normal lapse rate
Quick Summary
The normal lapse rate in meteorology refers to the rate at which temperature decreases as you move upward through the Earth's atmosphere. This is also known as the environmental lapse rate. On average, the temperature drops by about 6.5 °C (11.7 °F) for every kilometer (0.6 miles) of altitude in the troposphere, the lowest layer of the atmosphere.1
This cooling occurs because as air rises, it encounters lower atmospheric pressure. This allows the air to expand, and this expansion uses energy, causing the air to cool down. This is known as adiabatic cooling. The lapse rate is crucial for meteorologists in forecasting weather phenomena like cloud formation and thunderstorms.21
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