ite of the 
:n et al., 
'urrently the 
gen band 
model in 
t are 
LLSSF 
sentedas 
ted surface 
Wavelength (nm) 
Figure 6 : NLLSSF for the water vapor at the polo field. 
i 
800 
\ygen band 
950 1000 1050 
Wavelength (nm) 
er vapor. In 
agnitude. to 
Conel et al., 
1987) and 
isured and a 
ion to water 
surface leaf 
ipectrum for 
overlapping 
and figure 8 
Figure 7 : Spectral fit for water vapor at the golf course.