🌉 How Cities Work 〰 Vibration No background needed 8 min read

Why don't bridges and skyscrapers
collapse when they sway in the wind?

On a windy day, the upper floors of a skyscraper sway slowly. That sway is built into the design. Yet in 1940, a bridge in the United States collapsed in wind that wasn't even especially strong. And the explanation textbooks gave for decades was wrong.

Published: 2026.08.16 Difficulty: ★★☆ (no background needed) Formulas appear only in the final foldout
First, think about a swing

When you push a child on a swing, pushing hard doesn't make it swing higher. Only when the timing matches does a light push, repeated, build the swing bigger and bigger.

Every swing has a "speed it wants to swing at." A long swing goes slowly, a short swing goes fast. Push in time with that speed, and small pushes stack up into a big swing.

Bridges and buildings have exactly the same property. Each one has its own "speed it wants to sway at." Taller buildings sway more slowly; shorter ones sway faster.

So the first question an engineer asks is: "Is there anything nearby that pushes at that exact speed?"

1
When timing matches, small forces build into big sways

This is resonance. A crowd walking in step across a bridge, or an earthquake wave whose period matches a building's — once they match, the sway stacks up.

2
But the Tacoma Narrows collapse wasn't resonance

A steady wind doesn't push periodically. Yet the bridge twisted more and more on its own. It wasn't pushed — it grew the motion itself.

These two look alike but are different mechanisms. And they stayed confused in textbooks for a long time. Let's go through them in order.

① Resonance — matched timing builds up pushpush againpush again arc keeps growing ※ Only happens when push timing matches the swing's own period ② Tacoma Narrows — steady wind, self-grown twist steady wind (not periodic pushing) slight twist twist grows grows more twisted shape catches wind force that force twists it further not pushed — self-grown
Figure 1: Top is resonance. Only when a push is timed to the sway's own period do small forces stack into a big sway. Bottom is what happened at Tacoma Narrows. The wind was steady, not periodic. A slight twist caught force from the wind (red arrows), and that force twisted the deck further still — a loop that kept feeding itself.

First, what is resonance?

Every object has its own "speed it likes to sway at." Push a swing once and let go, and it keeps swinging at a fixed tempo, set by its length — you can't change that by pushing differently.

Push in time with that tempo, and each push adds force in the same direction. Even small pushes, repeated, add up to a big sway. That's resonance.

You can find examples everywhere.

How do bridges and buildings deal with this?

In design, engineers check "is there anything nearby that pushes at this building's own tempo?" Then they take steps such as:

Modern design doesn't try to "stop the sway" — it tries to "let it escape safely." Making a structure rigid to contain the sway just passes the force straight into the frame.

Skyscrapers swaying in the wind isn't
a design failure — it's by design.

So what actually happened at Tacoma Narrows?

In 1940, a suspension bridge completed in Washington State, USA, collapsed just four months after opening. Footage of the deck twisting violently and undulating apart is still used as science teaching material today.

The wind that day was around 20 metres per second — nowhere near a typhoon, just a strong breeze. The bridge had been designed to withstand far stronger winds.

For decades, this accident was explained as "a textbook case of resonance" — the idea that the period of wind-generated vortices matched the bridge's own sway speed. But this is wrong.

A study published in the 1990s showed the vortex-shedding period and the bridge's twisting speed did not match. And the wind that day blew steadily from one direction — there was no periodic push, like a hand timed to a swing, at all.

What really happened — a sway that grew itself

What actually occurred was a loop like this (bottom of Figure 1):

  1. Something makes the bridge deck twist slightly
  2. The tilted shape changes how the wind strikes it
  3. As a result, a force acts that increases the twist
  4. The twist grows further, and the cycle returns to step 2

The key point: there was no periodic push from outside. The bridge itself drew energy from a steady wind and grew its own sway. This is called self-excited vibration.

The difference from resonance is decisive. Resonance happens "when pushed at the matching timing," so it stops if the pushing stops. Self-excited vibration grows on its own, as long as the wind exceeds a certain speed. And the bigger the sway gets, the more force it draws in.

This bridge's deck was a flat, I-beam cross-section. It was a shape prone to twisting when hit by wind. Today's suspension bridge decks use smooth cross-sections like an aircraft wing, or shapes with gaps that let wind pass through. That's a direct lesson learned from this accident.

💡 Why did the wrong explanation stick around so long?

This accident stayed in textbooks as "an example of resonance" because, it's been argued, the explanation was simple and the footage was striking. Resonance is taught in secondary school; self-excited vibration is a university specialist topic. The easier explanation to teach was chosen, and it stuck.

Even after papers pointing out the error were published, it took a long time for the correction to spread. It's still cited today as an example of how "the easy explanation" can crowd out "the correct explanation."

🔎 Another famous case — a bridge shaken by people walking

In 2000, a new footbridge opened in London. On its first day, once large crowds began crossing, the bridge started swaying sideways. It was closed after two days, and it took over a year of fixes before it reopened.

The cause, again, wasn't simple resonance. When the bridge swayed slightly sideways, people unconsciously adjusted their balance and fell into step with the sway. Their footsteps then landed in unison, and the sway grew further. An unintended synchronization arose between people and bridge.

This wasn't "pushed periodically from outside" either — the system itself grew the sway — putting it in the same family as Tacoma Narrows.

Something you can check at home

🧪 A 3-minute observation: making resonance with string and weights
  1. Hang three strings of different lengths from a horizontal cord or curtain rail, and tie a weight (like an eraser) to each
  2. Hold the ends of the horizontal support and move it side to side at a slow, steady tempo
  3. Only the longest weight swings widely. The others barely move
  4. Speed up the tempo, and the weight that swings widely changes in turn

You're shaking with the same force each time, but which one responds changes. You can see with your own eyes that each has a different "speed it likes to sway at." This is the same reason different buildings suffer different amounts of damage from the same earthquake.

Summary

Bridges and buildings survive wind because engineers identify each structure's "own sway speed" and design so nothing pushes it there. And the Tacoma Narrows collapse wasn't resonance — the bridge itself drew energy from a steady wind and grew its own sway.

It wasn't pushed into swaying.
It grew the sway itself.

Flow generating its own rhythm also happens in the kitchen. In Why does water glug out in bursts when you turn a bottle upside down?, you can see how water and air trading places produces a regular rhythm.

Want to go deeper? — terms, formulas, and textbook connectionsRanges from junior-high science to active research, each labeled by level
How to read the labels below
  • JHSCovered in junior high school science
  • HSCovered in high school physics ("Physics Basics"/"Physics")
  • HS+High school "Physics," or advanced/column content in textbooks
  • UnivNot taught in high school — university-level specialist courses (vibration engineering, wind engineering)
  • ResearchNot settled fact even at university — an active research question

JHSTerms: words for talking about sway

HSChecking with a formula: how often should you push a swing?

Resonance is "matched timing makes it swing big." So what exactly is the timing you need to match, in seconds? That can be calculated.

① The formula itself

T = 2π √(L ÷ g)

T time for one full swingunit: seconds
L length of the stringunit: m
g strength of gravity9.8 m/s²
 square rootthe value that, squared, gives that number

Notice something odd here. The weight of whoever's riding doesn't appear in the formula. That means the swing's period doesn't change no matter who's on it. An adult or a child — same period. And that's exactly what happens in practice.

A formula like this tells you not only "what matters" but also "what doesn't".

② Plugging in numbers
Swing rope lengthL = 2.5 m
First, work out inside the brackets2.5 ÷ 9.8 ≒ 0.255
Find its square root0.505 × 0.505 ≒ 0.255, so the answer is about 0.505
Multiply by 2π (≒ 6.28)2 × 3.14 × 0.505 ≒ 3.2
AnswerT ≒ 3.2 seconds

Push once every 3.2 seconds and it swings highest. Push faster or slower and the pushes start cancelling each other out. Anyone who's ever pushed a swing already knows this rhythm in their body. Here it is, as a number.

③ The same idea applies to buildings

Buildings, too, swing back at a fixed speed when pushed. The exact calculation is complex, but as a rough rule of thumb, for steel-frame buildings, "number of floors × about 0.1 seconds" is sometimes used.

10-storey building10 × 0.1 = 1.0 sec
50-storey building50 × 0.1 = 5.0 sec
Wooden houseroughly 0.2–0.5 sec

This tells us something about damage patterns. A direct-hit earthquake carries strong short-period shaking, which matches wooden houses at 0.2–0.5 sec. Meanwhile, a large, distant earthquake carries slow, long-period shaking, which matches super-tall buildings at around 5 seconds. Buildings hundreds of kilometres from the epicentre swaying violently is attributed to this match.

※ These are rough figures. They vary with structure, shape, and ground conditions. Actual design calculations are done individually.

④ Practice: how do you halve the period?

Look closely at the formula: T is proportional not to L itself but to its square root. That means you'd need to cut the length to a quarter to halve the period. Let's check.

Cut length to a quarter2.5 ÷ 4 = 0.625 m
Inside the brackets0.625 ÷ 9.8 ≒ 0.0638
Its square root0.253 × 0.253 ≒ 0.0640, so about 0.253
Period2 × 3.14 × 0.253 ≒ 1.6 sec (exactly half of 3.2 sec)

Just as predicted. Plugging in numbers makes clear what "proportional to the square root" actually means. That's why a short pendulum swings so much more frantically than you'd expect.

HS+How sharp resonance is, and the role of damping

How large a sway resonance produces depends on the amount of damping. With zero damping, the amplitude would in theory grow without limit. Real structures always have some damping, so it settles at a finite value.

The quantity describing "how sharply something resonates" is the Q factor. A higher Q means a stronger response over a narrower range of periods. A wine glass sings well because it has a high Q; conversely, lowering Q (increasing damping) is a design goal for buildings.

A tuned mass damper's job is exactly to artificially add this damping. It attaches an "extra pendulum" tuned to the building's natural period, and swings out of phase with the building, soaking up the sway's energy.

UnivWhy self-excited vibration is fundamentally different from resonance

The forced-vibration equation is written m ẍ + c ẋ + k x = F₀ cos(ωt), with a periodic external force on the right-hand side. Resonance is when the response grows large as ω approaches the natural frequency.

In self-excited vibration, however, there's no periodic force on the right-hand side. Instead, the force appears as a function of the system's own motion, x and . In a structure sitting in a flow, this force can effectively act in the direction that cancels damping. If the overall damping coefficient turns negative, the amplitude grows exponentially.

What happened at Tacoma Narrows is understood as single-degree-of-freedom torsional flutter. Above a certain wind speed (the flutter onset speed), the system's effective damping turns negative, and it enters a state where the sway grows on its own. "Staying below this wind speed" is a design condition — simply making a structure strong enough to withstand high wind isn't enough.

Modern long-span bridges evaluate the flutter onset speed through wind-tunnel testing and numerical analysis, and address it by refining the cross-section — adding a central slot, fitting fairings, and similar measures.

ResearchWhat's still hard

Connections to textbooks, by level

LevelSubject / unitWhere in this article
JHSScience - Pendulums / Properties of sound / EarthquakesNatural sway speed, string-and-weight observation
HSPhysics - Simple harmonic motion and resonanceNatural period formula, rough building period figures
HS+Physics - Damped and forced vibration (advanced topic in many textbooks)Q factor, how dampers work
UnivVibration engineering, wind engineering, earthquake engineeringSelf-excited vibration, negative damping, flutter onset speed
ResearchStructural engineering (unresolved)Predicting damping, crowd synchronization, long-period ground motion
References and sources
  1. Billah, K. Y. & Scanlan, R. H., Resonance, Tacoma Narrows Bridge Failure, and Undergraduate Physics Textbooks, American Journal of Physics 59(2), 118–124, 1991 (the paper pointing out the error in the resonance explanation).
  2. Dallard, P. et al., The London Millennium Footbridge, The Structural Engineer 79(22), 17–33, 2001 (pedestrian-induced lateral sway).
  3. Simiu, E. & Scanlan, R. H., Wind Effects on Structures (a standard textbook of wind engineering).
  4. Explanatory materials on long-period ground motion from the Japan Meteorological Agency (気象庁) and the Building Research Institute (建築研究所).
  5. Guidelines on damping and vibration-control structures in buildings from the Architectural Institute of Japan (日本建築学会).

※ Figures such as natural period and wind speed vary greatly with structure and conditions. This article presents commonly used rules of thumb.

※ This article is a general-audience science explainer. The figures given are meant to aid understanding of the underlying mechanisms and are not actual design standards. For questions about a building's earthquake resistance or safety, please consult experts and your local authority.