Summer Solstice Sun Angle Calculator

Find accurate solstice sun height with simple inputs. Compare noon, shadows, daylight, and surface angles. Use clear outputs for solar planning at your site.

Calculator Inputs

North positive, south negative.
Use 12 for solar noon.
0 is flat. 90 is vertical.
0 north, 90 east, 180 south.

Formula Used

The calculator uses standard solar geometry. Latitude is φ. Solar declination is δ. Local solar time is t.

Here, β is surface tilt, A is solar azimuth, and γ is surface azimuth.

How to Use This Calculator

  1. Select the June or December solstice model.
  2. Enter latitude as a signed value. North is positive. South is negative.
  3. Enter local solar time. Use 12 for solar noon.
  4. Add object height for shadow length.
  5. Add surface tilt and azimuth for incidence angle.
  6. Press the calculate button.
  7. Review the result panel shown above the form.
  8. Use the CSV or PDF button to save the result.

Example Data Table

Example place Latitude Solstice Noon altitude Daylight length Shadow ratio
New York 40.71° June 72.73° 14.92 hours 0.31 : 1
London 51.51° June 61.93° 16.41 hours 0.53 : 1
Quito -0.18° June 66.38° 11.99 hours 0.43 : 1
Sydney -33.87° December 79.57° 14.26 hours 0.18 : 1

Understanding Summer Solstice Sun Angles

The summer solstice gives the highest noon Sun for many northern sites. It also gives the longest daylight period. This calculator turns that geometry into useful numbers. It uses latitude, solstice type, solar time, object height, surface tilt, and surface direction. The result helps with site planning, garden layout, roof studies, shade checks, and basic astronomy lessons.

Why the Sun Angle Matters

Sun angle controls how high the Sun appears above the horizon. A high angle creates short shadows. A low angle creates long shadows. At solar noon on the June solstice, the Sun is directly above the Tropic of Cancer. On the December solstice, it is above the Tropic of Capricorn. This difference changes the altitude, zenith angle, daylight length, and shadow ratio for every location.

Planning With the Result

The noon altitude shows the best daily peak. The custom-time altitude shows what happens away from noon. The azimuth tells the compass direction of the Sun. Shadow length uses object height and the tangent of altitude. The daylight estimate uses the sunrise hour angle formula. These outputs are practical for outdoor work, solar sketches, window shade checks, and classroom examples.

Surface and Panel Use

The surface incidence angle compares the Sun ray with a tilted plane. A smaller incidence angle means the Sun is closer to perpendicular to that surface. This is useful for simple solar panel studies. It also helps compare wall, roof, and ground exposure. The calculator does not replace local weather data, horizon obstructions, or professional solar design. It gives a clean mathematical estimate from standard spherical geometry.

Accuracy Notes

Use signed latitude carefully. North is positive. South is negative. Local solar time is different from clock time when longitude and time zone effects are ignored. For fast planning, solar noon is 12. For detailed field work, adjust for longitude, time zone, and the equation of time. The solstice declination is rounded to 23.44 degrees, which is accurate enough for most educational and early planning needs. Always review nearby trees, buildings, hills, and seasonal access paths before choosing a final design. Real sites rarely have a perfectly open horizon line.

FAQs

What is a summer solstice sun angle?

It is the Sun height above the horizon on the summer solstice. The value changes with latitude and time of day. Noon usually gives the largest altitude.

Should I enter north latitude as positive?

Yes. Use positive values for north latitude. Use negative values for south latitude. For example, 40 means 40° north, and -33 means 33° south.

Why does the calculator use local solar time?

Solar geometry is based on the Sun position, not clock labels. Local solar noon happens when the Sun reaches its daily highest point.

What is the zenith angle?

The zenith angle is measured from the point directly overhead. It equals 90 degrees minus the Sun altitude angle.

How is shadow length calculated?

Shadow length equals object height divided by tangent of the Sun altitude. A higher Sun creates a shorter shadow.

Can this help with solar panel planning?

Yes. The incidence angle can compare solar exposure on tilted surfaces. Still, final panel design should include local weather and shading checks.

Why is the Sun altitude sometimes negative?

A negative altitude means the Sun is below the horizon at that solar time. Shadow length is not meaningful in that case.

Is the daylight length exact?

It is a mathematical estimate. It ignores refraction, terrain, nearby buildings, and horizon height. Real sunrise can differ slightly.

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