Vapour-pressure deficit
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Through Greenhouse, Pascal (unit) and Ecology
In ecology, it is the difference between the 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.
Computing VPD for plants in a greenhouse
To compute the VPD, we need the ambient (greenhouse) air temperature, the relative humidity and, if possible, the canopy air temperature. We must then compute the saturation pressure. Saturation pressure can be looked up in a psychrometric chart or derived from the Arrhenius equation; a way to compute it directly from temperature is
where
- is the saturation vapor pressure in PSI,
- ,
- ,
- ,
- ,
- ,
- ,
- is temperature of the air in the Rankine scale.
To convert between Rankine and degrees Fahrenheit:
We compute this pressure for both the ambient and canopy temperatures.
We then can compute the partial pressure of the water vapour in the air by multiplying by the relative humidity [%]:
- ,
and finally VPD using or when the canopy temperature is known, or simply
- .
It can easily be seen from this formula that if rises (which raises ), but relative humidity remains constant, will increase.
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Climate
VPD can be a limiting factor in plant growth. Climate change is predicted to increase the importance of VPD in plant growth, and will further limit growth rates across ecosystems.
Application in contexts of wildfire
The vapour pressure deficit can be utilized when predicting behaviour of a wildfire. Such predictions are an essential tool of wildfire suppression.

