Relative humidity always has a ❌ sign.
Relative humidity (%) = ❌ in the air (g/m3) / ❌ the air can hold (❌) x 100%
Relative humidity also varies with . air can hold more water vapour than air. When temperature , the amount of water vapour in the air stays the same, but the rise in temperature makes the air able to hold water vapour. Thus, relative humidity as temperature increases.
occurs when relative humidity is at per cent. Thus, when air holds the amount of water vapour it can hold at a particular temperature, it is said to be . The particular temperature at which saturation occurs is known as the dew point temperature. At point temperature, starts to occur. Condensation is a process in which water vapour s to a liquid known as water droplets by .
In order for clouds to form, a few processes need to occur. They are
evaporation
condensation
particle-formation
coalescence
precipitation
effervescence
diffusion
extension
limitation
A cloud is a visible mass of water vapour or ice cubes that are suspended in the atmosphere.
