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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 />Fig. 3,8 <br /> <br />100 <br /> <br />c: <br />o <br />- <br />o <br />- <br />"0. <br />'u <br />f <br />~ <br /> <br />'0 <br />"" <br />=' <br />- <br />o <br />c <br />o <br />- <br /> <br />10 <br /> <br />01 <br />C <br />'0 <br />CD <br />CD <br /><<I) <br /> <br />'0 <br />.u <br />~ <br />- <br />"" <br />o <br />.l: <br />- <br />'i <br /> <br />1.0 <br /> <br />CD <br />- <br />G <br />"" <br /> <br />c: <br />o <br />:0:: <br />o <br />- <br />"0. <br />'u <br />CD <br />.. <br />Q. <br /> <br />0.1 <br /> <br />- <br />o <br /> <br />o <br />- <br />o <br />0: <br /> <br />,01 <br /> <br />- 87 - <br /> <br />6. <br /> <br />Altitude above MSL at <br />which precipitation oriQinates <br /> <br /> <br />6. <br /> <br /> <br />b.b. <br /> <br />6.:: 1.5 km <br />0:: 2.0km <br />o :: 2.5 km <br /> <br />b. <br /> <br />b. <br /> <br />9 <br />b. <br />OA <br /> <br />CD <br />Cb <br /> <br />b. <br /> <br />o <br /> <br />b. <br /> <br />o <br />~ <br /> <br />~ <br /> <br />o <br /> <br />o <br />&:l <br /> <br />o <br />o <br /> <br />o <br /> <br />b. <br /> <br />o <br /> <br />o <br /> <br />o <br /> <br />o <br /> <br />o <br /> <br />o 0 <br /> <br />o <br /> <br />o <br /> <br />o <br /> <br />2 <br /> <br />3 <br /> <br />4 <br /> <br />5 <br /> <br />Ratio of horizontal displacement of precipitation from <br />point of oriQin to Qround (artificially seeded I natural easel <br /> <br />~odel predictions of the effects of ice particle concentration <br />on precipitation rate and horizontal pathlength of precipitation <br />for westerly flow (simulated blocking) over Cascade Mountains. <br />"Artificial seeding" refers to a concentration of ice particles <br />of 25 or lOOj! -1 and "natural" refers to a concentration of II -1. <br />