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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 /> <br />I <br />I <br />I <br />I <br />I <br />I <br />I <br /> <br />to TAR are documented by PPI's at 0803 and 0903 in Fig. 49. The coverage of higher intensity echo <br />ob"iously increased over this time period and TAR recorded its highest precipitation rate between <br />0900 and 0930. The decrease in SL W depth noted at RRS and TAR, between 0900 and 10 15, was <br />likely in response to the increase in snowfall rate during this period. <br /> <br /> <br />0.... u...,..... " <br />',- "'.:I'~ <br />...,_ )!.to <br />,,_. , ~ <br />~'__; 11. <br />e''''''''.....I'... <br />...-.. <br /> <br /> <br />0... _,..... <br />. ,,_ "';OJ-~I <br />....~ 151 J <br />"-' " <br />"._ .7. <br />c'-"'''''''' <br />".-... <br /> <br />-. <br /> <br />- , I~I <br />~" - <br />,- , <br />- <br />-.-. <br />~'- '" <br />.-... ~ <br /> ~ <br /> <br />- <br /> <br />- <br /> <br />-.-. <br /> <br />.,- <br /> <br />--'.' <br /> <br />~ <br />"' <br />o <br /> <br />~ <br />"' <br />o <br /> <br />FIgure -/9. Radar PPl's taken 01 0803 (left) and 0903 (rtght) on 7 February /99-/, The target slle <br />rTAR) 1$ noted b.t' the small box in the northeasl quadrant. <br /> <br />The radar coverage during the middle portion of the field experiment is shown in Fig. 50. <br /> <br /> <br />0_. 1ol.4?......~...-.,..~ <br />'>-' 11:1?'11 ...., . <br />...-, ]1571 <br />"'_, t' <br />".-. '" <br />.,............."..... <br />,'._.. <br /> <br /> <br />__. tt.-e7..... <br />._ 1l:'1';~ <br />....~ . , <br />.'- ,. <br />"PI._ f7. <br />c"._.4.0.~\.. <br />.-._... <br /> <br />. "_0 lW'.i <br />. ....~. - <br />- , <br />-,. <br />... <br />~,- <br /> <br /> -. l~lI <br /> ..... - <br /> - , <br /> -.. <br /> -- <br /> ....... <br /> ..... '" <br /> ,-,.. ~ <br />. -, ~ <br /> <br />."-; <br />'-'" <br />. ., <br /> <br />- <br />"' <br />o <br /> <br />" - <br />. "' <br />o <br /> <br />FIgure 50, Radar PPI's taken at /007 (left) and / /03 (right) an 7 February /99-/. <br /> <br />The echo intensity at 1007 was similar to that at 0903, and reflects the generally higher precipitation <br />rate during this portion of the stonn. By 1103 the coverage of Level 50 echo had decreased <br /> <br />67 <br />