prof lj says . yes it does due to smoke temprature kinda like a sauna
The warmer the temperature, the more water vapor in the air. The colder the temperature, the less water vapor in the air.
How does temperature affect humity? The mount of water vapor that air can hold depends on the temperature of the air.
Temperature affects condensation by influencing the rate at which water vapor molecules in the air condense into liquid water. As temperature decreases, the air's ability to hold water vapor decreases, leading to the condensation of water vapor into liquid water droplets. Warmer temperatures can hold more water vapor, delaying or preventing condensation.
Factors that can affect the amount of water vapor in the air include temperature (warmer air can hold more water vapor), proximity to bodies of water, wind patterns, humidity levels, and altitude (higher altitudes generally have lower water vapor levels).
Higher temperatures increase the amount of water vapor that air can hold. When the temperature decreases, the air becomes saturated and condensation occurs, leading to the formation of water droplets or clouds. Warmer temperatures can also accelerate the evaporation of water into vapor.
Water vapor in the cool air condenses in to tiny droplets of water, forming clouds.
Water vapor condenses into liquid water at its dew point temperature.
The warm water evaporates. The water vapor returns to the land as rain.
Water vapor in air condenses into liquid water at the dew point temperature.
When the vapor pressure of water is 70 kPa, the corresponding temperature is approximately 45.6°C (114.1°F). This relationship can be determined using the water vapor pressure-temperature tables or the Antoine equation, which relates vapor pressure to temperature. At this pressure, water is in a state where it can coexist as both liquid and vapor.
When the temperature drops the less water vapor in the air
When the temperature of water vapor condenses into a liquid, it is called condensation. This process involves the conversion of water vapor back into liquid water due to a decrease in temperature.