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<br />- <br /> <br />where R(s) is the rainfall rate measured at a distance (s) along the <br />aircraft flight path and where the integral extends over the ith <br />pass. <br /> <br />2. Weighted average positions of the rainfall (5i) and standard <br />deviations (oi2) from these positions are calculated for each pass <br />accord i ng to the formul as <br /> <br />!;. = L J s R( s) ds <br />1 T. <br />1 <br /> <br />2 <br />Di = <br /> <br />I <br />T. <br />1 <br /> <br />J (5 - <br /> <br />2 <br />Si) R( s) ds <br /> <br />3. Between passes i and i + 1, the area integral of the rainfall <br />rate is estimated as <br /> <br />AI i = ~ 2lf TiT i +( i (j i <br /> <br />This would be an exact result if the rainfall were distributed in <br />a Gaussian distribution of the form <br /> <br />R(x.y) = Ro exp (- /2 -~) <br />20" 2(1 <br />X Y <br /> <br />For a uniform distribution of rainfall within a circle or an ellipse, <br />the same formula would hold with a constant of I3(T/2) = 2.72 instead <br />of ..[2:; = 2.51; sl ight1y different constants would apply to other <br />geometries. <br /> <br />4. AER is evaluated from <br /> <br />~ <br /> <br />N - I <br />AEIR~ == L: <br /> <br />1 = I <br /> <br />A . (t. - t. ) <br />1 1 + I 1 <br /> <br />where ti is the time of the ith pass and N is the total number <br />of passes at the +10 oC level. <br /> <br />21 <br />