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Title: Numerical simulations of mesoscale precipitation systems. Final progress report, 1 April-30 June 1981

Technical Report ·
DOI:https://doi.org/10.2172/5306154· OSTI ID:5306154

A numerical model designed for the study of mesoscale weather phenomena is presented. It is a three-dimensional, time-dependent model based upon a mesoscale primitive-equation system, and it includes parameterizations of cloud and precipitation processes, boundary-layer transfers, and ground surface energy and moisture budgets. This model was used to simulate the lake-effect convergence over and in the lee of Lake Michigan in late fall and early winter. The lake-effect convergence is created in advected cold air as it moves first from cold land to the warm constant-temperature lake surface, and then on to cold land. A numerical experiment with a prevailing northwesterly wind is conducted for a period of twelve hours. Two local maxima of the total precipitation are observed along the eastern shore of Lake Michigan. The results in this hypothetical case correspond quite well to the observed precipitation produced by a real event in which the hypothetical conditions are approximately fulfilled.

Research Organization:
Michigan Univ., Ann Arbor (USA). Dept. of Atmospheric and Oceanic Science
DOE Contract Number:
AC02-76EV01407
OSTI ID:
5306154
Report Number(s):
DOE/EV/01407-T1; ON: DE82016235
Resource Relation:
Other Information: Portions of document are illegible
Country of Publication:
United States
Language:
English