B.2.5—Solar constant S
- Syllabus
- First assessment 2025
- Objective
- —
- Level
- SL
Solar constant
The solar constant, S, is the solar-radiation intensity received per unit area at the Earth’s orbital distance, with the surface perpendicular to the incoming rays. Its units are W m⁻².
It is not the global mean
The solar constant describes the incident intensity on a surface facing the Sun. A planet’s spherical geometry spreads the intercepted power over a larger total surface, so the planet-wide mean incoming intensity is smaller.
Use it as an input
In an energy-balance problem, S is the incoming solar intensity before accounting for the planet’s projected area, albedo, atmospheric absorption or averaging over the whole sphere.
Common trap
Do not call the solar constant the total solar power intercepted by Earth. It is an intensity: power per unit area.
The evidence repeats a one-mark “state what is meant by the solar constant” prompt in a planetary energy-balance context.
State / Define
Define the solar constant as the solar-radiation intensity received per unit area at the Earth’s orbital distance, for a surface normal to the rays. Include “power per unit area” or intensity; do not call it total power.
Calling S total solar power or confusing S with the globally averaged S/4.
Representative question
State what is meant by the solar constant.
The intensity <<of solar radiation>> received by the Earth
Marking guidance:
Accept 'power per unit area' for
intensity.