"Saturated" or "At saturation point".
West wind typically brings cooler and moister air, as it originates from the west and moves eastward. It can also influence weather patterns and contribute to changes in temperature and precipitation.
85...The warmer the temperature, the more water vapor it can hold.
The air that contains water vapor in equilibrium at a certain temperature is called saturated air. At saturation, the air has reached its maximum water vapor capacity at that temperature, leading to a balance between evaporation and condensation.
The lakes have a high specific heat capacity.Answer:Air passing over the lakes becomes moister from evaporation. This evaporation of water requires heat which is absorbed from the air. As a consequence the air becomes cooler.
Yes, when the relative humidity is 100 percent, it means the air is holding the maximum amount of moisture it can at that temperature. At this point, the air temperature is equal to the dew point temperature, causing condensation to form as the air becomes saturated with moisture.
Humidity
It is lower then for Warmer air
its water holding capacity
The temperature at which air reaches saturation is called the dew point temperature. At this temperature, the air is holding the maximum amount of water vapor it can hold at that specific temperature, leading to condensation or saturation.
humidity
smog
West wind typically brings cooler and moister air, as it originates from the west and moves eastward. It can also influence weather patterns and contribute to changes in temperature and precipitation.
The temperature at which air is saturated and condensation forms is called the dew point. This is when the air is holding as much moisture as it can at that temperature, leading to water vapor in the air turning into liquid water droplets.
lets warm air in when it reaches a certain temperature.
the air is holding 75% moisture relative to the temperature
Relative humidity expresses the amount of water vapor present in the air as a percentage of the maximum amount of water vapor the air can hold at that temperature. For example, if the relative humidity is 50%, it means the air is holding half of the maximum water vapor it can hold at that temperature.
The temperature at which air becomes saturated with water vapor is called the dew point temperature. This is the point at which the air is holding as much water vapor as it can at that temperature, resulting in condensation.