At waters boiling point 100 degrees Celsius at sea level. At higher altitudes the temperature is less because there is less air pressure.
Air can become saturated by reaching its dew point temperature, which is the temperature at which the air can no longer hold all of its moisture and water vapor begins to condense into liquid form. When this happens, the air is at 100% relative humidity and is considered saturated.
Water vapor in air condenses into liquid water at the dew point temperature.
As air temperature increases, air molecules gain more energy and move faster, causing the air to expand and become less dense. This leads to a decrease in air pressure since the air molecules are more spread out. Conversely, as air temperature decreases, air molecules lose energy and move slower, causing the air to contract and become more dense, resulting in an increase in air pressure.
Do you mean at what temperature does air turn into a liquid or at what temperature does water condense out of the air?If the latter then air itself has not water in it and thus can never turn into water. It's the moisture (water vapor) in the air that will condense out of the air and turn into a liquid. This begins to occur at the dew point which depends on the how much moisture there is in the first place (humidity), the pressure, and the temperature. For example, current conditions where I am: Temp = 74 F, Pressure = 29.97 inches, Relative Humidity = 44%, dew point = 51 F. So this means that if we keep the pressure constant and drop the temperature to 51 F, water will begin to condense out of the air.If the former then, that's harder (for me anyway to answer). Usually the air is compressed AND cooled. At atmospheric pressure, the temperature would need to be extremely low for liquification. Nitrogen has a boiling temp of -195.8 C (the other gases boil at higher temps) so you would need to get the temperature below that.
Dew Point
The water temperature can be different from the air temperature.
To saturate the air with water vapor, you can lower the temperature to it's dew point, and leave out water to be evaporated.
Air temperature greatly affects water temperature. When the sun is strong, it increases the temperature of the air and water. On the other hand, when the sun is less intense, the temperature of the air and water decreases.
Water turn into a gas called water vapour. The air depending on its temperature will hold a certain amount of this. when the air comes into contact with water if the humidity of the air is such that it can hold more water vapour then the water that is touching the air will turn into the gas water vapour and become part of the air. it will do this at any temperature which explains why you can hang clothes out to drying sub zero temperatures and they dry.
If the water vapor content of air remains constant, lowering the air temperature causes relative humidity to increase. This is because relative humidity is the ratio of the current amount of water vapor in the air to the maximum amount the air can hold at that temperature. As the temperature decreases, the air's capacity to hold water vapor diminishes, resulting in a higher relative humidity percentage. If the temperature drops enough, the air can become saturated, leading to condensation and possibly precipitation.
Air can become saturated by reaching its dew point temperature, which is the temperature at which the air can no longer hold all of its moisture and water vapor begins to condense into liquid form. When this happens, the air is at 100% relative humidity and is considered saturated.
The temperature of water is typically colder than the temperature of the air.
Yes, air temperature can affect water temperature. Warmer air temperature can cause water to warm up, while colder air temperature can cause water to cool down. Wind and sunlight exposure can also play a role in influencing water temperature.
The relationship between air temperature and water temperature is that they are closely linked. Changes in air temperature can influence water temperature, as warmer air can heat up water and colder air can cool it down. This connection is important for understanding weather patterns and the overall climate.
When the air temperature reaches the dew point, water droplets that are in the air become visible. This is how you would get fog. Relative Humidity goes soaring to near 100%.
The water temperature can be different from the air temperature in a specific location. Factors like sunlight, wind, and depth of the water can affect the temperature of the water, making it either warmer or cooler than the air temperature.
The warmer the temperature, the more water vapor in the air. The colder the temperature, the less water vapor in the air.