Skip to content

Drawing No. EH–ES–002 // Environmental & Safety Engineering

Cooling-Tower Visible-Plume Predictor

Reviewed August 2026

Screen whether warm, moist cooling-tower exhaust can become supersaturated as it mixes with ambient air. The result indicates thermodynamic plume potential and shows the mixing path on a simplified psychrometric plot.

Scope: Use the temperature and relative humidity of the air leaving the tower, not the hot-water inlet temperature. This tool does not predict plume length, rise, opacity, ground contact, icing or drift deposition.

What this predictor does

Warm tower exhaust is mixed with ambient air in small steps. At each step, the tool conserves moist-air enthalpy and humidity ratio, then compares the mixed state with the saturation humidity ratio. A visible condensation plume is thermodynamically possible wherever the mixing path lies above saturation.

Inputs

Example conditions

Outdoor air temperature near the tower discharge.
Use a concurrent value, not a seasonal average.
Air temperature at the fan stack or tower outlet.
Wet-tower exhaust is often near saturation. Use measured or vendor data where available.
Pressure affects humidity ratio. Sea-level standard pressure is 101.325 kPa.

Results

THERMODYNAMIC PLUME POTENTIAL YES
Strong visible-plume potential A substantial part of the ideal mixing path is supersaturated.
Plume-potential scaleStrong
None
Marginal
Moderate
Strong
Maximum condensate potential: 1.02 g/kg dry airScreening scale — not measured opacity or plume length
Screening class
Strong
Based on peak supersaturation
Maximum mixed-air RH
118.2%
Before condensate removal
Maximum condensate potential
1.02 g/kg
Per kg of dry mixed air
Peak mixture temperature
12.4 °C
At maximum supersaturation
Condensation mixing range
8–92%
Exhaust fraction by dry-air mass
Ambient dew point
−2.0 °C
Moisture context
Cooling tower plume formationWarm moist exhaust rises from a cooling tower, mixes with ambient air, and may form a visible cloud when the mixture becomes supersaturated. WET COOLING TOWERVISIBLE PLUME POTENTIALAmbient airVisible water droplets / ice crystals

Psychrometric mixing path

The saturation curve is the maximum water-vapour content of air at each temperature. The red portion of the mixing path is above saturation and represents theoretical condensate formation.

Saturation boundaryUnsaturated mixingCondensation zone

Scroll the plot horizontally for readable labels.

Cooling tower moist-air mixing plotA chart of humidity ratio versus dry-bulb temperature showing the saturation curve and the line between ambient and tower exhaust states.

How to reduce visible plume

01
Use a dry or hybrid section

Heating or drying the discharge lowers its relative humidity and can keep the mixing path below saturation.

02
Mix in dry air before discharge

Plume-abatement systems blend warm dry air with saturated wet-section exhaust before it reaches the atmosphere.

03
Check concurrent winter conditions

Low ambient temperature and high relative humidity are typically the most plume-prone combination. Use site weather bins, not annual averages.

04
Escalate when impacts matter

For roads, airports, buildings or electrical equipment, use a site-specific dispersion/CFD study that addresses plume rise, recirculation, icing and ground contact.

Interpretation and limitations

Visible plume is not the same as drift. A visible plume is mainly condensed water vapour. Drift consists of liquid droplets carried out of the tower and may contain dissolved cooling-water constituents.

The predictor answers one question only: can ideal mixing cause supersaturation? A positive result does not mean a long or ground-level plume will occur. Wind speed, turbulence, exit velocity, tower geometry, ambient stability, droplet nuclei and sunlight all affect observed visibility.