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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International Archives of Photogrammetry and Remote Sensing. Vol. XXXI, Part B4. Vienna 1996