Heating and Cooling of Atmosphere
There are different ways of heating and cooling the atmosphere. The main are as follows:
1. Terrestrial Radiation
2. Conduction
3. Convection
4. Advection
1. Terrestrial Radiation:
The earth receives insolation in short waves, which heats the surface. The earth, once heated, transforms into a radiating body and emits energy in the form of long waves into the atmosphere. The atmosphere is heated from below by this energy. It is known as Terrestrial Radiation.
2. Conduction:
The process of transfer of heat from a warmer object to a cooler object by contact is known as “Conduction”. It is important for the lower layers of the atmosphere.
3. Convection:
The movement of a mass or substance from one location to another, usually vertically, with the purpose of transferring heat, is known as Convection.
4. Advection:
The transfer of heat through the horizontal movement of air is known as Advection. Variation in daily weather is due to the Advection.
Solar Radiation – Heat Balance, Transfer & Distribution of Temperature
Here we are going to discuss a Geography topic which is ” Solar Radiation – Heat Balance, Transfer & Distribution of Temperature “. This topic is a part of the general awareness of many competitive exams. This article covers the entire essence of the topic by which you get the most out of it. This article is very helpful for SSC, Banking, Railway and for other competitive exams.