Elevation Temperature Formula:
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The elevation temperature formula estimates the temperature at a given elevation based on the sea level temperature. It uses the standard atmospheric lapse rate of 6.5°C per 1000 meters.
The calculator uses the elevation temperature formula:
Where:
Explanation: The formula accounts for the typical decrease in temperature with increasing elevation in the troposphere.
Details: Understanding temperature changes with elevation is crucial for weather prediction, aviation, mountaineering, and ecological studies.
Tips: Enter sea level temperature in °C and elevation in meters. The elevation must be a positive number.
Q1: Is the lapse rate always 6.5°C per 1000m?
A: No, this is an average value. Actual lapse rates can vary depending on atmospheric conditions.
Q2: How accurate is this calculation?
A: It provides a general estimate but doesn't account for local weather patterns, humidity, or other microclimate factors.
Q3: Does this work for all elevations?
A: It's most accurate for elevations within the troposphere (up to about 11,000m at mid-latitudes).
Q4: Why does temperature decrease with elevation?
A: As air rises, it expands due to lower pressure, which causes it to cool adiabatically.
Q5: Can I use this for temperature inversion situations?
A: No, temperature inversions (where temperature increases with height) require different calculations.