The troposphere is the lowest layer of the Earth's atmosphere, extending from the Earth's surface up to an average altitude of about 8-15 kilometers (5-9 miles) above sea level. It is the layer in which all weather occurs, and it contains the majority of the atmosphere's mass and moisture. The troposphere is characterized by a decrease in temperature with increasing altitude, which is due to the absorption of solar radiation by the Earth's surface and the release of heat through processes such as convection and condensation.
To fully understand the troposphere, it is important to grasp the following concepts:
By mastering these key points, you will develop a comprehensive understanding of the troposphere and its significance in the Earth's atmosphere.