454 
(iu)Oz 
CÛ 
O 
0 
a 
T) 
X> '3 
S § 
CS o 
■® S 
J « 
•o U 
§ E 
U 
o 3 
CO 0 
U C/3 
3 c 
es — 
Q 
^ U 
l’S 
ÿ s 
?r ^ 
height, and the 
Instead, values 
CONCLUSIO 
The resultant n 
plotted in decit 
seven of the ve 
(in dB), and the 
rougher than tl 
(R^) is 0.79 fot 
We are now pr 
investigate the 
Second, we pia 
the empirical n 
ACKNOWLE 
We would like 
deploying con 
described in th 
contract with tl 
REFERENCE 
Arya, S. P., 1 
Meteorology. 
Blom, R. G., 5 
polarizations f 
Geosci Remote 
Brutsaert, W. 
Meterologv . Tl 
Evans, D. L., F 
geologic mapp 
Greeley, R., G 
S., Zebker, H., 
Mechanica 2: 
Greeley, R., D 
VanZyl, J„ W: 
Report 4378, V 
Greeley, R., A 
Thouvenot, E. 
J. Geophys. Re