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Last modified
7/28/2009 2:37:18 PM
Creation date
4/16/2008 10:30:31 AM
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Template:
Weather Modification
Title
Potential Opportunities for Precipitation Augmentation in the Eastern Tennessee Valley
Date
2/1/1988
Weather Modification - Doc Type
Report
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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 />Figure 5.19 <br /> <br />Figure 5.20 <br /> <br />Figure 5.21 <br /> <br />Figure 5.22 <br /> <br />Figure 6,.1 <br /> <br />Figure 6.2 <br />Figure 6.3 <br />Figure 6.4 <br />Figure 6.5 <br />Figure 6.6 <br />Figure 6.7 <br />Figure 6.8 <br />Figure 6.9 <br />Figure 13.1 <br />Figure :3.2 <br /> <br />Relationship between cloud base temperature and <br />daily precipitation measured above Chattanooga. <br />Best fit line is shown. . . . . . . . . . . . . 67 <br /> <br />Mean wind directions measured by rawinsonde ascents <br />through cloud layer for cold orographic cloud events <br />by 900 sectors. Mean for all cases shown at upper <br /> <br />right. II.................... 68 <br /> <br />Same as Fig. 5.20, but determined by echo motion <br />from Bristol radar (percent of hours available). 68 <br /> <br />Frequency of occurrence of rime observed on <br />Mt. Mitchell, North Carolina, by month <br />(from Hodge, 1969). . . . . . . . . . . . . <br /> <br />. 70 <br /> <br />Cloud base temperature predicted by GPCM model using <br />limitation of +14 oC heating per day for May 1981 <br />through 1987. .................... 75 <br /> <br />Example of the GPCM model output with all pertinent <br />parameters shown. ....... . . . . ,.' 77 <br /> <br />Percentage of soundings meeting limits imposed for <br /> <br />G P eM. . . . . . . . . .. .. .. .. .. .. .. .. .. .. .. .. .. .. 78 <br /> <br />Same as Fig. 6.3, but for May 198! through 1987. . . . 78 <br /> <br />~adius of cloud with dynamic potential as predicted by <br /> <br />GPCM.. .............................................. 80 <br /> <br />Bristol radar determined classification of convective <br />strength for May 1982 through 1987. 80 <br /> <br />Maximum echo tops by convective category shown in <br /> <br />f'igure 6.6.. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. .. 82 <br /> <br />Time ~f first echo as determined from Bristol radar <br />data for May 1982 through 1987. . 84 <br /> <br />Same as Fig. 6.8, but for time of last echo. .. . 84 <br /> <br />Reservoirs and areas augmented by cloud seeding.. 88 <br /> <br />Calculated zero precipitation flows for Douglas reservoir <br />inflows (bar graph - left axis) and corresponding weekly <br />correlation coefficients between Douglas inflow and <br />Asheville, North Carolina weekly precipitation (line <br />graph - right axis). ............... 90 <br /> <br />xi <br />
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