Based on the meteorological data in the middle areas of Shandong Province from 1980 to
2014, the reference crop evapotranspiration (ET0) was calculated by Penman-Monteith …

Based on the long-term climatic observational data including daily mean temperature,
maximum temperature, minimum temperature, relative humidity, wind speed and sunshine …

Reference crop evapotranspiration (ET0) is of importance to estimate crop water
requirement and make plans of irrigation scheme. Research on temporal and spatial …

Based on the daily data of 18 meteorological stations in Hainan Island from 1971 to 2010,
spatiotemporal change characteristics of ET0 of year and the four seasons were analyzed …

Based on daily meteorological data from 20 meteorological stations from 1966 to 2012, ET0
was calculated during crops growing season by using the Penman-Monteith equation. The …

Based on the FAO Penman-Monteith equation and the meteorological dataset in farming-
pastroral ecotone of northern China during 1961 to 2013, ET0 and its sensitivity coefficients …

Based on the long-term observed data of meteorological stations in Beijing, the reference
crop evapotranspirations (ET_0) for each month and each station were calculated, by using …

Reference crop evapotranspiration (ET0) was a key factor to estimate crop water
requirement and determine farming irrigation. The characteristics of ET0 and its major …

In order to determine reasonable crop irrigation system under changing climate in the
eastern plateau agricultural region of Qinghai province, reference crop evapotranspiration …

Based on the daily meteorological dataset during 1965 to 2006 from 10 meteorological
stations in Linghe basin of Liaoning province, the reference evapotranspiration (ET0) was …