KEVOS® MAKEOS · Engineering

Moist Air Dew Point and Surface Condensation Check (Humidity Ratio, Enthalpy, Dew-Point Margin)

At this air temperature, relative humidity and pressure, what are the dew point, humidity ratio and enthalpy of the air, and will a surface at this temperature stay dry with the margin you need?

Moist-air properties from the dry-bulb temperature, relative humidity and pressure (vapour pressure, humidity ratio, enthalpy, specific volume and dew or frost point), and a check of whether a surface at a given temperature stays above the dew point with the margin you need.

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How this tool works

Inputs, units and where to find them

InputUnitTypical source
Air dry-bulb temperature°CAir temperature from a thermometer or the hygrometer’s temperature reading.
Relative humidity of the air%Relative humidity of the air from a calibrated hygrometer, relative to saturation over liquid water.
Total (barometric) pressurekPaBarometric (total) pressure: 101.325 kPa at sea level, lower at altitude; local weather data gives it.
Surface
Surface temperature°CTemperature of the coldest surface the air touches: a contact thermometer, an infrared reading corrected for emissivity, or a heat-transfer calculation.
Margin required above the dew pointKHow far above the dew point the surface must stay to allow for sensor error and changes in conditions; your own specification or practice.

What each input means

Open an input to see what it is, its units, the worked example and the common mistakes, with a small diagram.

What this means: Air dry-bulb temperature
Illustration: Air dry-bulb temperatureA thermometer whose level rises with Air dry-bulb temperature; the level follows the value you type.TExample: 25 °CAir dry-bulb temperature
What it is
The dry-bulb temperature of the air around the surface, as an ordinary shielded thermometer reads it.
Units and format
Enter a number in °C: degrees Celsius. The form accepts 0 °C to 90 °C. Required: the tool does not calculate until every input is valid.
Example
The form opens with 25 °C as a worked example. It is an illustration, not a recommended value: replace it with your own figure.
Effect on the result
At a fixed relative humidity, warmer air holds more moisture, so the dew point rises.
Get it right
Measure the air near the surface but not touching it; the tool accepts 0 to 90 °C.
What this means: Relative humidity of the air
Illustration: Relative humidity of the airA bar of 100 parts with the share marked; Relative humidity of the air is that share out of 100. The bar follows the value you type.0 %100 %φExample: 60%Relative humidity of the air
What it is
How much water vapour the air holds as a share of the most it could hold at its temperature, relative to saturation over liquid water.
Units and format
Enter a number in %: percent: the number is read as a percentage, so type 8 for 8 %. The form accepts 0.1% to 100%. Required: the tool does not calculate until every input is valid.
Example
The form opens with 60% as a worked example. It is an illustration, not a recommended value: replace it with your own figure.
Effect on the result
Higher humidity raises the vapour pressure and the dew point, reducing the margin.
Get it right
Many hygrometers drift by several per cent; a recent calibration matters when the margin is small.
What this means: Total (barometric) pressure
Illustration: Total (barometric) pressureA pressure gauge whose needle moves with Total (barometric) pressure; the needle follows the value you type.PExample: 101.325 kPaTotal (barometric) pressure
What it is
The total pressure of the moist air, the barometric pressure at the site, used to turn vapour pressure into a humidity ratio.
Units and format
Enter a number in kPa: kilopascals. The form accepts 50 kPa to 110 kPa. Required: the tool does not calculate until every input is valid.
Example
The form opens with 101.325 kPa as a worked example. It is an illustration, not a recommended value: replace it with your own figure.
Effect on the result
Changes the humidity ratio, enthalpy and specific volume but not the dew point.
Get it right
Use about 101.325 kPa at sea level and roughly 1.2 kPa less per 100 m of altitude near the ground.

Surface

What this means: Surface temperature
Illustration: Surface temperatureA thermometer whose level rises with Surface temperature; the level follows the value you type.T_sExample: 22 °CSurface temperature
What it is
The temperature of the coldest surface in contact with the air, where condensation or frost would form first.
Units and format
Enter a number in °C: degrees Celsius. The form accepts -40 °C to 90 °C. Required: the tool does not calculate until every input is valid.
Example
The form opens with 22 °C as a worked example. It is an illustration, not a recommended value: replace it with your own figure.
Effect on the result
Raising it increases the margin above the dew point and the chance of staying dry.
Get it right
Infrared readings of shiny metal are badly wrong; use a contact probe or tape of known emissivity.
What this means: Margin required above the dew point
Illustration: Margin required above the dew pointTwo thermometers at different levels with the difference between them marked; Margin required above the dew point is that temperature difference.ΔTExample: 3 KMargin required above the dew point
What it is
The least temperature difference you accept between the surface and the dew point, covering measurement error and changes in the weather.
Units and format
Enter a number in K: kelvin (a difference of 1 K equals 1 °C). The form accepts 0 K to 30 K. Required: the tool does not calculate until every input is valid.
Example
The form opens with 3 K as a worked example. It is an illustration, not a recommended value: replace it with your own figure.
Effect on the result
Only moves the line between a dry result and a margin-too-small warning.
Get it right
A few kelvin is common practice; use more where conditions swing or sensors are uncertain.

Method and formulas

  1. Saturation pressure of water vapour from the Hyland–Wexler equations (ASHRAE Fundamentals, chapter 1): over liquid water at or above 0 °C, over ice below; they match the steam-table values in Çengel’s Table A-4 to within 0.02 % between 0.01 and 100 °C.
  2. Vapour pressure p_v = φ p_sat(T); humidity ratio ω = 0.622 p_v ÷ (P − p_v); enthalpy h = 1.005 T + ω (2500.9 + 1.82 T) kJ/kg of dry air; specific volume v = 0.287 (T + 273.15) ÷ (P − p_v).
  3. Dew point: the temperature at which p_sat equals p_v, solved by bisection; below 0 °C this is the frost point over ice.
  4. Margin = surface temperature − dew point: at or above the required margin the surface stays dry; between zero and the margin the margin is too small; at or below zero water (or frost) forms.
  5. Example: air at 25 °C and 60 % at sea-level pressure has a dew point of 16.7 °C and 11.896 g/kg of moisture; a surface at 22 °C stays 5.3 K above it, more than the 3 K required.

Limitations

  • Uniform air and steady conditions; real condensation often happens where air is trapped against a cold surface, at night, or when warm humid air enters a cool enclosure.
  • Air temperatures from 0 to 90 °C; relative humidity is taken over liquid water.
  • Hygrometers are often only accurate to a few per cent of relative humidity, which moves the dew point by about a degree; the margin should cover this.
  • Example values are illustrations. Replace them with values for your actual site.

Typical uses

  • Check whether cold pipes, ducts, tanks or walls will sweat
  • Check whether an electrical enclosure, machine or store needs heating or dehumidifying
  • Find the dew point and humidity ratio of air for psychrometric work

Who it is for

  • Mechanical services and maintenance engineers
  • Electrical and controls engineers
  • Building and facility managers

What you get

  • Dew point (frost point below 0 °C) and margin of the surface above it
  • Relative humidity the air would have at the surface temperature
  • Humidity ratio, enthalpy, specific volume, vapour and saturation pressure

Interpreting the result

  • High relative humidity at the surface, short of 100 %, can already support mould growth and corrosion on dusty or salty surfaces before liquid water appears.
  • The dew point depends only on the moisture in the air; heating the air does not change it, but heating the surface does.

Before relying on the result

  • Log temperature and humidity over a full day and night: the worst case is usually not when you visit.

References

  • Çengel Y. A. and Boles M. A., Thermodynamics: An Engineering Approach, 5th edition (McGraw-Hill, 2006), chapter 14 (sections 14-1 to 14-3: dry and atmospheric air, specific and relative humidity, dew-point temperature). Method reference; no tables, figures or examples are reproduced.
  • ASHRAE Handbook—Fundamentals (SI), chapter 1 Psychrometrics: Hyland–Wexler saturation pressure equations over ice and liquid water.
  • National Construction Code (Australian Building Codes Board), condensation management provisions for buildings.

Learn the Concepts Behind This Tool

These KEVOS® Library readings explain the method this tool uses, with worked examples.

Learning pathway

Check whether a cold surface will sweat

Learn how vapour pressure sets the dew point, then check your own surface against it with a margin.

  1. 1 Learn

    Read Water in air: vapour pressure, humidity and dew point in Condensation Control by the Numbers.

    What vapour pressure is, why it depends only on temperature, how relative humidity, dew point and absolute humidity follow from it, and why dew point is the number to watch.

  2. 2 Apply

    Open Moist Air Dew Point and Surface Condensation Check (Humidity Ratio, Enthalpy, Dew-Point Margin) and enter your own figures.

    At this air temperature, relative humidity and pressure, what are the dew point, humidity ratio and enthalpy of the air, and will a surface at this temperature stay dry with the margin you need?

  3. 3 Verify

    Read the tool’s feasibility and verification checks under the result, and test your answer against its stated limitations:

    • Uniform air and steady conditions; real condensation often happens where air is trapped against a cold surface, at night, or when warm humid air enters a cool enclosure.
    • Air temperatures from 0 to 90 °C; relative humidity is taken over liquid water.
    • Hygrometers are often only accurate to a few per cent of relative humidity, which moves the dew point by about a degree; the margin should cover this.
    • Example values are illustrations. Replace them with values for your actual site.
  4. 4 Improve

    Download the decision report or copy the link with your inputs to keep a record, then change one assumption at a time and compare.

    Next reading: Cold pipes, sweating and insulation in Condensation Control by the Numbers.

KEVOS® tools are screening and decision-support utilities. Verify important financial, engineering, safety, legal or operational decisions using appropriate professional standards and your organisation’s approved data.

Open the Moist Air Dew Point and Surface Condensation Check (Humidity Ratio, Enthalpy, Dew-Point Margin) calculator