Monthly mean total class A pan evaporation for the Australian continent between 1976-2005. Class A pan evaporation is useful for estimating evaporation rates and water need and use. Modelled by fittin
Reliable quantitative precipitation estimation with a rich spatiotemporal resolution is vital for understanding the Earth’s hydrological cycle. Precipitation estimation over land and coastal regions i
This dataset is about: Sub-daily meteorological observations of evaporation for Birao, Central African Republic. Please consult parent dataset @ https://doi.org/10.1594/PANGAEA.983618 for more informa
The potential evapotranspiration in Northwest China is calculated by the Penman-Monteith equation using meteorological data such as wind speed, sunshine duration, and maximum and minimum temperature.