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Propagation Effects Handbook for Satellite Systems - DESCANSO ...

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. .<br />

The equivalent heights <strong>for</strong> oxygen, hO, and water vapor, hW, are<br />

determined from:<br />

hw =<br />

[<br />

2.2 +<br />

hO=6km<br />

hO=6+<br />

<strong>for</strong> f < 57 GHz<br />

40 km <strong>for</strong> 63 < Y < 350 GHz<br />

(f - 118.7) 2<br />

+ 1<br />

(6.2-10)<br />

3 1 1<br />

(Y - 22.3) 2<br />

km<br />

+ 3 ‘(f- ‘(f- 1<br />

183.3) 2<br />

<strong>for</strong> f c 350 GHz<br />

+ 1 323.8) 2<br />

+ 1<br />

(6.2-11)<br />

The total slant path gaseous attenuation through the atmosphere, AE,<br />

is then found.<br />

with<br />

For () ~ 10°:<br />

For 6 < 10°:<br />

A~ =<br />

.—ho<br />

h,<br />

+<br />

Y. ho e VW hw<br />

sir 0<br />

YO ho VW hw<br />

AE=—<br />

9 (ho)<br />

+<br />

9(%)<br />

g(h) = 0.661% + 0.3394 ~ + 154h5.5<br />

d<br />

h~<br />

4250<br />

x = sin2El + —<br />

where h is replaced by ho or hW as appropriate.<br />

6-15<br />

dB<br />

dB<br />

(6.2-12)<br />

(6.2-13)<br />

(6.2-14)<br />

(6.2-15)

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