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<br />-14 r 5 <br /> <br />u <br />o <br />- <br /> <br />~ -8 <br />;j <br />- <br />o <br />l- <br />ll' <br />n. <br />E <br />lIJ <br />.... -5 <br /> <br />Fig. 4,3 <br /> <br /> <br /> <br />5 <br /> <br />20 <br /> <br />40 <br /> <br />-12 <br /> <br />/40 <br /> <br /> <br />/ <br />I /CO. <br /> <br />80 <br />/ <br />~"'-- //~//9.j <br />/ / <br />"--~-----.. ... // <br />._~-----//' <br />Cc:sc(1d~ <br />95 _____ Divide <br />---_95 I 95"""- <br />I~ ..' , <br />_.~___..-!-..-__~.__.__.-l,_~.1 . <br />~O 50 60 70. Eij::';";;;~Ii.J,tJ <br /> <br />-10 <br /> <br />40 <br /> <br />-4 <br /> <br />// <br />6~ <br /> <br />80 <br /> <br />-2 <br /> <br />o <br /> <br />, <br />Sea-Toe <br />Airport <br /> <br />_.1-___._.i. <br />10 20 <br /> <br />L <br />30 <br /> <br />Distcmce <br /> <br />{no'Jtical mi:es) <br /> <br />Isopleths for percentages of occasions on which water dominated over ice <br />in clouds over Cascade Mountains. Data is based on runs with continuous <br />particle sampl~r during flig~ts when winds were in the quadrant SW through <br /> <br />~~ <br />,-, <br />.... <br /> <br />NW, <br />