VPD, transpiration and climate control
Plants move water and nutrients by transpiring, and the rate is driven by how far the air is from saturation at the leaf surface. Hold VPD too low and that pull weakens — growth slows and humid air invites mold; push it too high and plants defensively close their stomata, also slowing growth. A target band by growth stage keeps the crop in the productive middle, which is why controlled-environment operations — greenhouse tomatoes and peppers, leafy greens, propagation nurseries — manage to VPD rather than humidity alone.
Because leaves run cooler than the air, the calculator evaluates VPD at the leaf using your offset, and flags the propagation, vegetative and flowering bands directly on the result.
Related tools
The VPD calculator has the full breakdown; the dew point calculator covers leaf wetness and disease risk, and vapor pressure over ice the frost point for freeze protection.
Frequently asked questions
Why do growers control vapor pressure deficit (VPD) instead of humidity?
VPD combines temperature and humidity into a single measure of how strongly the air pulls moisture out of a leaf. The same relative humidity is far more drying at 30 °C than at 18 °C; VPD captures that, so it predicts transpiration, stomatal behavior and nutrient uptake better than humidity alone. That is why greenhouse and indoor growers tune to a VPD target rather than an RH number.
What VPD should a greenhouse aim for?
As a rule of thumb: roughly 0.4–0.8 kPa for propagation and young plants, 0.8–1.2 kPa during vegetative growth, and 1.2–1.6 kPa during flowering or fruiting. Too low and transpiration stalls and disease pressure rises; too high and plants close their stomata and growth slows. Optimal values vary by crop, so treat these as starting points and the calculator above as the way to hit them.
How does dew point relate to leaf wetness and disease?
When a leaf or fruit surface cools to the dew point — overnight, or under cold glass — water condenses on it. Sustained leaf wetness is what many fungal and bacterial diseases need to establish, so the dew point is a practical disease-risk indicator. Below freezing the relevant threshold is the frost point, computed over ice.
Why use leaf temperature rather than air temperature?
Transpiration cools leaves a couple of degrees below the surrounding air, and VPD should be evaluated at the leaf surface where evaporation happens. The calculator includes a leaf-temperature offset (a default of −2 °C is common) so the VPD reflects what the plant actually experiences; set it to 0 for the plain air VPD.
References
Every formula on this page is implemented from, and validated against, the following primary standards and papers — see the verification methodology.
- Crop Evapotranspiration (FAO Irrigation & Drainage Paper 56) — Allen, Pereira, Raes & Smith 1998 — defines vapor pressure deficit, VPD = eₛ − eₐ
- Improved Magnus Form Approximation of Saturation Vapor Pressure — Alduchov & Eskridge 1996, J. Appl. Meteorol. 35:601
- IAPWS R6-95(2018) / Wagner & Pruss 2002 — International Association for the Properties of Water and Steam — the reference standard
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