The dew point is the temperature at which air becomes saturated with moisture, leading to condensation. In the context of thermometers, if one reads the wet-bulb temperature, the dew point can be estimated based on the difference between the wet and dry bulb readings. A smaller difference indicates a higher dew point, while a larger difference suggests a lower dew point. Thus, the dew point reflects the moisture content in the air under the given conditions.
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