Answer:
The troposphere is the lowest layer of the Earth's atmosphere, extending from the surface up to about 7-20 km (4-12 miles) depending on the latitude and season. It is the layer where most of the Earth's weather occurs, and where we live and breathe.
The troposphere is formed by a combination of processes involving the Earth's surface and the Sun's energy. The Sun's radiation heats the Earth's surface, causing it to warm up and create thermal energy. This thermal energy is then transferred to the air molecules in contact with the surface, causing them to rise and expand. As the warm air rises, it cools and loses some of its moisture, which condenses into clouds and precipitation.
At the same time, cooler air from higher altitudes sinks down to replace the rising warm air. This creates a convective cycle, where warm air rises and cool air sinks, creating a mixing of the atmosphere that distributes heat and moisture.
The boundary between the troposphere and the layer above it, the stratosphere, is marked by a temperature inversion layer called the tropopause, where the temperature stops decreasing with height and begins to increase again. This is due to the absorption of ultraviolet radiation by ozone molecules in the stratosphere, which creates a warming effect that prevents the mixing of air between the two layers.
Step-by-step explanation: