Crop water requirement mainly depends
upon crop sowing date, crop growth stages, crop duration and climatic
conditions during the growing season of an individual crop. A good estimate of evapotranspiration is essential for water balance irrigation scheduling and
water resource planning and management. Since, direct measurement of ET0
is difficult and time consuming, so most common practice is to estimate ET0
from meteorological data available for the area employing empirical equations.
There are numerous evapotranspiration equations developed and used by
researchers but still there is confusion in selecting the reliable
evapotranspiration estimation method for the area concerned. Some authors
compared estimates of different ET0 estimation methods for different
regions of the world. Al-Ghobari compared five different methods: FAO-Penman,
Jensen- Haise, Blaney and Criddle, Pan Evaporation and calibrated FAO-Penman
for four areas under local conditions of Saudi Arabia. The results showed that
estimated ET values were highly correlated with measured evapotranspiration
values. (Read more)

No comments:
Post a Comment