3D Hill Topographic Effects

Interactive animation of wind flow around isolated hills

Interactive Wind Load Animation

Use the controls to adjust wind speed, exposure category, and watch real-time wind particle flow

Understanding 3D Hill Wind Loads

Three-dimensional axisymmetric hills are isolated topographic features that create wind speed-up effects from all horizontal directions. Unlike 2D ridges where wind direction matters significantly, 3D hills amplify wind loads regardless of wind approach angle, making them particularly important for structural design. These rounded, isolated hills are characterized by similar dimensions in all horizontal directions and include features like volcanic cones, drumlin hills, isolated mountain peaks, and man-made features like waste mounds and storage facilities.

What is a 3D Axisymmetric Hill?

In ASCE 7 terminology, a 3D (three-dimensional) axisymmetric hill is a topographic feature that is relatively uniform in all horizontal directions—essentially circular or oval in plan view. The term "axisymmetric" means the hill has rotational symmetry about a vertical axis through its peak. Wind approaching from any horizontal direction encounters similar slopes and experiences similar speed-up effects, distinguishing 3D hills from directionally-dependent 2D ridges.

Defining Characteristics

ASCE 7 Requirements for 3D Hills

ASCE 7 Section 26.8 addresses 3D axisymmetric hills with specific K1 values in Table 26.8-1 that are typically lower than those for 2D ridges and escarpments, reflecting the three-dimensional flow patterns.

ASCE 7 3D Hill Criteria

3D Hill topographic effects apply when ALL of the following are met:

  1. The hill is isolated and unobstructed for 100H or 2 miles
  2. The hill protrudes above upwind terrain by a factor of two or more
  3. The structure is in the speed-up region (typically 0 to 5H from summit)
  4. H/Lh ≥ 0.2 where H is hill height and Lh is distance to half-height
  5. Feature has approximately equal dimensions in plan (not elongated like a ridge)

Topographic Factor Calculation for 3D Hills

The topographic factor for 3D axisymmetric hills uses the same formula structure but with 3D-specific K1 values:

Kzt Formula for 3D Hills

Kzt = (1 + K1 K2 K3)²

K1 = shape factor for 3D axisymmetric hills (Table 26.8-1)
K2 = horizontal distance factor (radial from summit)
K3 = vertical height factor above ground

Calculation Procedure

  1. Measure H - Height of hill above surrounding terrain
  2. Determine Lh - Average radial distance from summit to half-height contour
  3. Calculate H/Lh - Confirm ≥ 0.2 for topographic effects to apply
  4. Select K1 - Use 3D axisymmetric hill values from ASCE 7 Table 26.8-1
  5. Determine K2 - Based on radial distance from summit (x/Lh)
  6. Calculate K3 - Based on height above local ground (z/Lh)
  7. Compute Kzt - Apply formula for all wind directions

Wind Flow Patterns Around 3D Hills

Understanding how wind behaves around isolated hills helps engineers appreciate why topographic factors matter:

Real-World 3D Hill Examples

Engineering Best Practices

Key Considerations for 3D Hill Design:

3D vs 2D Classification

Determining whether a topographic feature is 2D or 3D is critical for accurate Kzt calculation:

Professional Solution: Our wind load calculator automatically determines whether 2D or 3D topographic factors apply based on site geometry input, applies the correct K1 values from ASCE 7 tables, and calculates accurate Kzt for all applicable wind directions—eliminating guesswork and ensuring code compliance.

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