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.
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.