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Overhang Eave Depth Calculation by Latitude for Passive Solar

How to calculate the correct eave overhang depth for passive solar shading at your latitude. MÉTODO explains the geometry, the formula, and how it informs section design.

MÉTODO Arquitectos · 8 de junio de 2026 · 7 de lectura

MÉTODO · CDMX × Denver

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Overhang Eave Depth Calculation by Latitude for Passive Solar

The overhang depth for a passive solar house is not a design preference — it is a calculation. The geometry of the sun's arc across the sky at your latitude determines exactly how much horizontal projection above a south-facing window is required to block summer sun while admitting winter sun. This is one of the oldest calculations in architecture and one of the most reliable.

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The Solar Geometry at the Foundation of the Calculation

The sun's altitude angle at solar noon changes with the seasons. At the summer solstice, it reaches its maximum height above the horizon. At the winter solstice, it is at its lowest. The difference between these two angles is what makes a fixed overhang a functional shading device.

At Denver (39.7 degrees north latitude):

  • Summer solstice noon sun altitude: approximately 73.3 degrees
  • Winter solstice noon sun altitude: approximately 26.3 degrees

The spread between these two is about 47 degrees. That spread is what a fixed overhang exploits. The overhang projects far enough to intercept the high summer sun while the low winter sun passes beneath it and enters the glazing.

The Basic Formula

For a horizontal overhang at the top of a south-facing window:

Overhang projection = window height / tan(summer noon altitude)

At Denver, tan(73.3°) = 3.35

For a 1.8-meter-tall window:

  • Overhang projection = 1.8 / 3.35 = approximately 0.54 meters

This means a 54-centimeter horizontal projection above the window will provide full shade at summer solstice noon and allow full solar exposure at winter solstice noon.

Adjusting for Real Performance Goals

The basic formula optimizes for the solstice moments. In practice, you want the shading to extend a bit further into the shoulder seasons:

  • Summer cooling concern: you want shading to begin in late May and continue through late September, not just on June 21
  • Winter heating benefit: you want solar access to begin in late September and continue through late March

Adjusting to shade the window from April 21 through August 21 (a common design target), using the noon altitude of approximately 61 degrees on April 21 at Denver latitude:

  • Overhang projection = 1.8 / tan(61°) = 1.8 / 1.80 = 1.0 meters

This is nearly double the solstice-only calculation. The practical resolution is often an intermediate overhang dimension (0.7 to 0.75 meters) combined with interior shades or exterior roll-down screens for the early and late summer periods when the overhang alone is insufficient.

Latitude Comparison: Denver vs Mexico City

The section as narrative: the section drawing through the south facade at two latitudes tells two different stories.

At Mexico City (19.4 degrees north latitude):

  • Summer noon altitude: approximately 87 degrees (nearly vertical)
  • Winter noon altitude: approximately 43 degrees
  • A shallow overhang of 0.3 meters provides substantial summer shading because the summer sun is nearly overhead

At Denver (39.7 degrees north):

  • Summer noon altitude: 73 degrees
  • Winter noon altitude: 26 degrees
  • A 0.54-meter overhang achieves the equivalent summer shading at solstice

At higher latitudes (45 degrees north, northern Colorado or Montana):

  • Summer noon altitude: approximately 68 degrees
  • Winter noon altitude: approximately 21 degrees
  • Required overhang depth increases again; the lower winter sun angle also means deeper penetration of winter solar gain into the room

In MÉTODO, we design in both Mexico and the Mountain West. The overhang depth calculation runs every time, because the latitude difference between a project in Mexico City and a project in Denver changes the geometry by a factor that affects every solar-facing element of the design.

East and West Overhangs: Why They Do Not Work the Same Way

The horizontal overhang calculation only works for south-facing surfaces (in the northern hemisphere). East and west-facing glazing receives sun at low angles in the morning and afternoon — when the sun is near the horizon. A horizontal overhang at the top of an east or west window provides almost no shading benefit because the low-angle sun passes under it.

For east and west glazing, shading must come from:

  • Vertical fins that block the low-angle sun from the sides
  • Deep setbacks within the building mass
  • Overhanging trees or site features
  • Interior or exterior roller shades

This is one reason we minimize east and west glazing in passive solar designs and concentrate glazing on the south face where the geometry works.

The Section Drawing as the Verification Tool

The verification of the overhang calculation happens in the section drawing. Draw the summer solstice noon sun angle as a ray from outside the building through the section. If the ray is blocked by the overhang before it reaches the glass, the shading is adequate. Draw the winter solstice noon sun angle. If it passes below the overhang and enters the glazing to reach the thermal mass on the floor, the design is working.

This takes minutes with a protractor and a scaled section. There is no substitute for drawing it.

Próximos pasos

Overhang design is resolved in the section drawing during schematic design — before structural and framing decisions are made. We include sun angle analysis in our early design deliverables for passive solar projects.

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Preguntas frecuentes

How do you calculate overhang depth for passive solar shading?

The basic formula is: overhang projection = window height divided by tangent of the summer noon solar altitude. At 39.7 degrees north latitude (Denver), the summer solstice noon altitude is approximately 73 degrees, giving a tangent of about 3.3.

Should the overhang block sun in summer or admit sun in winter?

Both. A correctly sized overhang at south-facing glazing should provide full shade at summer solstice noon and allow full solar penetration at winter solstice noon. The latitudinal difference in sun altitude makes this geometrically possible.

Does the overhang depth change by latitude?

Yes significantly. At 25 degrees north latitude (Mexico City), the summer noon sun is very high and a shallow overhang provides shade. At 45 degrees north, the summer sun is lower and a longer overhang is needed for the same shading effect.

What adjustments does MÉTODO make beyond the basic formula?

We adjust for the thermal transition period — we want the overhang to begin admitting sun in early September (not just December) and to block sun through late October. This shifts the overhang geometry slightly beyond the solstice-only calculation.

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