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<br />"! <br /> <br /> <br />JULY, 17 1979 2100 GMT <br /> <br /> <br /> 500 <br />&> <br />E <br />\OJ <br />II: 700 <br />;J <br /><f) <br /><f) <br />\OJ <br />II: <br />... <br /> 900 <br /> <br />Rador echo <br />locations <br /> <br />~ <br />?/ /... <br /> <br />79071721 <br /> <br />300 <br /> <br />/~ <br /> <br />20 Lot1gltude <br /> <br />-.5 A~G -16.0 <br />\1.1 A~G 11.1 <br /> <br />-.1 flYG -16.5 <br />16.7 flYG 11.5 <br /> <br />21. 9 A~G <br />16.3 flYG <br /> <br />-2.6 <br />9.1 <br /> <br /> <br />· ti . <br />~~- ,'-'~~~\\",,;,~./ <br /> <br />3-D rLOW rlELOS <br /> <br />101f\L r\ ELOS <br />300 IMBI <br />W "IN -16.7 I1Ax <br />v"IN 6.3 t1Ax <br /> <br />13.9 RVG -7.9 <br />21. 3 A~G 15.9 <br /> <br />3.D <br />2.S <br />z 2.0 <br />a: 1.5 <br />a:: \.0 <br />D.S <br />D.D <br /> <br />79/07/\7 1800 10 79/07/16 0300 IllIl1l <br />lOlf\L r\ ELO <br /> <br />16 <br /> <br />102.2 102.0 101.8 101.6 101.1 <br />LONG. <br /> <br />101.2 101.0 100.8 <br /> <br />R' . \6. .\2 IINI N' 22 <br />COCL or VRR. - .66 VOl.Lft:. 1.221:'07 <br /> <br />Figure 3.4_Three-dimensional wind vector analysis (a) conceptual model of airflow and radar echo and <br />(b) structure at 2100 G.m.t.. July 17. 1979. showing the correlation between lifting and deep <br />convective cloud growth. <br /> <br />SOD IMBI <br />-12.7 I1AX <br />6.0 I1AX <br /> <br />700 IMBI <br />-32.0 I1Ax <br />3.5 I1Ax <br /> <br />900 IMBI <br />W "IN -25.5 I1Ax <br />V "IN 1.6 t1AX <br />