Variation in the Net Heat Budget at the Earth’s Surface
- The amount of radiation that the earth’s surface receives varies. While certain areas of the globe have an excess of radiation, others are in deficit.
- Between 40 degrees north and south, there is a surplus of net radiation balance, whereas the areas close to the poles have a deficit. The tropics do not gradually get warmer due to the buildup of excess heat or the high latitudes do not become permanently cold due to excess deficiency because the surplus heat energy from the tropics is reallocated polewards.
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.