Deficit
Vapour Pressure Deficit, or
VPD, is the difference (deficit) between the amount of moisture in the air and how much moisture the air can hold when it is saturated. Once air becomes saturated water will condense out to form clouds, dew or films of water over leaves. It is this last instance that makes VPD important for
greenhouse regulation. If a film of water forms on a plant leaf it becomes far more susceptible to rot. On the other hand, as the VPD increases the plant needs to draw more water from its roots. In the case of
cuttings, the plant may
dry out and die. For this reason the ideal range for VPD in a greenhouse is from 0.45
kPa to 1.25 kPa, ideally sitting at around 0.85 kPa. As a general rule, most plants grow well at VPDs of between 0.8 to 0.95 kPa
[1]
In
ecology, it is the difference between the actual
water vapour pressure and the saturation water vapour pressure at a particular
temperature. Unlike relative humidity, vapour pressure deficit has a simple nearly straight-line relationship to the rate of
evapotranspiration and other measures of evaporation.