Wind Loads on Buildings: Pressure, Uplift, and Code Requirements
Wind is not a single static force applied to a building's face. It is a dynamic, turbulent flow that creates positive pressure on windward surfaces, negative pressure (suction) on leeward and side walls, and complex uplift patterns across roofs. These pressures act simultaneously on every surface and must be resisted by a chain of structural elements running from the outermost cladding through the wall framing, floor diaphragms, and lateral force-resisting system down to the foundation. ASCE 7-22, Minimum Design Loads and Associated Criteria for Buildings and Other Structures, is the primary US reference for wind load determination, and its methods translate measured wind speeds into design pressures through a systematic procedure.
Wind Speed Maps and Risk Categories
ASCE 7-22 Chapter 26 begins with basic wind speed V, defined as the 3-second gust speed at 10 metres above ground in open terrain, expressed in miles per hour or metres per second. Wind speed maps in ASCE 7-22 Figures 26.5-1A through 26.5-1D provide values for four Risk Categories. Risk Category I (low occupancy buildings) uses a return period of approximately 300 years for the design wind speed. Risk Categories II (typical buildings), III (substantial hazard), and IV (essential facilities such as hospitals and emergency response centres) use progressively higher return periods, resulting in higher design wind speeds for the same location.
In Miami, a Risk Category II building might have a design wind speed of 185 mph (83 m/s). In Chicago, the same category gives approximately 115 mph (51 m/s). In inland areas away from hurricane exposure, speeds can be as low as 95 mph (42 m/s). The wind speed maps were derived from a comprehensive probabilistic analysis of historical wind records, and they represent a significant update from the older fastest-mile wind speed concept used in earlier editions of ASCE 7.
ASCE 7-22 uses 3-second gust speeds directly for design, eliminating the conversion factors needed under the older fastest-mile wind speed approach used before ASCE 7-05. The 3-second gust speed is consistently higher in magnitude than the mean hourly speed and corresponds to the peak loading on typical structural components.
Velocity Pressure and the qz Equation
The first step in converting wind speed to structural load is calculating the velocity pressure qz at height z above ground. ASCE 7-22 Eq. 26.10-1 gives:
qz = 0.00256 * Kz * Kzt * Ke * V^2 (in pounds per square foot, with V in mph)
Each coefficient accounts for a specific physical effect. Kz is the velocity pressure exposure coefficient, which reflects how wind speed increases with height above ground. It depends on the Exposure Category and height. At 10 metres in Exposure C, Kz = 1.0 by definition. At 30 metres, Kz rises to approximately 1.21. At 60 metres, it reaches about 1.35. At grade level, Kz is set to a minimum of 0.85 for Exposure B to avoid unrealistically low pressures.
Kzt is the topographic factor, which accounts for speed-up effects when wind flows over hills and escarpments. For flat terrain, Kzt = 1.0. On the crest of an isolated hill, Kzt can reach 1.3 or higher, significantly amplifying design pressures. Ke is the ground elevation factor introduced in ASCE 7-22, accounting for the lower air density at high elevations. At sea level Ke = 1.0; at 1,500 metres elevation it drops to approximately 0.85, reducing design pressures proportionally.
Exposure Categories and the Boundary Layer
The Exposure Category captures the roughness of the terrain surrounding the building, which determines how the wind velocity profile varies with height. Exposure B applies to suburban and urban areas with numerous closely spaced obstructions: trees, buildings, other structures at least 10 metres tall. The boundary layer is thick, wind speed at low heights is significantly reduced, and the velocity profile rises more steeply with height. Exposure C applies to open terrain with scattered obstructions less than 10 metres tall, including flat open country, grasslands, and shorelines facing away from large water bodies. Exposure D is the most severe, applying to flat unobstructed areas exposed to large bodies of water over a fetch of at least 1,500 metres, including ocean coastlines and large lake shores.
The selection of Exposure Category has a large influence on design pressures. A building in Exposure D at 10 metres above grade might experience a velocity pressure 30 to 40 percent higher than the same building in Exposure B, because the lower surface roughness allows the wind to retain higher speed near the ground. ASCE 7-22 Section 26.7 defines these categories in detail, and the selection requires careful assessment of the terrain in all wind directions, not just the predominant wind direction.
External and Internal Pressure Coefficients
Velocity pressure qz is multiplied by pressure coefficients to obtain net design pressures on each surface. The external pressure coefficient Cp from ASCE 7-22 Figure 27.3-1 depends on the building's plan geometry, roof slope, and the surface considered. For a typical enclosed rectangular building, the windward wall carries a positive external pressure coefficient of Cp = +0.8, acting as inward pressure. The leeward wall carries Cp = -0.2 to -0.5 depending on the building's depth-to-width ratio, acting as suction that pulls the wall outward. Side walls carry Cp = -0.7. Roof surfaces typically experience negative pressure (suction) across most of their area, with Cp ranging from -0.18 to -0.7 depending on roof slope, wind direction, and position on the roof.
Internal pressure coefficients GCpi account for the pressure inside the building, which depends on how enclosed or open the building is. For enclosed buildings (openings less than approximately 1 percent of the wall area), GCpi = +/-0.18, meaning internal pressure can be either slightly positive or slightly negative. For partially enclosed buildings, where large openings are present on the windward wall, internal pressure becomes strongly positive, with GCpi = +/-0.55. The worst case for any wall or roof element must be considered: outward pressure on the windward wall is the sum of external positive pressure plus internal suction; net uplift on a roof is the sum of external suction plus internal pressure pushing upward.
Main Wind Force Resisting System vs. Components and Cladding
ASCE 7-22 provides separate procedures for the Main Wind Force Resisting System (MWFRS) and for Components and Cladding (C&C). The distinction matters because wind load is not uniform across a surface; it peaks dramatically at corners, edges, and roof overhangs where local aerodynamic effects create much higher pressures than the average over a large area.
The MWFRS is the structural system that transfers wind loads from the entire building to the foundation: typically moment frames, shear walls, or braced frames. Because the MWFRS averages wind pressure over large tributary areas, the design pressures in Chapter 27 of ASCE 7-22 are moderate. A ten-story office building in Miami with Exposure C might have a design base shear from wind of 3 to 5 percent of its seismic weight.
Components and Cladding are designed for peak local pressures that can be two to three times the average MWFRS pressures. Corner zones of walls, eave and ridge regions of roofs, and roof edges experience dramatically elevated local suctions. ASCE 7-22 Chapter 30 defines effective wind areas and pressure coefficients GCp for C&C design. A metal panel at a roof corner might experience a design uplift pressure of -80 psf (-3.8 kPa) while the average roof design pressure for the MWFRS is only -30 psf. Roof-to-wall connections, cladding anchors, and window glazing are governed by these C&C provisions.
Dynamic Analysis, Gust Factor, and Flexible Buildings
For rigid buildings, defined as those with a fundamental natural frequency greater than 1 Hz (period less than 1 second), the gust factor G = 0.85 is a constant that accounts for dynamic amplification of the mean wind pressure by turbulent gusts. This standard gust factor is appropriate for most low to mid-rise buildings where the structural period is short relative to the duration of wind gusts.
Tall or slender buildings with fundamental periods exceeding 1 second are classified as flexible structures. Their natural frequencies can fall within the range of significant wind energy content, leading to resonant dynamic response that amplifies the mean wind pressure significantly. ASCE 7-22 Section 26.11 requires a calculated gust factor Gf for these structures, derived from the building's natural frequency, damping ratio (typically 1 to 2 percent of critical damping for steel buildings), and exposure characteristics. For a 50-story steel office building with a 5-second period, Gf might be 1.1 to 1.3, increasing the effective design pressure by 30 to 50 percent above the rigid building baseline.
Unusual building shapes such as tapered towers, buildings with setbacks, domes, or canopies generate complex aerodynamic flow patterns that the ASCE 7-22 tabular methods cannot accurately capture. For these buildings, Chapter 31 of ASCE 7-22 permits and in many cases requires wind tunnel testing using a scale model in a boundary layer wind tunnel that simulates the atmospheric turbulence at the building site. Wind tunnel testing typically yields lower design pressures than code methods for ordinary shapes, but for unusual shapes it is the only reliable method.
Combining Wind and Seismic Loads
ASCE 7-22 load combinations in Section 2.3 (LRFD) require wind to be checked separately from the design-level seismic event. The factored wind load combination is 1.0W in LRFD, combined with 1.2D + L + 0.5Lr (or S). The design seismic force combination 1.0E appears separately. ASCE 7-22 does not require the simultaneous application of the full design wind speed and the full Maximum Considered Earthquake ground motion, recognising that the probability of both occurring at their design levels simultaneously is extremely low. In practice, wind typically governs the lateral design of tall buildings in hurricane-prone regions such as the Gulf Coast, while seismic loads govern in high seismic zones such as coastal California and the Pacific Northwest, and both cases require careful drift control to maintain serviceability.