Interactive animation of wind flow around isolated hills
Use the controls to adjust wind speed, exposure category, and watch real-time wind particle flow
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.
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.
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.
3D Hill topographic effects apply when ALL of the following are met:
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
Understanding how wind behaves around isolated hills helps engineers appreciate why topographic factors matter:
Key Considerations for 3D Hill Design:
Determining whether a topographic feature is 2D or 3D is critical for accurate Kzt calculation:
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