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<br />SEEDING A TYPICAL AlR-MASS STORM <br /> <br />:0000 FT <br /> <br />--'---:'\ <br />......... <br /> <br /> <br />~r <br />,r-- <br />~ <br /> <br />~ <br /> <br />JO.OO'JFT. <br /> <br />76-20.000 FT. <br /> <br />CLOUD TOP SEEDING <br /> <br /> <br />10,000 FT <br />MSl <br /> <br />MATURE <br />STORM CELL <br /> <br />'COOn <br />"SL <br /> <br />--- . <br /> <br />CLOUD BASE <br />SEEDING <br /> <br />, <br /> <br />UPDRAFT AREA <br /> <br />l ooa n <br />YSL <br /> <br />-' <br /> <br />. . Fig. 2 <br /> <br />at times. The updraft locations important to the hail process on these type of cloud systems are along <br />a line on its front side, running from a few miles to many miles in length. Other times, the best seeding <br />area may be around only one end of the line. Multi-celled lines may also appear as a remnant of "a <br />weakened squall line or as part of a line of storms associated with fronts, surface troughs and <br />thunderstorm outflows. <br /> <br />8 <br />