Formula Used:
From: | To: |
Total solar irradiance, also known as the solar constant, is the amount of solar energy reaching the top of a planet's atmosphere per unit area. It represents the total power from the sun incident on a surface perpendicular to the sun's rays at the average Earth-sun distance.
The calculator uses the solar irradiance formula:
Where:
Explanation: This formula calculates the solar energy flux at a given distance from a star based on its size and temperature.
Details: Calculating solar irradiance is crucial for understanding planetary energy balance, climate studies, solar energy applications, and astronomical research. It helps determine the energy available for solar power generation and influences climate modeling.
Tips: Enter the radius of the sun in meters, effective surface temperature in Kelvin, and mean distance between sun and planet in meters. All values must be positive numbers.
Q1: What is the typical value of solar constant for Earth?
A: The solar constant for Earth is approximately 1361 W/m², though it varies slightly with solar activity.
Q2: How does distance affect solar irradiance?
A: Solar irradiance decreases with the square of the distance from the sun (inverse square law).
Q3: Why is temperature raised to the fourth power?
A: This comes from the Stefan-Boltzmann law, which states that the total energy radiated per unit surface area is proportional to the fourth power of the temperature.
Q4: What factors can affect solar irradiance values?
A: Solar activity cycles, atmospheric conditions, and orbital variations can all affect measured solar irradiance values.
Q5: How is this calculation used in practical applications?
A: This calculation is used in climate science, astronomy, solar energy system design, and space mission planning.