Sunlight exposure and shade calculator

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Accurately calculating sunlight exposure and shade is critical for optimizing energy efficiency and plant growth.

This article explores formulas, tables, and real-world examples for precise sunlight and shade calculations.

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Example User Prompts for Sunlight Exposure and Shade Calculator

  • Calculate sunlight hours for a 45° roof tilt at 40° latitude on June 21.
  • Determine shade length for a 10-meter tree at 30° solar elevation angle.
  • Estimate daily solar radiation on a south-facing window in New York City.
  • Find optimal shading device size to block sunlight between 10 AM and 2 PM.

Comprehensive Tables of Common Values for Sunlight Exposure and Shade Calculations

ParameterTypical ValuesUnitsDescription
Solar Elevation Angle (α)0° to 90°Degrees (°)Angle between the sun and the horizon
Solar Azimuth Angle (γ)-180° to 180°Degrees (°)Sun’s horizontal direction relative to true south
Latitude (φ)-90° to 90°Degrees (°)Geographic coordinate north or south of the equator
Declination Angle (δ)-23.45° to +23.45°Degrees (°)Sun’s angular position relative to the equatorial plane
Hour Angle (H)-180° to 180°Degrees (°)Angular displacement of the sun from solar noon
Solar Constant (I₀)1361W/m²Average solar irradiance outside Earth’s atmosphere
Surface Tilt Angle (β)0° (horizontal) to 90° (vertical)Degrees (°)Angle between surface and horizontal plane
Shadow Length (L)Varies with object height and solar elevationMeters (m)Length of shadow cast by an object
Month/DayDeclination Angle (δ)Day Length (hours)Solar Noon Elevation (°) at 40° Latitude
March 21 (Equinox)1250°
June 21 (Summer Solstice)+23.45°15.173.45°
September 23 (Equinox)1250°
December 21 (Winter Solstice)-23.45°926.55°

Fundamental Formulas for Sunlight Exposure and Shade Calculations

1. Solar Declination Angle (δ)

The declination angle represents the sun’s angular position relative to the equator and varies throughout the year.

It can be approximated by the formula:

δ = 23.45 × sin(360/365 × (284 + n))
  • δ: Declination angle in degrees (°)
  • n: Day of the year (1 for January 1, 365 for December 31)

2. Solar Elevation Angle (α)

The solar elevation angle is the height of the sun above the horizon at a given time and location.

Calculated by:

α = arcsin[sin(φ) × sin(δ) + cos(φ) × cos(δ) × cos(H)]
  • α: Solar elevation angle (°)
  • φ: Latitude of the location (°)
  • δ: Declination angle (°)
  • H: Hour angle (°), calculated as 15° × (solar time – 12)

3. Solar Azimuth Angle (γ)

The solar azimuth angle defines the sun’s horizontal direction relative to true south.

Calculated by:

γ = arccos[(sin(δ) × cos(φ) – cos(δ) × sin(φ) × cos(H)) / cos(α)]
  • γ: Solar azimuth angle (°)
  • Positive values indicate west of south, negative east of south

4. Shadow Length (L)

Shadow length is the horizontal distance cast by an object due to sunlight.

Calculated by:

L = h / tan(α)
  • L: Shadow length (meters)
  • h: Height of the object casting the shadow (meters)
  • α: Solar elevation angle (°)

5. Incident Solar Radiation on Tilted Surface (I)

Calculates solar radiation on a surface tilted at an angle β from horizontal.

I = I₀ × [sin(α) × cos(β) + cos(α) × sin(β) × cos(γ – γₛ)]
  • I: Solar radiation on tilted surface (W/m²)
  • I₀: Solar radiation on horizontal surface (W/m²)
  • α: Solar elevation angle (°)
  • β: Surface tilt angle (°)
  • γ: Solar azimuth angle (°)
  • γₛ: Surface azimuth angle (°), 0° = south-facing

Detailed Real-World Examples of Sunlight Exposure and Shade Calculations

Example 1: Calculating Shadow Length of a Tree at Solar Noon

Consider a 10-meter tall tree located at 35° latitude on June 21 (summer solstice). Calculate the shadow length at solar noon.

  • Step 1: Determine the declination angle (δ) for June 21.

From the table, δ = +23.45°.

  • Step 2: Calculate the solar elevation angle (α) at solar noon (H = 0°).

Using the formula:

α = arcsin[sin(35°) × sin(23.45°) + cos(35°) × cos(23.45°) × cos(0°)]

Calculate:

  • sin(35°) ≈ 0.574
  • sin(23.45°) ≈ 0.398
  • cos(35°) ≈ 0.819
  • cos(23.45°) ≈ 0.917
  • cos(0°) = 1

Therefore:

α = arcsin[(0.574 × 0.398) + (0.819 × 0.917 × 1)] = arcsin[0.228 + 0.751] = arcsin[0.979] ≈ 78.5°
  • Step 3: Calculate shadow length (L):
L = h / tan(α) = 10 / tan(78.5°)

Calculate tan(78.5°) ≈ 4.7

Thus:

L = 10 / 4.7 ≈ 2.13 meters

Result: The tree’s shadow length at solar noon on June 21 is approximately 2.13 meters.

Example 2: Estimating Solar Radiation on a Tilted Solar Panel

A solar panel is installed at 30° tilt facing true south (γₛ = 0°) at 40° latitude on March 21 (equinox) at 10 AM solar time. Calculate the incident solar radiation.

  • Step 1: Calculate the declination angle (δ) for March 21.

From the table, δ = 0°.

  • Step 2: Calculate the hour angle (H):

H = 15° × (solar time – 12) = 15° × (10 – 12) = -30°

  • Step 3: Calculate solar elevation angle (α):
α = arcsin[sin(40°) × sin(0°) + cos(40°) × cos(0°) × cos(-30°)]

Calculate:

  • sin(40°) ≈ 0.643
  • sin(0°) = 0
  • cos(40°) ≈ 0.766
  • cos(0°) = 1
  • cos(-30°) ≈ 0.866

Therefore:

α = arcsin[0 + 0.766 × 1 × 0.866] = arcsin[0.663] ≈ 41.5°
  • Step 4: Calculate solar azimuth angle (γ):
γ = arccos[(sin(0°) × cos(40°) – cos(0°) × sin(40°) × cos(-30°)) / cos(41.5°)]

Calculate numerator:

  • sin(0°) × cos(40°) = 0
  • cos(0°) × sin(40°) × cos(-30°) = 1 × 0.643 × 0.866 = 0.557
  • Numerator = 0 – 0.557 = -0.557

Calculate denominator:

  • cos(41.5°) ≈ 0.75

Therefore:

γ = arccos(-0.557 / 0.75) = arccos(-0.743) ≈ 137.8°

Since γ > 90°, the sun is west of south.

  • Step 5: Calculate incident solar radiation (I).

Assuming solar radiation on horizontal surface I₀ = 800 W/m² (typical clear day value):

I = 800 × [sin(41.5°) × cos(30°) + cos(41.5°) × sin(30°) × cos(137.8° – 0°)]

Calculate components:

  • sin(41.5°) ≈ 0.662
  • cos(30°) ≈ 0.866
  • cos(41.5°) ≈ 0.75
  • sin(30°) = 0.5
  • cos(137.8°) ≈ -0.743

Calculate bracketed term:

(0.662 × 0.866) + (0.75 × 0.5 × -0.743) = 0.573 – 0.279 = 0.294

Therefore:

I = 800 × 0.294 = 235.2 W/m²

Result: The solar panel receives approximately 235.2 W/m² at 10 AM on March 21.

Additional Technical Considerations for Sunlight and Shade Calculations

  • Atmospheric Effects: Solar radiation reaching the surface is affected by atmospheric conditions such as cloud cover, aerosols, and air mass. Models like the Clear Sky Model or empirical data can refine calculations.
  • Solar Time vs. Clock Time: Solar time accounts for the sun’s position relative to the local meridian and differs from standard clock time due to time zones and daylight saving.
  • Surface Orientation: Azimuth and tilt angles of surfaces significantly influence incident solar radiation and shading patterns.
  • Shadow Casting Objects: Complex geometries require vector-based calculations or 3D modeling software for accurate shadow mapping.
  • Seasonal Variations: Declination angle changes throughout the year, affecting sunlight duration and intensity.

Authoritative Resources and Standards

Understanding and accurately calculating sunlight exposure and shade is essential for architects, engineers, horticulturists, and energy professionals. This article provides the foundational knowledge, formulas, and practical examples necessary to perform these calculations with confidence and precision.