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<br />USBR STEADY STATE CONVECTION MODEL PROGRAM <br />AMAOO 09/05/73 <br /> <br /> RADIUS C/S CLOUD TOP RAINFALL MA:>=: SEEI'AB I L ny <br />I PRESS. TEMP. HEIGHT MSL PER CLOUII UPDR TOP HEIGHT RAIN <br />i (KM) (MB) (C) (1(1'1 ) O(FT) (MM) (INCH) (M,-'S) (KM)(KFT) (IN) <br />I~ OBSERVED OR HAND CALCULATED CLOUD BASE <br />I <br /> 0.50 NAT 570. -1.6 4.:3 15.7 0.0'5 0.002 6.0 <br />I MOD 570. -1.6 4 ,=> 15.7 0.05 0.002 6.0 0.0 0.0 0.000 <br /> .v <br />~\ <br />I 1. 00 NAT 3:30. -22.8 8.1 26.4 5.1::: 0.204 14.0 <br /> MOD 310. -:33.6 9.6 31.1 :3.67 0.342' 15.7 1.5 4.:3 O. 1:38 <br /> 1.50 NAT 250. -40 . '3 10. '3 35.,3 13 .21 0.520 21.0 <br /> MOD 220. -47.2 11.7 38.1 14.9,3 0.588 23.7 0.9 2.8 0.068 <br /> 2.00 NAT 210. -49.5 12.0 39.1 17.17 0.676 25.7 <br /> MOD 180. -55.6 13.0 42.3 1'3.12 0.753 :30.9 1.0 ~ .-, 0.077 <br /> .~ ..,:. <br /> 2.50 NAT 180. -55.6 1:3.0 4'=> ':' 20.51 0.807 31.3 <br /> &;;;;, . "-' <br /> MOD 160. -59.7 13.8 44.7 21 .5~, 0.849 37.5 0.7 2.4 0.041 <br /> :3.00 NAT 170. -57.5 13.4 . 4::::.5 22.08 0.86'3 35.3 <br /> MOD 140. -6:3.:3 14.6 47.4 24.21 0.953 41.E, 1 ';:. 4.0 o . 0:34 <br /> .... <br /> 3.50 NAT 150. -61.'3 14.2 46.1 24.54 o . '366 38.7 <br /> MOD 1:30. -.::.4 .8 15.0 48.'3 25.75 1.014 44.9 0.9 2.':;' 0.047 <br /> 4.00 NAT 150. -61 .9 14.2 46.1 24.'39 0.984 41.0 <br /> MOD 120. -66.4 15.5 50.5 ,27.0';' 1.067 48.2 1.4 4.5 0.083 <br /> ..00 NAT 120. -66.4 15.5 50.5 :33.49 1..319 67.6 <br /> MOD 120. -66.4 15.5 50.5 :32.61 1.284 77 .1 0.0 0.0 -- . 035 <br /> <br />CLOUD'BASE PRESSURE <br />CLOUD BASE HEIGHT <br />SUB CLOUD MIXING RATIO <br />SURFACE CONV. TEMP., <br />CLOUD COVER <br />'nop <br /> <br />?:3 O. MB <br />2.8 KM 9174. FEET <br />10.76 GM/KG <br />29 .6 C :35. F <br />67. PERCENT <br /> <br />" <br />I <br />I <br /> <br />inches (column 8) ofrainfall under natural <br />conditions. If seeded, however, it could <br />produce .342 inches (column 8), or an <br />increase of .138 inches (column 12) over <br />the natural cloud. The model also says <br />that seeding large clouds, above 4 kilo- <br />meters in radius, would cause a decrease <br />of rainfall,. 035 inches (column 8). <br /> <br />I~ <br />I <br />! <br /> <br />In addition, many sophisticated electronic <br />instruments and more conventional meas- <br />uring tools are used to monitor the heart- <br />beat of weather systems and to assist in <br />recognizing seeding opportunities. <br /> <br />If anyone measurement tool could be <br />termed as a key to the qualitative and <br />quantitative understanding of weather <br />modification effects, it would be radar. <br />The unique characteristics of radar have <br />already established it as the operational <br />eye of Skywater research. <br /> <br />Radar units, modified for specific purposes <br />and teamed with computers, are Icapable <br />of watching the formation of rain within a <br />cloud. The image on the screen cannot <br />only track a storm or storm system but <br />can also inform a trained observer of the <br /> <br />4 <br />