Saturation vapor pressure–
Vapor pressure deficit–
For most crops–
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Vapor pressure deficit

Warm air can hold more water vapor than cool air. The Tetens equation estimates the saturation vapor pressure in kilopascals as 0.6108 x exp(17.27 x T / (T + 237.3)), with T in °C. The actual vapor pressure is that times relative humidity, and the deficit is the difference: VPD = saturation pressure x (1 minus RH / 100).

Inside the leaf the air is nearly saturated at leaf temperature, so VPD is a good measure of the pull on water leaving the stomata. This model uses air temperature for both, a common simplification; a sunlit leaf is often a few degrees warmer, which raises the real deficit. Stomatal opening here is a simple teaching curve, not a physiological model.

Try it: hold humidity at 60 percent and raise the temperature from 20 to 35 °C. The deficit more than doubles even though relative humidity never changed, and the water vapor stream speeds up.

Why growers watch VPD

Greenhouse growers often aim for roughly 0.4 to 1.6 kPa. Too low and leaves cannot move water and nutrients well, and fungal disease thrives. Too high and plants close their stomata to avoid wilting, which slows photosynthesis and growth.

Where Avid uses this

Temperature and humidity readings turned into VPD are among the signals a precision agriculture system like Avid's VerdantaIQ can use to time irrigation.

How to cite this model

Avid Solutions International. (2026, November 11). How leaves breathe through stomata [Interactive 3D model]. Avid Field Lab. https://avidsolutionsintl.com/explore/transpiration-stomata

Last updated November 11, 2026

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