journal of the Atmospheric Sciences; (United States), Vol. 51:12; ISSN 0022-4928
Country of Publication:
United States
Language:
English