Interaction between the Earth’s atmosphere and sun’s heat is a never-ending process and is always a constant. Every part of the atmosphere doesn’t get heated up equivalently at the same time. This in-equivalence makes the large masses of air to move about as an automatic response of the atmosphere to balance itself. The varied types of weather are a direct result of this mass movement of air.
The existing air mass in a region gets encountered that is already there when another air mass moves in. front is the boundary that is created between these two air masses. Cold front is when the cold air replaces the warm air and when cold front gets replaced, it is known as a warm front.
A cold air mass when encounters a warm front, the colder air get pushed below the warm front. Condensed water vapor changes into clouds when the warm front rises and cools down. Appearance of mid-level clouds follows high cirrus clouds. Mid-level cloud is followed by Thick stratus clouds. Precipitation and wind come next.
Often cold fronts produce weathers that are more volatile by nature. The warm air mass moves upward sharply when it comes in contact with a cold...
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