FRESENIUS ENVIRONMENTAL BULLETIN, cilt.27, sa.12, ss.9500-9508, 2018 (SCI-Expanded)
Evapotranspiration (ET) is one of the most difficult processes in nature. The most accurate and reliable method to determine ET is lysimeter, which is
difficult, expensive and time-consuming. On the
other hand, ET can be estimated using reference crop
evapotranspiration (ETo) and crop coefficient (kc).
easily Many ETo equations using meteorological
data have been developed. The most widely accepted
equation for ETo is FAO-56 Penman-Monteith
(FAO-56 PM) equation. However, FAO-56 PM
equation needs numerous meteorological data and is
hard to measure for farmers. For this reason, equations which need less meteorological data have been
gaining importance. Characteristic Mediterranean
climate prevails in coastal areas of Antalya, Turkey.
In the present study, long term data (1985 to 2015)
obtained from meteorological stations was used to
compute ETo in Antalya. Seven different ETo equations (Penman, FAO 24 Penman, Hargreaves, Turc,
Priestley-Taylor, FAO 24 Pan, Christiansen Pan)
were compared with FAO-56 PM. It was shown that
the Turc equation gives results close to FAO-56 PM
equation.