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<br /> <br />,iif'~ """f~~>j"'?""''f'''f'~~.. <br />.~;...-;.;. <br />'><';;",~ '. . <br /> <br />'~~~"iit;;, <br /> <br />p <br />I <br />I <br />I <br />I <br />I <br /> <br />'1f:/:JfP'P' <br /> <br />I <br />I <br />A <br /> <br />, <br />, <br /> <br />.' <br /> <br />;p" <br />,0 <br /> <br />" <br /> <br />'7 <br /> <br />A <br /> <br />c <br /> <br /> <br /> <br /> <br />':'1---- <br />:"..W'" "';?' <br /> <br />LmEHll <br /> <br />A. Cub1cal mass of air exl"A.......g <br />trOll J.OOCIIIIb to 2OQab. <br /> <br />ChaZIge or sbape neces8Q7 ror: <br /> <br />B. l1Dcb or prec1p1tat1oD. <br />C. 2 1DCbes or prec1p1tation. <br />D. 5 1DCbes of prec1p1tation. <br />E. 2 1DCbes or precip1tat1on with <br />" v1Dd direction constant with <br />bs1ght toward pos1t1ve 11 wb1ch <br />1Dcreasee l1De....l,y trom 0 to 50 <br />kDots _lID J.OOCIIIIb 8IId 2OQab. <br /> <br />FIGURE 2-2.-Change in shape of a cubical mass of saturated air required to produce various rainfall amounts, assuming <br />a 1,OOO-mb. temperature of 70" F. and a pseudoadiabatic lapse rate. <br /> <br />2.3.8 Other verticltls such ltS HI. could be se- <br />leered, ltnd A integrated both verticltlly ltnd <br />longitudinltlly. This procedure would provide ltd- <br />ditional profiles of C, or precipitation, which could <br />be added. The composite shape of C would depict <br /> <br />8 <br /> <br />the preeipitlttion profile over the barrier. <br />2.3.9 ,Vind vectors over the barrier would be <br />required to eVltluate the diagram (fig. 2--3). The <br />precipitation-formation profile, A, would have to <br />be integrated for different forms of water; i.e., <br />