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ExplainerFluid DynamicsCoriolis Effect· 7 min read· in Opinion

Rossby Numbers Above 1,000 Prove Sinks Drain Blind to Earth's Rotation

The popular belief that water drains in opposite directions in different hemispheres is contradicted by fluid dynamics. The Rossby number reveals that the Coriolis effect is thousands of times too weak to influence a household sink.

By Deniz Kaya

In short

  • The Rossby number determines whether the Earth's rotation or a fluid's own inertia dictates its movement.
  • A household sink has a Rossby number above 1,000, meaning the Coriolis effect is thousands of times too weak to steer the water.
  • The direction a sink drains is determined entirely by the basin's geometry and the residual angular momentum from how it was filled.

The binding constraint for the Earth's rotation to steer a moving fluid is that the fluid's own inertia must be small enough for the planetary spin to matter. In fluid dynamics, this balance is measured by a single dimensionless figure known as the Rossby number.[1]

If the Rossby number is small, the Earth's rotation dictates the flow; if it is large, the fluid moves blind to the planet. For the water draining from a standard household sink, that constraint fails completely. The inertial forces of the water easily overpower the subtle pull of the spinning Earth.[1][3]

The myth that sinks and bathtubs drain counterclockwise in the Northern Hemisphere and clockwise in the Southern Hemisphere is one of the most enduring misconceptions in popular science. "Because the earth rotates, a fluid that flows along the earth's surface feels a 'Coriolis' acceleration perpendicular to its velocity," writes physicist Matthew R. Feinstein in a University of Southampton explainer.[3]

But the Coriolis acceleration is incredibly weak at human scales. It only dominates when a system is very large and lasts a long time, conditions that a bathroom sink never meets. To understand why the hemisphere does not matter in your kitchen, you have to look at the underlying math.[3]

The Rossby number illustrates how the Coriolis effect dominates large systems but vanishes at the household scale.

The Mechanics of the Coriolis Force

The Coriolis effect was first described mathematically in 1835 by the French engineer Gustave-Gaspard Coriolis. He was studying the transfer of energy in rotating machinery, not weather patterns, but his equations applied perfectly to the atmosphere.[2]

The effect describes how anything moving across a rotating surface appears to curve relative to that surface. Because the Earth is a sphere, the surface at the equator spins faster than the surface near the poles. As fluid moves north or south, it retains its initial eastward momentum, causing it to deflect.[2]

In the Northern Hemisphere, this deflection pushes moving air and water to the right. In the Southern Hemisphere, the deflection is to the left. This is the mechanism that steers the major ocean currents and dictates the rotation of massive storm systems.[2]

The Rossby Number Dictates the Scale

But knowing that the force exists is not enough; you have to know whether it is strong enough to matter. That question is answered by the Rossby number, named after the Swedish-American meteorologist Carl-Gustaf Rossby. The number is a simple ratio comparing a fluid's inertial force to the Coriolis force.[1]

The formula divides the fluid's velocity by the product of the Coriolis parameter and the length scale of the system. The Coriolis parameter depends on the latitude, but in the mid-latitudes, it is roughly 0.0001 radians per second. The resulting dimensionless number tells you exactly who is driving the fluid.[1]

When the Rossby number is much less than one, the Coriolis effect is the dominant steering force. The fluid is said to be in geostrophic balance, meaning the pressure gradient is perfectly opposed by the Coriolis deflection. This is the realm of global weather.[1]

In massive weather systems, the Coriolis deflection perfectly balances the pressure gradient.

Hurricanes Versus Household Plumbing

Consider a large mid-latitude weather system spanning 1,000 kilometers, with wind speeds of 10 meters per second. When you plug those figures into the equation, the Rossby number comes out to approximately 0.1. Because the number is so small, the Earth's rotation firmly dictates the spin.

That low Rossby number is why hurricanes and cyclones reliably spin counterclockwise north of the equator and clockwise south of it. The storm is so massive, and the air moves across such a vast distance, that the subtle planetary deflection has time to accumulate and steer the entire system.

A household sink operates on a completely different scale. The water moves relatively quickly—perhaps 0.2 meters per second—over a distance of just 30 centimeters. When you calculate the Rossby number for a draining basin, the result is well above 1,000, and often closer to 10,000.[3]

At a Rossby number of 1,000, the inertial forces of the water are a thousand times stronger than the Coriolis acceleration. The Earth's rotation is present, but it is entirely overwhelmed by the fluid's own momentum. The sink simply does not feel the planet spinning.[3]

What Actually Steers the Water

If the Coriolis effect is too weak to matter, something else must determine the direction of the swirl when you pull the plug. The answer lies in the initial conditions of the water and the physical geometry of the basin.[3]

The way the tap filled the bowl, a slight millimeter tilt in the plumbing, or the residual currents left over from washing your hands all impart a tiny amount of angular momentum to the water. Even a temperature gradient across the room can create a subtle convection current.[3]

As the physical scale of a fluid system increases, its Rossby number plummets, allowing the Earth's rotation to take over.

As the water moves toward the drain, the radius of its rotation decreases. Just like a figure skater pulling their arms in to spin faster, the conservation of angular momentum amplifies that initial, imperceptible rotation. By the time the water reaches the drain, the vortex is highly visible.[3]

Because these initial conditions are effectively random, a household sink can drain clockwise on one occasion and counterclockwise on another. The direction depends entirely on how the water was introduced and the shape of the container, making the hemisphere completely irrelevant.[3]

The Ascher Shapiro Experiment

Proving that the Coriolis effect can influence a draining tank requires extreme measures to eliminate every other variable. In the fall of 1962, MIT engineering professor Ascher Shapiro built a perfectly symmetrical, flat-bottomed circular tank, six feet across and six inches deep, to test the theory.[4]

Shapiro filled the tank with room-temperature water, deliberately swirling it clockwise while filling so that a later counterclockwise drain could not be blamed on the filling current. He then covered the tank with a plastic sheet and let it sit perfectly still for 24 hours.[4]

The long settling time was necessary to dissipate any residual angular momentum, driving the fluid's velocity down to an almost imperceptible crawl. By reducing the velocity and increasing the length scale, Shapiro artificially forced the Rossby number down until the Coriolis effect became the dominant force.[4]

When Shapiro finally pulled the plug at the end of a 20-foot hose, nothing happened for the first 15 minutes. Then, a pair of wooden slivers floating above the drain began to turn counterclockwise, eventually reaching one full rotation every three to four seconds.[4]

Illustration: Ascher Shapiro's 1962 experiment required a perfectly symmetrical tank and a 24-hour settling period to isolate the Coriolis effect.

Confirming the Physics Down Under

Shapiro published his results in the journal Nature in December 1962, proving that the Earth's rotation could select the direction of a vortex under strictly controlled conditions. But the true test of the Coriolis theory required replicating the experiment south of the equator.[4]

Three years later, a team at the University of Sydney, led by Lloyd Trefethen, built a similar apparatus in Australia. They applied the same rigorous controls, allowing the water to settle for a full day before carefully opening the drain.[3]

Just as the physics predicted, the Sydney team observed a clockwise swirl. The two experiments demonstrated that the Coriolis effect is real and acts exactly as expected, but only when practically every other variable has been painstakingly removed from the environment.[3]

Tornadoes and the Limits of Scale

The dominance of the Rossby number explains other rotational mysteries in nature, such as the behavior of tornadoes. While tornadoes are incredibly violent, they are relatively small in diameter, often measuring just a few hundred meters across.

Because of their high wind speeds and small size, tornadoes have a Rossby number of around 10. "For much smaller dimension systems... the Coriolis effect plays a much less significant role compared to the balance between the radial centrifugal forces and the pressure gradient," notes the LibreTexts classical mechanics reference.

Illustration: With a Rossby number of around 0.1, a hurricane is firmly steered by the rotation of the Earth.

As a result, while the vast majority of tornadoes in the Northern Hemisphere spin counterclockwise because they are spawned by larger, Coriolis-driven storm systems, a small percentage actually spin clockwise. The local dynamics of the thunderstorm dictate the rotation, not the hemisphere.

The draining sink myth persists because it takes a complex, invisible force and scales it down to something you can watch in your bathroom. But physics does not scale linearly. The same underlying law can be the dominant force in one setting and a rounding error in another.[5]

How we did this

Method
Calculated the magnitude difference in rotational influence by comparing the Rossby number of a standard household sink drain to that of a mid-latitude weather system.
What we found
The Earth's rotation exerts a steering force on a draining sink that is thousands of times weaker than the inertial forces of the water, proving that any observed swirl is dictated entirely by basin geometry and filling currents.
What we worked from
  • Rossby number of a large weather system: 0.1
  • Fluid velocity threshold for Coriolis significance in a bathtub: < 2×10^-6 m/s — University of Southampton
Limits of this analysis
The exact Rossby number for a sink varies based on the specific dimensions and drain speed, but it consistently remains orders of magnitude above the threshold where Coriolis forces matter.
Geophysical Fluid Dynamicists 40%Experimental Physicists 35%Meteorologists 25%
Geophysical Fluid Dynamicists
Argues that scale determines the dominant forces, using the Rossby number to separate weather from plumbing.
Experimental Physicists
Focuses on the extreme laboratory conditions required to isolate the Coriolis effect from residual inertia.
Meteorologists
Applies the Coriolis effect to large-scale atmospheric phenomena like hurricanes and ocean currents.

Perspectives this story doesn't cover

  • Plumbing Manufacturers
  • Science Educators

Sources

Source coverage

5 outlets

3 viewpoints surfaced

Geophysical Fluid Dynamicists 40%Experimental Physicists 35%Meteorologists 25%
  1. [1]WikipediaGeophysical Fluid Dynamicists

    Rossby number

    Read on Wikipedia →
  2. [2]WikipediaGeophysical Fluid Dynamicists

    Coriolis force

    Read on Wikipedia →
  3. [3]University of SouthamptonExperimental Physicists

    Which Way Will my Bathtub Drain?

    Read on University of Southampton →
  4. [4]WikipediaGeophysical Fluid Dynamicists

    Ascher H. Shapiro

    Read on Wikipedia →
  5. [5]Factlen Editorial TeamExperimental Physicists

    Synthesis by Factlen editorial team

    Read on Factlen Editorial Team →

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