SUMMARY
The temperature decreases with altitude due to the adiabatic cooling process, where rising air expands and loses internal energy. As altitude increases, air pressure and density decrease, leading to less heat absorption from the ground. The ground heats the air through conduction and radiation, but at higher altitudes, the air is less dense and receives less heat. Additionally, the presence of clouds acts as a heat shield, further cooling the air above them.
PREREQUISITES
- Understanding of adiabatic processes in thermodynamics
- Knowledge of gas laws, particularly Charles' Law
- Familiarity with atmospheric pressure and density concepts
- Basic principles of heat transfer: conduction and radiation
NEXT STEPS
- Research the principles of adiabatic cooling in atmospheric science
- Study the effects of altitude on human physiology, particularly oxygen levels
- Explore the role of clouds in temperature regulation in the atmosphere
- Investigate the differences in temperature profiles across various atmospheric layers, including the troposphere and stratosphere
USEFUL FOR
Students studying meteorology, atmospheric scientists, and anyone interested in understanding the effects of altitude on temperature and air density.