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began to pick up, and in about 5 rninut,es the wiild increasedfrom about 10 1n.p.h. to about 50 m.p.h. and the ocvan becameextremely rough. The high winds (about, 50-55 n1.p.h.) continued,developing waves of nearly 10 feet. The wind shifted from eastt o south and blew all night a t a b o u t 50-55 m.p.h., although tllcrain did not get above a heavy drizzle.Neither the LIiami WBO radar (the new WSR-57) northe reconnaissance aircraft radar could pick up any wallcloud around the eye during t'he night
began to pick up, and in about 5 rninut,es the wiild increasedfrom about 10 1n.p.h. to about 50 m.p.h. and the ocvan becameextremely rough. The high winds (about, 50-55 n1.p.h.) continued,developing waves of nearly 10 feet. The wind shifted from eastt o south and blew all night a t a b o u t 50-55 m.p.h., although tllcrain did not get above a heavy drizzle.Neither the LIiami WBO radar (the new WSR-57) northe reconnaissance aircraft radar could pick up any wallcloud around the eye during t'he night
pressure 1001.0mb, tendency -0.6 mb, then steady temperature 22OC,and a heavy drizzle. The storm remnant was without asource of kinetic energy (Malkus et al., 1959) and waspractically "run down."USAF reconnaissance confirmed dissipation of Bonnyto no more than a minor depression at 1800 GMT, July 8,but a stratified cloud vortex was still very much inevidence on ESSA-6 pictures (fig. 5). The reconnaissanceobserver summarized: "NO RADAR RETURNS NOSGNFT CLDS ABV 80 CLD TPS ABV 400 NEGCENTER DATA
pressure 1001.0mb, tendency -0.6 mb, then steady temperature 22OC,and a heavy drizzle. The storm remnant was without asource of kinetic energy (Malkus et al., 1959) and waspractically "run down."USAF reconnaissance confirmed dissipation of Bonnyto no more than a minor depression at 1800 GMT, July 8,but a stratified cloud vortex was still very much inevidence on ESSA-6 pictures (fig. 5). The reconnaissanceobserver summarized: "NO RADAR RETURNS NOSGNFT CLDS ABV 80 CLD TPS ABV 400 NEGCENTER DATA
