Climatic Chamber Configurator
Discover the Climatic Chamber Configurator
Our guide to choosing the climate chamber best suited to your needs.

When working with humidity and temperature climate chambers, it is important to have a solid understanding of thermodynamic states and in particular of dew condensation.
In the following article, we will discover what the dew point is and why it is important for our climate chamber tests.
Thermodynamics identifies a series of thresholds that determine the transition of a substance from one state to another. These thresholds are called "points."
The best-known of these is undoubtedly the boiling point , which marks the beginning of the gasification process of a liquid. As we all learn in school, the boiling point of water at sea level is reached at a temperature of 100°C.
The dew point can be considered the inverse because it identifies the threshold below which a two-phase mixture (such as water and air) becomes saturated with vapor, resulting in a change of state. Condensation occurs when the air temperature drops, reducing the amount of energy available to maintain the water in the vapor form, which returns to its liquid state.
It is what we also call “dew” in common language.
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The dew point is related to three parameters: temperature, humidity and atmospheric pressure.
Assuming that atmospheric pressure is constant (like the example of water at sea level), it is the other two parameters that are decisive.
For example, at 85° and 85% relative humidity, the dew point falls to 80.9°; at 23° the dew point falls to 12° if the relative humidity is 50% but to -10° if the relative humidity is only 10%.
One of the main standards for measuring the dew point of an environment is the ASTM D4230-02.
The dew point is a crucial threshold for measuring the relative humidity of an environment. In fact, it is relative humidity that causes a gas to become saturated and condenses into dew. As the previous examples show, a simple equation can calculate the relative humidity of an environment by knowing its temperature and observing the dew point.
Meteorologists use the dew point to interpret the climate of an area, but it is also important for a whole series of laboratory tests , not least climate tests that use humidity and temperature chambers.
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In climatic chambers, temperature plays a fundamental role together with the other essential parameter: relative humidity.
When carrying out climatic tests relating to the corrosion of metals, for example, humidity is the first factor to take into consideration.
For this reason, it is extremely important to ensure that the sample we are testing is always above the dew point to prevent condensation from forming, which would alter the test values.
FDM climatic chambers guarantee the operator full control of all the parameters examined, thanks to our two highly technological controllers: stillFACE and revoFACE.
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The dew point (Tdp) is the temperature at which air reaches saturation (100% RH) and vapor begins to condense. It is measured using three methods: chilled mirror hygrometers (accuracy ±0.1°C, metrological reference), capacitive HMP sensors (accuracy ±1°C, industrial use), and psychrometers (wet/dry bulb, low cost). For compressed air and process gases, ISO 8573-1 certified dew point transmitters are used
ISO 8573-1:2010 classifies compressed air into 6 humidity classes: Class 1 dew point ≤ -70°C (critical pharmaceutical), Class 2 ≤ -40°C (electronics), Class 3 ≤ -20°C (clean industrial), Class 4 ≤ +3°C (standard industrial), Class 5 ≤ +7°C, Class 6 ≤ +10°C. Classes 1-3 require adsorption dryers; 4-6 require refrigeration dryers.
The dew point is the condensation temperature above 0°C (droplet formation). The frost point is the freezing point below 0°C (frost forms directly by sublimation). In metrological measurement below 0°C, it is differentiated to avoid errors: at -20°C, the frost point, the absolute humidity is different from the theoretical dew point at -20°C. For precision calibrations, the NIST-traceable Modified Magnus Formula is used for the conversion.
Industrial compressed air (ISO 8573-1): humidity class verification for pharmaceutical, electronic, and automotive processes. Insulating oils (ASTM D1533): water in electrical transformers, critical above 30-40 ppm. Natural gas: hydrocarbon dew point for pipelines. Environmental chambers: humidity control validation in extreme ranges. Electronic component testing: condensation prediction and MSL (Moisture Sensitivity Level) for reflow soldering.
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