Laserfiche WebLink
<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 4.16 (a) Mesoscale convective complex approaching the <br />eastern TVA region on 5 April 1983 as seen on a <br />combined visible/infrared image. Infrared super- <br />imposed for visible at CTT1s colder than -32 oC. <br />,(b) Total 4-day preci~itation total over southeast <br />United States from a series of MCC1s (from Fritsch <br /> <br />et al., 1986). ................... 27 <br /> <br />Figure 4.17 Same as Fig. 4.14, only showing results for month of <br />March for each year. Percentages shown beneath each year <br />are percentages of normal precipitation above Chattanooga <br />for March of that year. . . . . . . . . . . . . 28 <br /> <br />Figure 4.18 <br /> <br />Figure 4.19 <br />Figure 4.20 <br />Figure 4.21 <br />Figure 4.22 <br /> <br />Same as Fig. 4.17, only for synoptic/mesoscale <br />classifications. . . . . . . . . . . 28 <br />Same as Fig. 4.17, only for April. . 30 <br />Same as Fig. 4.18, only for April.. . 30 <br />Same as Fig. 4.17, only for May. . . . . 31 <br />Same as Fig. 4.18, only for May. . 31 <br /> <br />Figure 4.23 Bristol radar areal coverage with inner dark range ring <br />at 120 nmi and outer ring at 240 nmi. Location of four <br />primary target areas and rawinsonde sites also <br /> <br />. annotated. ....................... 34 <br /> <br />Figure 4.24 Number of hours having radar echoes by month for each <br />year as observed by Bristol radar. Percentages atop each <br />bar are the percent of the total hours available each <br />month. The percentages shown to right of each month are <br />the averages for the 6-year study. ......... 34 <br /> <br />Figure 4.25 Same as Fig. 4.24, only showing the number of days per <br />month having radar echoes. ............. 36 <br /> <br />Figure 4.26 Average number of echo hours per day with echoes. . . 36 <br /> <br />Figure 4.27 Percent frequency of radar echoes classified as either <br />convective or stratiform. See text for details. .. 37 <br /> <br />Figure 4.28 Pro9ability of occurrence of cloud base temperature <br />colder than the indicated temperature for upper air <br />stations in the vicinity of the TVA region. The <br />analysis represents all soundings taken during May <br />from 1981 through 1987. Soundings were generally <br />taken twice daily, at 0000 and 1200 GMT (0700 and <br /> <br />1900 e.s.t) . . .. ............... 40 <br /> <br />vii i <br />