geo-referenced (a 
layers) for easy oy TEE e— -— 
ayers included 3 : 
perature, eight 3870 
e layer of soil 
| an unique 
of spatial and 
soil moisture. 
which has been 
gically active 
ershed and also 
s with strong 
ace and time 3860 
3865 © 
Northing (km) 
ent measures 
whose intensity Mi M us \ 
S temperature. 570 580 590 600 
92 experiment Easting (km) 
s temperature 
An data (b) June 13, 1992 
a series of two 
enerated using 
such maps for 
e maps clearly 
poral variation 
the watershed. 
rature data of 
tershed can be 
ions of low 
909 K) on the 
re separated by 
r temperatures 
je of 2509 K). 
1e brightness 
ally stronger 
ast day (figure 
reased all over 
1aracterized by 
at is observed 
no significant 
f brightness 
  
  
Northing (km) 
  
  
  
end of the 
ation of cold 
, changed to 
> on June 18, - 
and temporal £ 
ation, and will vd 
soil moisture. = 
zZ Es pu 
an established 2. | 
ve brightness ÿ = 
isture. For the : À € 
jatershed, the 
en employed 
soil moisture 
en developed Eosting (km) 
re and field , ; ; ; ture (in © K) acquired by 
isti Figure 2. Two dimensional contour maps of multi-temporal brightness temperature (i db 
fe. Statistical ESTAR Sides the Washita'92 hf Patterns of brightness temperature variation observed within 
ignships howe the shaded areas closely follow the distribution of sand, loamy fine sand, and fine sandy loam as shown in 
noisture from figure 7 : 
ire watershed.