Skip to main content
DigiCalcs

如何计算Solar Irradiance

learn.whatIsHeading

Solar irradiance is solar power density reaching Earth's surface. It varies by location, time, clouds, and atmospheric conditions.

分步指南

  1. 1Direct normal irradiance (DNI): beam radiation perpendicular to surface
  2. 2Diffuse horizontal irradiance (DHI): scattered radiation from entire sky
  3. 3Global horizontal irradiance (GHI): total arriving at horizontal surface

例题解析

输入
Clear day, sea level, solar noon
结果
GHI ≈ 1000 W/m² (AM 1.5 standard spectrum)
Peak theoretical

常见错误注意事项

  • Using peak 1000 W/m² without accounting for clouds and seasons
  • Neglecting angle-of-incidence effects

常见问题

How does altitude affect irradiance?

Higher elevation reduces atmospheric path, increasing irradiance. 1000 m altitude ~10% higher than sea level.

Why do solar panels need tilting?

Tilting captures more direct irradiance. Optimal angle ≈ latitude for fixed systems.

准备好计算了吗?尝试免费的 Solar Irradiance 计算器

自己尝试一下 →

设置

隐私条款关于© 2026 DigiCalcs