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<br />APRIL 1990 <br /> <br />DESHLER, REYNOLDS AND HUGGINS <br /> <br />317 <br /> <br /> <br /> <br /> <br /> <br />2255 UTe <br /> <br />2300 UTe <br /> <br />2305 UTe <br /> <br />2310 UTe <br /> <br />:r: <br />I- <br />0:: <br />o <br />Z <br />w 20 <br />u <br />z <br />~ <br />(f) <br />Q 15 <br /> <br />.../1 <br /> <br />, . <br />, . <br />=, <br />'. , <br />'- <br /> <br />~;.1 i" <br /> <br />\ , <br />- - , <br />-. \ . <br />i ", <br />'-........ <br /> <br />-> <br /> <br />10 <br /> <br /> <br /> <br />dBZ <br />fE 0-12 <br />1IlI13-20 <br /> <br />/ <br /> <br />70 75 <br /> <br />(km) <br /> <br /> <br /> <br /> <br />2255 UTe <br /> <br />2320 UTe <br /> <br />2345 UTe <br /> <br />40 <br />I <br /> <br />" <br />~ ...... ~ <br />I ~...1 <br /> <br />" <br /> <br /> <br />. <br />'\ <br />N3 <br /> <br /> <br />z <br /><( <br />e 30 <br />0:: <br />W <br />:r: <br />(f) <br />u- <br />025 <br />:r: <br />I- <br />0:: <br />o <br />z <br />w20 <br />u <br />z <br />~ <br />(f) <br />Q <br /> <br />t <br />N3 <br />I <br />-.~\- <br />\ <br />\.~.. <br /> <br />, <br />.' . <br /> <br /> <br />~ <br />p. <br />I <br />N3 <br />\ <br /> <br /> <br />,~ <br />/ -'It.,''' <br /> <br />- . <br /> <br />. ',," <br />.':;-,B <br /> <br />';". \ <br />'J <br /> <br />810 89 <br />.2B +32 <br /> <br />'. <br /> <br />89 <br />+7 <br /> <br />dBZ <br />fE 0-12 <br />Ii! 13-20 <br /> <br />55 <br /> <br />60 <br /> <br /> <br />70 <br /> <br />75 <br /> <br />(km) <br /> <br />FIG. 20. (Continued) <br /> <br />rimed crystals 0.1-1 mm in size. In two regions of <br />cloud, needles and columns were observed along with <br />the rimed crystals. One of these regions was upwind <br />of SlO at 2314. The other was at about the same 10- <br /> <br />cation during the initial MOCA descent of the cloud <br />physics aircraft. <br />In Fig. 19a (using 3040 at 11 m s -1) and Fig. 19b <br />the interception of S 1 0 is at the downwind edge of a <br />