Astronaut Scientific Debriefings, 1962-1963
NASA-UAP-D015 · page 43 of 216
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LOS ALAMOS SCIENTIFIC LABORATORY UNIVll:llalTY 0,, CAL.1,,0IINIA LOe ALAM0e, NIEW MUICO • 1'0z nr. Jocelyn Gill DATBz July 13, 1962 For a horizontal path (sin 8 • 0) te.nsent to the baae of a layer (path No. 3) we ·note that y << l in the contributing region, hence, can get an approximate form l ~r. ~ ex, Y2 N • RPo •e ccy (7) O which has the value ~ N•\J 2 Po (8) Here Po is the density at the base of the layer, as in eqµation (6). 'I An astronaut's view thru a layer :from above would see twice the path computed I by equation (7), ·giving N3 • Po ✓ 2nRY molecu.les/-cm2 (9) f • Aline of sight tangent to the earth and passing thru a layer at base altitude H (path No . 2) will have . .1!J., N- ~y [pl e y J (10) ..fu. and we note that [P1. e ~] is the density at H1 , the base of the layer, which we set eqµal to Po as in equations (6) and (9), RY • ~ N,a • Po -L • Po - (11) 2H1. r-