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<br />6.3.3 <br /> <br />6.3.4 <br /> <br />6.3.5 <br /> <br />6.3.6 <br /> <br />6.4.1 <br /> <br />6.4.2 <br /> <br />6.4.3 <br /> <br />6.4.4 <br /> <br />sive locations of the AgI seeding curtain, on 20 <br /> <br />February 1979 case study. . . . . . . . . <br /> <br />Typical power spectra of lateral (v') and true air- <br /> <br />speed (TAS'), on 20 February 1979 case study. <br /> <br />A sample of analog traces of longitudinal (u') and <br /> <br />la tera 1 (v') wind components <br /> <br />Autocorrelation functions of longitudinal (u') and <br /> <br />lateral (v') wind components, from data presented in <br /> <br />Fig. 6.3.4 <br /> <br />L <br />Calculated values of variances for different T (solid <br />1/3 <br />lines) by the LTD model, and S (dashed line) by the <br /> <br />Da tche lor's S approach when 0 = Y = 125 m <br /> <br />Flight track of the K/A on 8 February 1978, over the <br /> <br />Sierra Nevada Mountains <br /> <br />Aircraft sounding for 8 February 1978 case study. <br />Horizontal wind speed (V), potential temperature (8) <br /> <br />and indicated turbulence (IT) are shown. . . . . . . <br /> <br />Vertical cross section along the 60 0 radial over the <br /> <br />Sierra Nevada Mountains. The light line, with arrows <br /> <br />corresponding to 5 min intervals, represents the K/A's <br /> <br />flight tracK. Wind direction, isotach and isentrope <br /> <br />analysis, and observed AgI plume are also indicating. <br /> <br />Traces of potential temperature (8 '), longitudinal <br /> <br />(u'), lateral (v'), and vertical (w') wind components <br /> <br />with respect to the wind direction, for 8 February <br /> <br />1978. They correspond to the flight segment a t I tun <br /> <br />. <br /> <br />xli <br /> <br />. <br /> <br />159 <br /> <br />161 <br /> <br />. <br /> <br />163 <br /> <br />. <br /> <br />165 <br /> <br />. <br /> <br />168 <br /> <br />.' <br /> <br />173 <br /> <br />., <br /> <br />174 <br /> <br />. <br /> <br />175 <br /> <br />. <br /> <br />. <br /> <br />. <br />