Formula Used:
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The effective surface temperature formula calculates the surface temperature of the sun or a star based on the solar constant, mean distance between the sun and planet, and the radius of the sun. It applies the Stefan-Boltzmann law to determine the temperature from radiative energy balance.
The calculator uses the formula:
Where:
Explanation: The formula derives from equating the solar radiation received at Earth's distance to the radiation emitted by the sun's surface, using the inverse square law and Stefan-Boltzmann law.
Details: Calculating the sun's effective surface temperature is fundamental in astrophysics and climatology. It helps understand stellar properties, solar radiation effects on planetary climates, and validates theoretical models of stellar structure and evolution.
Tips: Enter mean distance in meters, total solar irradiance in W/m², and sun's radius in meters. All values must be positive. For Earth-sun system, typical values are L = 1.5×10¹¹ m, Gs = 1361 W/m², r = 6.96×10⁸ m.
Q1: What is the difference between effective temperature and actual surface temperature?
A: Effective temperature is the temperature of a black body that would emit the same total radiation. The sun's actual photospheric temperature varies with depth.
Q2: Why use the Stefan-Boltzmann constant in this calculation?
A: The Stefan-Boltzmann law relates the total energy radiated per unit surface area of a black body to the fourth power of its temperature, making it essential for this calculation.
Q3: How accurate is this temperature estimation?
A: This provides a good approximation but assumes the sun is a perfect black body and doesn't account for atmospheric absorption variations.
Q4: Can this formula be used for other stars?
A: Yes, the formula applies to any star when you have the appropriate values for distance, irradiance at that distance, and stellar radius.
Q5: What factors affect solar irradiance measurements?
A: Solar irradiance varies with solar activity, Earth's orbital eccentricity, and atmospheric conditions during measurement.