Evapotranspiration in millimeters accumulated for 1h, 3h, 6h, 12h, or 24h. Evapotranspiration (ET) is the sum of evaporation and plant transpiration from the Earth's land and ocean surface to the atmosphere. Evaporation accounts for the movement of water to the air from sources such as the soil, canopy interception, and bodies of water. Transpiration accounts for the movement of water within a plant and the subsequent loss of water as vapor through stomata in its leaves. Evapotranspiration is an important part of the water cycle.
Available intervals: 1h, 3h, 6h, 12h, 24h
Show the amount of evapotranspiration over the entire world.
Growing degree days (GDD), also called growing degree units (GDUs), are a heuristic tool in phenology. GDD are a measure of heat accumulation used by horticulturists, gardeners, and farmers to predict plant and animal development rates such as the date that a flower will bloom, an insect will emerge from dormancy, or a crop will reach maturity.
Show the accumulated growing degree days from the first of January on.
This is a special form of the GDD (Growing degree days). It is used for the date determination for the start of field work after the winter. Accumulation of the mean day temperatures starts on the first of January of the indicated year.
Show the grass land temperature sum along with the temperature at two meters.
Leaf wetness describes the amount of dew and precipitation left on surfaces. It is used for detection of fog and dew conditions and early detection of rainfall. The output is binary where 1 indicates wetness.
Show the binary leaf wetness index with a 30 minute resolution. It is clearly visible that leaf wetness is present in the evening, night and morning.