What is the state of atmospheric instability?

Atmospheric instabilities are formed in a different way from atmospheric depressions. When warm air rising from the lower layers of the atmosphere meets cold air descending from the upper layers of the atmosphere over a certain geographical area, in conjunction with the presence of moist air in the atmosphere, a state of lack of Atmospheric stability, this condition leads to the formation of the so-called cumulus clouds that grow vertically to the upper layers of the atmosphere, increasing their thickness, and accompanied by the occurrence of several weather phenomena, namely: thunderstorms that may be strong - heavy rain, which may be in a short period of time - Downdraft - High winds and sandstorms - Showers of hail, which can be large in size, causing some damage.