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evapotranspiration B-climate-nature
is O
the O
transfer O
of O
energy O
between O
the O
Earth B-climate-nature
's I-climate-nature
surface I-climate-nature
and O
the O
atmosphere B-climate-nature
and O
it O
is O
the O
most O
productive O
mechanism O
of O
communication O
between O
the O
hydrosphere B-climate-nature
, O
lithosphere B-climate-nature
and O
biosphere B-climate-organisms
. O
This O
study O
focuses O
on O
predicting O
potential B-climate-properties
evapotranspiration I-climate-properties
in O
Golpayegan O
basin O
as O
a O
response O
to O
climate O
change O
. O
For O
this O
purpose O
, O
six O
algorithms O
including O
Hargreaves B-climate-models
- I-climate-models
Samani I-climate-models
, O
Thornthwaite B-climate-models
, O
Romanenko B-climate-models
, O
Oudin B-climate-models
, O
Kharrufa B-climate-models
and O
Blaney B-climate-models
- I-climate-models
Criddle I-climate-models
and O
also O
, O
Penman- B-climate-models
Monteith- I-climate-models
FAO I-climate-models
as O
a O
standard O
algorithm O
, O
were O
used O
for O
estimating O
the O
potential B-climate-properties
evapotranspiration I-climate-properties
. O
The O
results O
showed O
that O
the O
Hargreaves B-climate-models
- I-climate-models
Samani I-climate-models