Air can hold finite amount of moisture in a given volume of air. When temperature increases the space between the molecules increases letting more moisture accumulating in the atmosphere.How ever this depends on the local water bodies.
Moisture in air is expressed as Relative humidity . It has no units as it is a percentage.
moisture content
moisture content
Wind direction is the direction which the wind blows. If the wind direction is coming from an arid region, such as a desert, the air will be dry and moisture content will be low. If the wind direction is coming from an ocean, lake, or tropical area, the air will have a higher moisture content.
When the temperature of air is cooled or reduced the relative humidity (RH) increases. The moisture content of the air remains the same until the RH rises to the point of 100% saturation and condensation occurs.
Amount of sun, amount of clouds and amount of moisture in the air are 3 examples of things that could affect temperature.
moisture content
Air masses can affect the weather because different air masses differ in temperature, density, and moisture content.
By The source region
Moisture and Temperature
moisture content
Yes, temperature in the air has more moisture content . Due to the condensation of particles in the humidity liberates the particle which has high heat particles which increases the temperature.
warmer air can hold more moisture.
when there is more moisture in the air, it is warmer and thicker. when there is less moisture in the air it is cooler and thinner. so if it is cooler temperature then it will drop faster.
Wind direction is the direction which the wind blows. If the wind direction is coming from an arid region, such as a desert, the air will be dry and moisture content will be low. If the wind direction is coming from an ocean, lake, or tropical area, the air will have a higher moisture content.
When the temperature of air is cooled or reduced the relative humidity (RH) increases. The moisture content of the air remains the same until the RH rises to the point of 100% saturation and condensation occurs.
low moisture content and low temperature
Amount of sun, amount of clouds and amount of moisture in the air are 3 examples of things that could affect temperature.