The wet-bulb temperature is a measurement that determines, in essence, how much water vapour the atmosphere is capable of holding given the current conditions. When the wet bulb temperature is lower, the air is drier and has a greater capacity for holding water vapour than it does when the wet-bulb temperature is higher.
The temperature of a parcel of air that has been cooled to saturation (100 percent relative humidity) by the evaporation of water into it is referred to as the wet-bulb temperature. This temperature is calculated using the latent heat that is supplied by the parcel. The temperature that is displayed on a wet-bulb thermometer is very near to the actual (thermodynamic) temperature of a wet bulb. The wet-bulb temperature is the lowest temperature that can be attained under the existing conditions of the environment only by the evaporation of water. This is the temperature at which the wet-bulb temperature scale begins.
Wet-bulb Temperature Line
The wet-bulb temperature has absolutely nothing to do with light bulbs, despite the fact that this is likely the first thing that comes to mind. Instead, it is the temperature that is read by a specialised thermometer that is vented and wrapped in fabric that has been drenched in water. A psychrometer is a piece of equipment that includes this thermometer as one of its components. It is equipped with a dry-bulb thermometer, a wet-bulb thermometer, as well as a psychrometric chart, which is a graph that plots the correlations between the dry-bulb temperature, the wet-bulb temperature, the relative humidity, and the dew point at a constant pressure.
The lowest temperature that a piece of air can achieve solely through the process of evaporative cooling is referred to as the wet-bulb temperature. The wet-bulb temperature is equivalent to the average air temperature when the relative humidity of the air is at its highest level (100 percent) (dry-bulb temperature). When there is less moisture in the air, the temperature measured by a wet-bulb thermometer drops below the ambient air temperature.
When it comes to avoiding our body from overheating, having accurate information about the temperature of the wet bulb is quite necessary. Because water evaporates more slowly in more humid conditions, our bodies cool down a lot more slowly in humid situations even though our bodies sweat as a means of cooling down. Because of this, the temperature on the inside of our body rises. People in the surrounding region are at danger of developing hyperthermia if the wet-bulb temperature remains at or above 35 ° Celsius (95 ° Fahrenheit) for an extended period of time.
Constant Wet Bulb
Since we are aware that evaporation is a process that takes place at the boundary between air and water, we may say that it is (or any liquid). The surface molecules of the water are able to exit out of the water by taking the latent heat of vaporisation because they have their own kinetic energy and they also get energy from the atmosphere. As a result, the temperature of the bulb will drop since the average kinetic energy of the system will be reduced.
As the temperature of the system drops, the wick absorbs an increasing amount of heat from the surrounding air. As a result, a greater amount of evaporation takes place. This will continue until the air has reached its maximum capacity, at which point no more liquid vapour can be added to it. At that point, the temperature of the wick stabilises and provides an accurate measurement of the temperature of the wet bulb.
The temperature at which adiabatic saturation occurs is referred to as the Wet Bulb temperature. This is the temperature that is shown by a thermometer bulb that has been soaked in water and then exposed to airflow.
The temperature measured with a wet bulb will always be lower than the temperature measured with a dry bulb, but they will be the same when the relative humidity reaches 100%.
A psychrometric diagram or a Mollier chart can be used to determine the status of the humid air by combining the dry bulb temperature with the wet-bulb temperature. The Psychrometric Chart is organised with lines of constant wet-bulb temperatures running in a diagonal direction from the top left to the lower right.
Wet-Bulb Temperature
The wet-bulb temperature is the lowest temperature that can be attained under the existing conditions of the environment only by the evaporation of water. This is the temperature at which the wet-bulb temperature scale begins.
Even persons who are used to the heat won’t be able to participate in routine outdoor activities once the wet-bulb temperature reaches 32 ° Celsius (90 ° Fahrenheit), which is comparable to a heat index of 55 ° Celsius (130 ° Fahrenheit).
At a wet-bulb temperature that is maintained at or above 35 ° Celsius (95 ° Fahrenheit), it is highly likely that even people who are physically fit and healthy will perish, even if they are unclothed, in the shade, next to a fan. This is because at this temperature, human bodies switch from losing heat to the environment to gaining heat from it.
This is one of the factors that contribute to humans’ seemingly high body temperatures. The lower the relative humidity of the air, the more water vapour it can store in addition to the water vapour that is already present, and the easier it is for any additional water to evaporate. Dryer air causes sweat to evaporate more quickly, which in turn helps bring down the temperature of the skin more rapidly. When the relative humidity is one hundred percent, no water can evaporate, which means that there is no way to cool yourself by sweating or evaporating water.
Once the relative humidity reaches 100 percent, a wet-bulb thermometer will no longer be able to be cooled by evaporation, and as a result, its reading will be the same as that of an unwrapped thermometer.
Conclusion
The wet bulb temperature is a measurement that determines, in essence, how much water vapour the atmosphere is capable of holding given the current conditions. When the wet-bulb temperature is lower, the air is drier and has a greater capacity for holding water vapour than it does when the wet-bulb temperature is higher. The wet-bulb temperature is determined using a specialised thermometer that is vented and wrapped in a fabric that has been drenched in water. A psychrometer is a piece of equipment that includes this thermometer as one of its components. The wet-bulb temperature is the lowest temperature that can be attained under the existing conditions of the environment only by the evaporation of water. This temperature is measured in degrees Fahrenheit. Even persons who are used to the heat won’t be able to participate in routine outdoor activities once the wet-bulb temperature reaches 32 ° Celsius (90 ° Fahrenheit), which is comparable to a heat index of 55 °Celsius (130 ° Fahrenheit).