Abstract

Abstract During May and June of 1985, an experiment to study mesoscale convective systems (MCSs) was carried out in central Kansas and Oklahoma, using many of the latest measurement technologies in the atmospheric sciences. Among these were three 50-MHz radar wind profilers. Two cases of mesoscale squall-line systems are used to describe profiler performance in the highly convective environment of the United States High Plains in early summer. The 10–11 June squall-line system was intense and well organized, and passed over the profiler sites near Liberal and McPherson, Kansas; the 26–27 June system was less coherent and was studied when it passed over the Norman, Oklahoma profiler. For the stronger event, both profilers supplied good time-height coverage of the horizontal winds during the pre- and post-squall-line periods, but could not resolve them well while the strongly convective line was overhead. In contrast, the Norman profiler supplied good horizontal-wind information throughout the weaker system...

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