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<br />------------------- <br /> <br />4.5 <br /> <br />4.0 <br /> <br /> <br />- <br />E <br />~ <br />- <br />.. <br />:> <br />~ <br />0 <br />. <br />II <br />c: <br />0 <br />. <br />E <br />., <br />:> <br />0 <br />.D <br />0 <br />- <br />.c: <br />0- <br />"i 1.0 <br />::J: <br /> ,5 <br /> <br />o <br />-100 -90 <br />W <br /> <br />Fig, 3.5 <br /> <br /> <br />Modified smoothed profile <br />of Cascades to simulate <br />blockinO <br /> <br />-70 <br /> <br />-60 <br /> <br />- Trajectory for assumed concentration <br />of I ice particle per liter <br />-- - - Trajectory for assumed concentration <br />of 25 ice particles per liter <br />... . . . Trajector~ for assumed concentration <br />of 100 ice particles per liter <br /> <br />lX) <br />I-' <br /> <br />-- <br />-....... <br />.... <br />"" <br />" <br />. " <br />. " <br />. " <br />" <br />" <br />" <br />" <br /> <br />. <br /> <br />. <br /> <br />. . . <br /> <br />Smoothed profile <br />actual Cascades <br />W-E line <br /> <br />-50 <br /> <br /> <br />-40 <br /> <br />-30 -20 <br />It (kml <br /> <br />40 <br /> <br />50 <br />E <br /> <br />Predicted trajectories of growing precipitation particles as they fallout <br />over the Cascade Mountains in a westerly airstream, The streamlines used in <br />the calculations are those shown in Fig, 3,3 (simulated blocking), Number <br />at end of each trajectory gives the precipitation rate of water equi~alent <br />in cm hr-l originating from indicated trajectory. <br />