Conclusions
The
wide and varying discrepancy in ET values calculated using the two different
methods compared in this study highlights the necessity for using more accurate
formulas that take into account the specific
conditions observed at the given location. While using the alfalfa-specific
Kimberly-Penman equation as a standard across the RAWS network may be useful
for standardizing the Keech-Byram index for comparison across stations, it may
not be the most accurate method for measuring actual ET at most sites in which
RAWS stations are located. The four weather stations that were used in this
study are located at different elevations and different ecosystems; perhaps
there is no one formula that would provide accurate ET values for all four
sites. Local, direct ET measurements would be required to derive an accurate
formula for each site. Future studies will involve calculating ET using
different values for ra and rs
that more accurately represent the conditions found at each weather station
location and comparing those to ET values calculated using MODIS data.