evapotranspiration , ET (Abkürzung)

Evapotranspiration is an important part of the water cycle.

Evapotranspiration is a key indicator for water management and irrigation performance.

It can also be characterized by having more evapotranspiration than precipitation.

A diminished river flow will also contribute to higher evapotranspiration.

Potential evapotranspiration, then, is the amount of water that could evaporate in any given region.

The semiarid classification is due to the city's high evapotranspiration.

The process generally occurs in areas where precipitation is greater than evapotranspiration.

The evapotranspiration is twice that of precipitation, causing a water deficit.

Strong winds, low humidity and high temperatures all increase evapotranspiration from leaves.

Soil moisture is almost always high because of lower evapotranspiration due to the cool climate.

Fifty-six percent of the average annual rainfall are lost to evapotranspiration.

A third methodology to estimate the actual evapotranspiration is the use of the energy balance.

After being removed from the production greenhouse the plant slows evapotranspiration.

Actually, it contributes to freshness thanks to the evapotranspiration phenomenon.

Where such water enters the atmosphere through evapotranspiration, these salts are left behind.

There are three general approaches to estimate evapotranspiration indirectly.

The remaining water is lost through evaporation and evapotranspiration.

Evapotranspiration can be measured or estimated using several methods.

The difference between potential evapotranspiration and precipitation is used in irrigation scheduling.

Through the evapotranspiration of water, trees discharge excess heat from the forest canopy.

And major deforestation would decrease recycling of rainfall through evapotranspiration.

Green roofs that cool buildings with extra thermal mass and evapotranspiration.

The dual effects of evaporation and transpiration are called evapotranspiration.

Evapotranspiration is a significant water loss from drainage basins.

Due to its high evapotranspiration, Faisalabad features an arid climate.