Temperature Lapse Rate Equation:
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Temperature Lapse Rate is the rate at which an atmospheric variable, normally temperature in Earth's atmosphere, falls with altitude. It is a crucial parameter in meteorology and atmospheric sciences.
The calculator uses the Temperature Lapse Rate equation:
Where:
Explanation: The equation calculates the temperature lapse rate based on the specific gravity of the fluid and empirical constants a and b derived from atmospheric conditions.
Details: Accurate temperature lapse rate calculation is essential for weather forecasting, atmospheric modeling, and understanding vertical temperature distributions in the atmosphere.
Tips: Enter Specific Gravity of Fluid (G), Constant b, and Constant a. All values must be positive numbers greater than zero.
Q1: What is the typical range of temperature lapse rate values?
A: The environmental lapse rate is typically around 6.5°C per kilometer (0.0065°C/m) in the troposphere.
Q2: How does temperature lapse rate affect weather patterns?
A: Different lapse rates can indicate atmospheric stability or instability, which influences cloud formation and precipitation.
Q3: What are the different types of lapse rates?
A: The main types are environmental lapse rate, dry adiabatic lapse rate, and moist adiabatic lapse rate.
Q4: How is this equation derived?
A: The equation is derived from thermodynamic principles and empirical relationships in atmospheric physics.
Q5: What units are used for temperature lapse rate?
A: Temperature lapse rate is typically measured in degrees Celsius per meter (°C/m) or degrees Celsius per kilometer (°C/km).