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Escarpments—cliffs, bluffs, and steep slopes—create some of the most dramatic wind speed-up effects in structural wind engineering. When wind encounters a sharp change in elevation, it accelerates as it flows up and over the escarpment face, creating a zone of increased wind speeds that can significantly amplify design pressures on structures. Understanding these topographic effects is critical for buildings located near coastal bluffs, river gorges, quarry edges, and natural or man-made escarpments where wind load amplification factors can exceed 50%.
In ASCE 7 terminology, an escarpment is a topographic feature characterized by a relatively steep slope with a cliff-like face. The upwind terrain approaches the feature at a relatively low elevation, then rises sharply to a higher elevation plateau. This sharp transition creates a significant change in terrain elevation over a relatively short horizontal distance, distinguishing escarpments from gradually sloping hills or ridges.
ASCE 7 Section 26.8 provides specific criteria and methodology for calculating the topographic factor Kzt for escarpments. The analysis involves determining three multipliers (K1, K2, K3) that account for different aspects of the topographic effect.
You must calculate Kzt > 1.0 when ALL of these conditions are met:
The topographic factor for escarpments is calculated using three multipliers that account for shape, horizontal position, and vertical position:
Kzt Formula for Escarpments
Kzt = (1 + K1 K2 K3)²
K1 = shape factor from Table 26.8-1 (based on H/Lh)
K2 = distance factor (based on x/Lh position)
K3 = height factor (based on z/Lh above ground)
Wind speed-up on escarpments is most pronounced in specific zones relative to the crest:
Critical Considerations for Escarpment Design:
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