What is the formula for evapotranspiration?

Crop evapotranspiration is calculated by multiplying ET_o by K_c, a coefficient expressing the difference in evapotranspiration between the cropped and reference grass surface.

How do you calculate ET?

Generally what you’ll do is add the highest temperature during a 24-hour period to the lowest temperature during that same period, then divide that sum by 2. This will give you a good estimate for the average temperature during that time.

How do you calculate annual evapotranspiration?

Obviousely, you want to estimate ET (evapotranspiration) using the water balance method: ET=P-R-TWSC, where P is precipitation, R is runoff and TWSC is change in terrestrial water change.

What increases evapotranspiration?

Temperature – As temperature increases, the rate of evapotranspiration increases. Evaporation increases because there is a higher amount of energy available to convert the liquid water to water vapor. Transpiration increases because at warmer temperatures plants open up their stomata and release more water vapor.

What is evapotranspiration rate?

The evapotranspiration rate is normally expressed in millimetres (mm) per unit time. The rate expresses the amount of water lost from a cropped surface in units of water depth. The time unit can be an hour, day, decade, month or even an entire growing period or year.

How do you calculate enzyme concentration in kcat?

Computing Kcat by hand Usually it is straightforward to express this (or convert to ) moles/minute/mg of protein. If you know the concentration of enzyme sites you’ve added to the assay (E_t) then you can calculate the catalytic constant K_cat. It is defined to equal V_max/E_t.

What is P pet?

P-PET = precipitation less the potential evapotrans- piration. 3. ACPWL, = accumulated potential water loss, which is the amount of soil water lost when PET exceeds P; i.e., there is less precipitation than potential evapotranspiration.

What is potential and actual evapotranspiration?

Actual evapotranspiration or AE is the quantity of water that is actually removed from a surface due to the processes of evaporation and transpiration. Potential evapotranspiration requires energy for the evaporation process. The major source of this energy is from the Sun.

What is meant by potential evapotranspiration?

Rosenberg says that potential evapotranspiration (abbreviated as ETP by him, but as PET by most others) is “the evaporation from an extended surface of [a] short green crop which fully shades the ground, exerts little or negligible resistance to the flow of water, and is always well supplied with water.

What are four factors affecting evapotranspiration?

Factors that affect evapotranspiration include the plant’s growth stage or level of maturity, percentage of soil cover, solar radiation, humidity, temperature, and wind. Through evapotranspiration, forests reduce water yield, except for in unique ecosystems called cloud forests.

Does temperature affect transpiration?

Temperature: Transpiration rates go up as the temperature goes up, especially during the growing season, when the air is warmer due to stronger sunlight and warmer air masses. Wind and air movement: Increased movement of the air around a plant will result in a higher transpiration rate.