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Temperature Lapse Rate Formula:
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The Temperature Lapse Rate is the rate at which atmospheric temperature decreases with an increase in altitude. It is a crucial parameter in meteorology and atmospheric science for understanding vertical temperature profiles in the atmosphere.
The calculator uses the Temperature Lapse Rate formula:
Where:
Explanation: The formula calculates the rate of temperature change with altitude based on gravitational acceleration, gas properties, and specific atmospheric constants.
Details: Accurate temperature lapse rate calculation is essential for weather forecasting, climate modeling, aviation safety, and understanding atmospheric stability and convection processes.
Tips: Enter acceleration due to gravity in m/s², universal gas constant in J/(mol·K), and specific constant value. All values must be positive numbers.
Q1: What is the typical value of temperature lapse rate in Earth's atmosphere?
A: The average environmental lapse rate in Earth's troposphere is approximately 6.5°C per kilometer.
Q2: How does temperature lapse rate affect weather patterns?
A: Different lapse rates determine atmospheric stability, which influences cloud formation, precipitation, and storm development.
Q3: What factors can cause variations in temperature lapse rate?
A: Variations can occur due to latitude, season, time of day, humidity levels, and atmospheric pressure conditions.
Q4: How is this calculation used in aviation?
A: Pilots use lapse rate information to predict temperature changes at different altitudes, which affects aircraft performance and fuel efficiency.
Q5: What's the difference between dry and moist adiabatic lapse rates?
A: Dry adiabatic lapse rate is about 9.8°C/km, while moist adiabatic lapse rate varies but is typically around 5°C/km due to latent heat release.