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Margaret A. LeMone, Fei Chen, Mukul Tewari, Jimy Dudhia, Bart Geerts, Qun Miao, Richard L. Coulter, and Robert L. Grossman

circulations with maximum amplitude above the CBL on 20 June. Mesoscale structures on 22 June are overwhelmed by the rolls. On 17 June, there are some weak warm upwelling regions and cool downwelling regions in the CBL; but little mesoscale circulation evident in the cross section in Fig. 11a , with maxima and minima above the CBL at 1800 UTC, consistent with the ambiguous observations in Figs. 9 and 10 . There is a large response to the Wichita urban heat island ( Fig. 12 ) on 30 May (distance = 20 km

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