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<br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I, <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />Table 5. - Daily precipitation frequencies for each of a wet, normal and dry <br />winter at station group GP5.* <br /> <br />PRECIPITATION FREQUENCY <br /> <br />Stat ion <br />group GP5 Winter Condition <br />Preclpltatlon Wet (1982-83) (1981-82) Dr Ll..!J80-81 ) <br />range (in) Nor'm <br />0 135 159 156 <br />>0 - 0.2 24 14 14 <br />>0.2 - 0.4 8 4 6 <br />>0.4 - 0.6 5 2 2 <br />>0.6 - 0.8 2 1 2 <br />>0.8 - 1.0 1 1 <br />>1.0 - 1.5 4 <br />>1.5 - 2.0 1 <br />>2.0 - 2.5 1 <br />Total cases 181 180 181 <br /> <br />*Precipitation measurements were generally taken at 1800 local. <br /> <br />Given in tables 6-12 are the frequency counts with stratification by pre- <br />ci pi tat i on category, season type and 500 mb temperature. The temperature <br />intervals selected, -5 to -10 oC, -11 to -20 oC, -21 to -26 oC, and -27 oC <br />and colder, are likely to be of importance to the index-ation of cloud seed- <br />ability (Mielke et al., 1971). The results for the southern mountain sites, <br />obtained by extrapolation with the Winslo~' sounding, must be interpreted with <br />due regard to the distance and intervenin~J barrier presence. Several important <br />features were noted as follows: <br /> <br />1. On the Mogollon Rim most cases with precipitation amount <br />~ 0.2 inch occurred with 500 mb temperatures in the -11 to -20 oC <br />interval. This was true in wet, normal and dry winters. A distant <br />second in counts was the temperature interval -21 to -26 oC (same <br />precipitation interval). Counts for the Mule and Chiricahua <br />Mountains were generally lower. <br /> <br />35 <br />