Unlike the rapid pressure drop in the troposphere, the stratosphere exhibits a more gradual flattening of pressure as altitude increases. Therefore, as the stratosphere warms with altitude, the air molecules move faster and exert greater force, creating a plateau in pressure decrease.
Understanding Stratosphere Air Boundary Transition Effects
Consequently, the air pressure behavior is not just a result of gravity but is actively modulated by this solar-driven chemical process. According to the ideal gas law, pressure is directly proportional to temperature when volume is constant.
Comparison with Other Atmospheric Layers. Consequently, the air pressure behavior is not just a result of gravity but is actively modulated by this solar-driven chemical process.
How Stratosphere Air Boundary Transition Affects Air Pressure Gradients
Altitude (Kilometers) Approximate Pressure (Millibars) 10 (Tropopause) 100 20 10 30 1 50 (Stratopause) 0. The stability provided by this warming effect suppresses vertical convection, allowing the pressure to behave in a more uniform manner than in the turbulent troposphere below.
More About What is the air pressure in the stratosphere
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