Solar Angles – Fundamentals of Solar Positioning

In today’s rapidly evolving renewable energy landscape, optimizing solar panel installation is critical for maximizing energy production. Two fundamental parameters determine how effectively your solar panels capture sunlight: orientation and tilt. These factors, when properly calculated, can significantly increase your system’s efficiency and return on investment.

Orientation refers to the directional facing of your panels relative to the sun’s path (typically measured as azimuth angle), while tilt represents the angular position relative to the horizontal ground. Together, these parameters determine how directly sunlight strikes your panels throughout the day and across seasons.

The Science Behind Solar Angles

Solar energy optimization relies on understanding several interconnected angular relationships:

Solar Declination (δ)

The Earth’s axial tilt of 23.45° relative to its orbital plane creates a daily variation in the angle between the Earth-Sun line and Earth’s equatorial plane. This angle, known as solar declination (δ), can be calculated using:

δ = 23.45° × sin[360° × (284 + N)/365]

Where N represents the day of year (with January 1 = 1).

Solar Position Coordinates

The sun’s position is defined by:

  • Solar altitude (β): Angle between the sun and the horizontal plane
  • Solar azimuth (ϕ): Angular displacement from true south measured in the horizontal plane

Surface-Solar Relationships

For optimal energy capture, we must determine the angle of incidence (θ) between direct solar radiation and the panel surface normal. This depends on:

  • Surface tilt angle (Σ): Measured from horizontal
  • Surface azimuth (ψ): Direction the surface faces relative to true south
  • Surface-solar azimuth (γ): Angular difference between solar azimuth and surface azimuth

Calculating Optimal Panel Positioning

The angle of incidence (θ) for any surface with tilt angle Σ can be determined by:

cos θ = cos β × cos γ × sin Σ + sin β × cos Σ

For specific surface types:

Vertical Surfaces (Σ = 90°)

cos θ = cos β × cos γ

Horizontal Surfaces (Σ = 0°)

cos θ = sin β

Advanced Considerations for Solar Tracking

The sun’s position at any hour (τ) is expressed through the hour angle (ω):

ω = 15° × (τ – 12)

Where τ represents the solar time in hours, with morning hours negative and afternoon hours positive.

Solar altitude can be determined with:

sin β = sin δ × sin φ + cos δ × cos φ × cos ω

Where φ represents latitude.

More deep on solar angles?

The axis about which the earth rotates is tilted at an angle of 23.45 degrees to the plane of the earth’s orbital plane and the sun’s equator. The earth’s axis results in a day-by-day variation of the angle between the earth–sun line and the earth’s equatorial plane called the solar declination δ. This angle may be estimated by the following equation:

$$\delta = 23.45 \sin\left[\frac{360}{365}(284 + N)\right]$$

where N = year day, with January 1 + 1

To determine the angle of incidence θ between a direct solar beam and the normal to the surface, the surface azimuth ψ and the surface-solar azimuth γ must be known. The surface-solar azimuth is designated by γ and is the angular difference between the solar azimuth ϕ and the surface azimuth ψ. For a surface facing the east of south, γ = ϕ − ψ in the morning, and γ = ϕ + ψ in the afternoon. For surfaces facing the west of south, γ = ϕ + ψ in the morning and γ = ϕ − ψ in the afternoon. For south-facing surfaces, ψ = 0 degree, so γ = ϕ for all conditions. The angles δ, β, and ϕ are always positive.

Table 1: Solar Declination Values Throughout the Year (2025)

MonthRepresentative DayDay Number (N)Declination (δ)
January15th15-21.27°
February15th46-13.28°
March15th74-2.82°
April15th1059.41°
May15th13518.79°
June15th16623.31°
July15th19621.52°
August15th22713.78°
September15th2582.22°
October15th288-9.97°
November15th319-19.15°
December15th349-23.34°

Table 2: Optimal Fixed Tilt Angles by Latitude

Latitude (°N)Optimal Year-Round Tilt (°)Winter Optimal Tilt (°)Summer Optimal Tilt (°)
0 (Equator)01515
1010255
2020355
30304515
40405525
50506535
60607545

Table 3: Surface-Solar Azimuth (γ) Calculation Reference

Surface OrientationMorning CalculationAfternoon Calculation
East of Southγ = ϕ – ψγ = ϕ + ψ
West of Southγ = ϕ + ψγ = ϕ – ψ
Directly Southγ = ϕ (ψ = 0°)γ = ϕ (ψ = 0°)

Table 4: Solar Position Angles at Different Hours (Example for 40°N Latitude on May 15, 2025)

Solar Time (hr)Hour Angle (ω)Solar Altitude (β)Solar Azimuth (ϕ)
6:00-90°8.7°-110.8°
8:00-60°28.7°-88.7°
10:00-30°48.0°-53.8°
12:00 (noon)58.8°0.0°
14:0030°48.0°53.8°
16:0060°28.7°88.7°
18:0090°8.7°110.8°

Table 5: Estimated Energy Production Ratio by Orientation and Tilt (Normalized to Optimal)

Panel OrientationPanel TiltAnnual Energy RatioSummer Energy RatioWinter Energy Ratio
SouthLatitude1.000.981.00
SouthLatitude-15°0.981.000.93
SouthLatitude+15°0.970.931.00
EastLatitude0.850.870.81
WestLatitude0.850.870.81
SE/SWLatitude0.950.950.94
Horizontal0.890.950.76

Table 6: Solar Tracking System Comparison

Tracking System TypeEnergy Gain vs. FixedComplexityMaintenance RequirementsRelative Cost
Fixed (optimized)BaselineLowMinimalLow
Single-axis (E-W)+25-35%MediumModerateMedium
Single-axis (N-S)+15-20%MediumModerateMedium
Dual-axis+35-45%HighSignificantHigh
Seasonal manual adjustment+4-8%LowLow (quarterly)Very Low

These tables provide critical reference data for solar system design, allowing for quick evaluation of optimal configurations based on geographic location, installation constraints, and seasonal performance requirements.

Practical Applications

The position of the sun can be defined in terms of its altitude β above the horizon and its azimuth ϕ measured in horizontal plane.

Understanding these relationships allows us to:

  1. Determine optimal fixed panel positions based on location-specific parameters
  2. Calculate seasonal adjustments to maximize year-round production
  3. Evaluate potential benefits of tracking systems versus fixed installations
  4. Estimate energy production throughout different times of day and year