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Units & Measurements

Solar Constant

Radiant power of the sun per square metre at the top of Earth's atmosphere -- approximately 1,361 W/m².

Also known as: Solar Irradiance Constant

What Is the Solar Constant?

The solar constant indicates the radiant power of the sun hitting a surface of one square metre oriented perpendicular to the radiation at the top of Earth’s atmosphere. Its value is approximately 1,361 W/m².

Physical Background

The solar constant is not exactly constant but fluctuates slightly:

FactorVariation
Elliptical Earth orbit+/- 3.4% (perihelion vs. aphelion)
Sunspot cycle (11 years)+/- 0.1%
Long-term fluctuationsVery minor

Relationship to the Earth’s Surface

Of the 1,361 W/m² at the edge of the atmosphere, a maximum of approximately 1,000 W/m² reaches the Earth’s surface under clear skies. The difference is absorbed and reflected by the atmosphere. This value of 1,000 W/m² is also used as the basis for the Standard Test Conditions (STC) of solar modules.

Significance for Photovoltaics

The solar constant defines the theoretically maximum available solar energy. In practice, it is used for the following calculations:

  • STC conditions are based on 1,000 W/m² (ground level)
  • Yield estimates account for the actual irradiance at the location
  • Comparison of solar resources at different locations

Practical Tip

The Standard Test Conditions (1,000 W/m²) correspond to a clear summer day around noon. The annual average irradiance in Germany is only about 125 W/m² — this shows how much weather and time of day affect the yield.