Velocity Pressure qz Step by Step - How to Calculate qz with Kz, Kzt, Ke (ASCE 7-22 Eq. 26.10-1)
2:26Published October 31, 2026Narrated, with captions and a full transcript
How do you calculate wind velocity pressure qz? By ASCE 7-22 Equation 26.10-1, qz = 0.00256 Kz Kzt Ke V2 in psf, with V in mph. Kz comes from Table 26.10-1 for the exposure category at each height z, and the directionality factor Kd is NOT in this equation in ASCE 7-22 - it moved into the design pressure equation, Eq. 27.3-1. Reusing a spreadsheet from an earlier edition double counts it.
This is Step 1 of a full Chapter 27 Directional Procedure worked example on a gable-roof house (V = 100 mph, Exposure C, mean roof height h = 22 ft): Kz from Table 26.10-1, Kh interpolated at the mean roof height (0.916), one full hand substitution at z = 15 ft (21.76 psf), the velocity pressure profile at every height the building needs (qh = 23.45 psf), and a sensitivity check on exposure and wind speed.
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Questions this video answers
- What is the velocity pressure equation in ASCE 7-22?
- qz = 0.00256 Kz Kzt Ke V2 (Eq. 26.10-1), in psf with V in mph.
- Is Kd in the velocity pressure equation?
- No. In ASCE 7-22 Kd moved into the design pressure equation, Eq. 27.3-1; putting it in qz as well double counts it.
- Where does Kz come from?
- Table 26.10-1, by exposure category and height z, interpolated linearly between tabulated rows.
- How do you get Kh at the mean roof height?
- Interpolate Table 26.10-1 at h - here 22 ft between the 20 ft and 25 ft rows, Kh = 0.916.
- What is qz at 15 ft for 100 mph, Exposure C?
- 0.00256 x 0.85 x 1 x 1 x 1002 = 21.76 psf.
- Which surfaces use qh instead of qz?
- The leeward wall, both side walls, the roof and the internal pressure all use qh; only the windward wall varies with height.
- How much does exposure category change qh?
- Exposure B drops it to 16.28 psf (31% lower); Exposure D raises it to 28.06 psf (20% higher).
- How much does a 10% higher wind speed change pressure?
- About 21% - pressure grows with V2, so 110 mph gives qh = 28.37 psf.
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Transcript
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Velocity pressure qz - the equation
0:00Step one, velocity pressure. The velocity pressure equation. Zero point zero zero two five six, times K sub Z, times K sub Z T, times K sub E, times V squared, in pounds per square foot with V in miles per hour. Notice what is missing: K sub D, the directionality factor, is not in this equation in ASCE 7-22 — it moved into the pressure equation instead, equation 27.3-1. Reusing an old spreadsheet from an earlier edition here double counts it. Keep that in mind; we will use K sub D properly in Step 3.
Kz from Table 26.10-1
0:35K sub Z comes from Table 26.10-1. Here are the rows bracketing the heights this building needs, values exactly as tabulated, for exposure C.
Interpolating Kh at the mean roof height
0:46Between tabulated rows, interpolate linearly. At the mean roof height, twenty two feet — the number we found from the building drawing a minute ago — K sub H comes out to zero point nine one six. That twenty-two-foot mean roof height is the same number we found from the elevations at the very start — it is what makes this interpolation possible.
Hand substitution at z = 15 ft
1:08One full substitution, so the arithmetic is not a black box. At fifteen feet, Exposure C gives K sub Z equal zero point eight five. Zero point zero zero two five six, times zero point eight five, times one, times one, times one hundred squared — twenty one point seven six pounds per square foot.
The qz profile at every height
1:25And the full velocity pressure profile at every height this building needs. Twenty three point four five pounds per square foot, at h, is the workhorse value — the leeward wall, both sidewalls, the roof, and the internal pressure all use q sub H. Only the windward wall varies with height and uses q sub Z directly.
Sensitivity - exposure category and wind speed
1:43Same building, same height, run through the same engine three ways. Exposure B instead of C drops q sub H to sixteen point two eight — thirty one percent lower. Exposure D raises it to twenty eight point zero six — twenty percent higher. And wind speed matters even more: a ten percent increase, to one hundred ten miles an hour, raises q sub H to twenty eight point three seven — a twenty one percent jump in pressure, because pressure grows with velocity squared. Terrain roughness and wind speed are worth more than most member size decisions — classify them honestly, they deserve the first minutes of any wind calculation, not the last.
