lergy 
land 
  
ration 
latent 
water 
ots of 
urban 
latent 
) In 
of 
ly in 
rate 
m, in 
r/land 
en in 
was 
on of 
s will 
t. For 
, and 
ct on 
t flux 
n that 
ig net 
flat or 
Ibedo 
other 
. least 
e heat 
f the 
with 
polo- 
Yellow Sea 
  
1.0 
  
  
2.0 
Figure 5. Estimated daily evapotranspiration from LAN DSAT TM with ancillary meteorological data. 
gical data. The surface parameters such as albedo, 
vegetation index, surface temperature, was calculated 
deom LANDSAT TM data. Unfortunately, the 
comparision of estimated results with measurements 
could not accompolished. To evaluate the accuracy of 
proposed method and employed empirical formulations, 
collection of a number of in-situ data in test area and 
further research will be required. 
References 
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transpiration by land cover changes. - À case study 
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Brest, C. L., and Goward, S. N., 1987. Deriving surface 
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International Journal of Remote Sensing, 8, pp. 351 - 
35 
367. 
Brutsaert, W., 1982. Evaporation into the atmosphere: 
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Jackson, R. D. and Hatfield, J. L., 1983. Estimation of 
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Jackson, R. D., 1985. Evaluating evapotranspiration at 
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Kotoda, K., 1986. Estimation of river basin 
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International Archives of Photogrammetry and Remote Sensing. Vol. XXXI, Part B4. Vienna 1996