Free Tool · EN 1991-1-3:2003

Snow Load Calculator

Derive EN 1991-1-3 snow actions for roofs. Computes characteristic ground snow load sk with altitude correction, roof shape coefficients μ12 per Table 5.2, exposure coefficient Ce (Table 5.1), thermal coefficient Ct, and design snow load s = μi·Ce·Ct·sk for undrifted and drifted cases in kN/m².

μ₁ = 0.80 μ₁ = 0.80 s = — s = — α ← b₁+b₂ →

EN 1991-1-3 §5.3 — roof shape coefficient distribution

National Annex divergence

NL NEN-EN 1991-1-3/NA:2011: single zone s_k = 0.56 kN/m² (flat country; linear altitude correction +0.10 kN/m² per 100m).

DE DIN EN 1991-1-3/NA:2012: four zones Z1/1a/2/3 (0.65–1.10 kN/m² at sea level); altitude formula s_k = max(s_k0, 0.31 + (A/256)²).

0.68 kN/m²
Governing design snow load s_max
DE Zone 2, A = 40m, α = 20°, Ce = 1.0

1. Ground snow load s_k (§4.1 + Annex C)

s_k,0 at sea level0.85 kN/m² altitude40 m methodde s_k at site altitude0.85 kN/m²

2. Exposure coefficient C_e (Table 5.1) / 3. Thermal coefficient C_t (§5.2(8))

C_e exposure coefficient1 C_t thermal coefficient1 exposure classnormal

4. Shape coefficient μ₁ (Table 5.2)

Case Slope 1 (μ) Slope 2 (μ)
Undrifted0.80.8
Drifted Case I0.40.8
Drifted Case II0.80.4

5. Design snow load s = μ·Ce·Ct·sk (eq. 5.1)

Case Slope 1 s (kN/m²) Slope 2 s (kN/m²)
Undrifted0.680.68
Drifted Case I0.340.68
Drifted Case II gov0.680.34

ψ factors (EN 1990 load combinations)

ψ₀0.5 ψ₁0.2 ψ₂0 noteNA override (DE)

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Snow loads integrated into full frame analysis

Pro automatically applies s_k, μ, and C_e/C_t to every rafter and portal frame in your drawing set — combined with wind (EN 1990 §6.4.3.2) and output to the fabrication drawing.

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FAQ

How is the characteristic ground snow load s_k determined?

EN 1991-1-3 uses national zone maps. s_k,0 is the reference value at sea level; altitude correction per Annex C eq. C.1: s_k = s_k,0 · [1 + (A/728)²]. For the DE NA: s_k = max(s_k,0, 0.31 + (A/256)²). For NL: single zone s_k = 0.56 + 0.10·(A/100) kN/m².

What is the shape coefficient μ₁?

μ₁ governs roof snow load: μ₁ = 0.8 for α ≤ 30°; linear decay to 0 at α = 60°; 0 above. This reflects that steep roofs shed snow more effectively. The drifted case uses 0.5·μ₁ on one slope (asymmetric).

When does the drifted case govern?

For duopitch roofs the drifted arrangement (one slope at 0.5·μ₁, other at μ₁) is checked alongside the undrifted symmetric case. The drifted case often governs the lighter (windward) slope at low pitches because of redistribution.

What does the valley accumulation coefficient μ₂ mean?

For multi-span (saw-tooth) roofs, wind and sliding snow accumulate in the valley. μ₂ = μ₁ + μ_w + μ_s, capped at 2.0. μ_w depends on bay widths and ridge-to-valley height; μ_s on sliding from steep slopes (α > 30°).