The word "evapotranspiration" is correct and usable in written English.
You can use it when referring to the movement of water in nature, usually used in the context of climates and geography. An example sentence might be: "The evapotranspiration of water in the desert is much higher than in other climates."
The forest, by recycling the water that falls on it through evapotranspiration, plays an important part in this system.Between a quarter and half of the water molecules that fall in the western Amazon have previously fallen on the rainforest.
The only water truly lost in a hydrologic system is through evapotranspiration, since no one can make further use of it once it is in the atmosphere.
They calculate how much water will be available if the table is not to fall, decide which crops to grow and estimate how much water they will use, bearing in mind that about half will go in evapotranspiration.
These two processes, known in combination as evapotranspiration (ET), tend to be overlooked by water policymakers.
The images they beam back to earth can be used to generate data about land cover, surface temperature, vegetation and evapotranspiration.
Cutting down trees leads to a reduction in evapotranspiration, which results in less downwind precipitation.
Yet it hardly constitutes the discovery of an aqueous elixir.The difficult problem that still awaits an answer is how to get higher yields from food crops without a commensurate rise in the loss of water through evapotranspiration.
Because precipitation in tropical rainforest regions exceeds evapotranspiration at almost all times, a nearly permanent surplus of water exists in the soil and moves downward through the soil into streams and rivers in valley floors.
However, their most fundamental characteristic is a shortage of available moisture for plants, resulting from an imbalance between precipitation and evapotranspiration.
Actual evapotranspiration is never greater than precipitation except on irrigated land because of percolation of water into groundwater bodies and surface runoff.
The soil moisture zone gains water by precipitation and infiltration and loses water by evapotranspiration, overland flow, and percolation of water downward due to gravity into the groundwater zone.
