Everyday Mysteries Fluids No background needed ~6 min read

Why does tap water get thinner as it falls?
― No water is vanishing. It's just in a hurry

Open a tap just a little, and the stream of water is thickest at the spout and gets thinner as it falls. The water isn't disappearing along the way. As it falls it speeds up, so the same amount of water fits through a narrower channel. And once the stream gets thin enough, it slices itself into drops.

Published: 2026.10.06 Difficulty: ★☆☆ (no background needed) Formulas appear only in the final collapsible section
First, picture this scene

You turn the kitchen tap gently to fill a glass. The water that comes out looks like a clear glass rod — so still it almost seems frozen in place.

Look closely, though, and that rod is thick at the top and tapers as it goes down. Near the bottom of the sink, the surface sometimes turns bumpy and scatters into little drops.

We see this every single day, yet almost nobody ever explains why it happens.

Just two reasons

1
The faster it falls, the thinner it gets

The amount of water leaving the tap each second is the same at every height. Lower down, the water is moving faster, so a thinner stream is enough to carry the same amount.

2
Surface tension pinches the thin stream into drops

Water's surface always tries to shrink to the smallest area possible. A long thin column wastes a lot of surface area, so a pinch point grows and grows until the stream snaps into drops.

The first reason explains why the shape tapers; the second explains why it finally breaks. Let's look at each in turn.

Thinner, exactly in proportion to how much faster it goes

Tap water neither gains nor loses volume along the way. One second after leaving the spout, the water has always moved down to the next level. So the amount of water passing any cross-section each second is the same — right at the spout, 10cm below, or 20cm below.

But the water keeps speeding up as it falls. Fast-moving water can carry the same amount through a narrower channel. It's a bit like a road: where cars move faster, they spread further apart. Water does something similar, except instead of spreading apart, the column itself gets narrower.

Try the slider in Figure 1 to change how hard the tap is opened (the water's speed at the spout). Open it gently, and the stream accelerates a lot right after the spout, so it narrows sharply. Open it hard, and the water is already fast, so falling barely changes its speed ratio — the stream stays almost straight.

Tap Bottom of sink 0 cm 10 cm 20 cm Just below spout (slow) Thickness 1.0 cm / Speed 0.5 m/s Water passing per second is the same at every height → Faster flow means a thinner stream 20 cm down (fast) Thickness 0.49 cm / Speed 2.0 m/s
Moving the slider changes how the stream narrows
Figure 1: Side view of a stream of water falling from a tap. The ruler on the left shows the distance fallen. The dashed labels show the thickness and speed just below the spout (top) and 20cm below (bottom). The slider shows that opening the tap more gently makes the stream thinner lower down (breaking into drops near the bottom is left out of this figure).

If the spout thickness is 1cm and the speed is 0.5m per second, falling 20cm roughly quadruples the speed. The cross-sectional area drops to a quarter, so the thickness (diameter) is almost halved. Figure 1's starting values are exactly this case.

A thin stream snaps itself into drops

Water's surface behaves like a stretched rubber membrane, always pulling itself inward. This is surface tension. For the same amount of water, a round drop needs less surface area than a long thin column.

Tiny, invisible ripples are always present on the stream's surface, stirred up by small vibrations in the tap. Where the stream pinches in, the surface curves more sharply, pushing inward harder. The water squeezed out there escapes into the bulging parts nearby, so the pinch keeps getting tighter (Figure 2).

Top: smooth column Looks clear, like a glass rod Middle: pinch grows Red arrows: thinner spots push inward harder Yellow arrows: squeezed water escapes to the bulge Bottom: splits into drops Small drops often get trapped between big ones
Figure 2: A thin water column breaking into drops, top to bottom over time. The left-right arrows in the middle show the surface tension pushing a pinch inward; the up-down arrows show squeezed water moving into the bulge. At the bottom the column has split into a row of round drops.

As in the bottom of Figure 2, once the column breaks it leaves a row of round drops. A tiny drop often gets trapped between two larger ones. The thinner the falling stream gets (reason 1), the stronger surface tension's effect becomes, relatively speaking. That's why a gently-opened, thin stream turns into drops over a shorter distance.

💡 Why does the stream turn cloudy when you open the tap hard?

Open the tap wide, and the stream loses its glass-rod clarity, turning whitish and rough-looking. The flow becomes turbulent inside the spout, and the surface ripples finely, scattering light in all directions. If you want to see a clear stream, the trick is to open the tap just a little.

💡 Inkjet printers use this same effect

The way a liquid column breaks into evenly-spaced drops has been used by some printers to produce uniform ink droplets. The very phenomenon you see in your kitchen sink has also become a manufacturing tool.

In short

Tap water gets thinner going down not because water is disappearing, but because it speeds up as it falls. Since the same amount passes any point each second, a faster spot needs only a thinner column. And once the stream is thin enough, surface tension pinches it in and it finally splits into drops.

Water gets thinner the faster it hurries.
Once too thin, it rounds itself up into drops.

For more on the "round shape" that surface tension makes, see Why does a soap film stay round even on a square frame?, and for how poured liquid clings to an edge, see Why does liquid poured slowly from a kettle dribble down the outside?

🧪 Try it at your own kitchen tap
  1. Open the tap just a little to make a clear stream. Hold a ruler right behind the flow and compare the thickness just below the spout with the thickness about 15cm lower.
  2. Open the tap bit by bit and watch the tapering become more gradual (the same as moving Figure 1's slider to the right).
  3. Film near the bottom of the sink in slow motion on your phone. You may catch the moment the stream pinches and snaps into drops.

Don't leave the water running — turn it off as soon as you've checked. It's easier to see with a dark background and light from the side.

Want to go deeper? ― terms, formulas, and textbook linksWe mark which level each part belongs to, from middle-school science to university-level courses
How to read the labels below
  • MSCovered in middle-school science
  • HSCovered in high-school physics
  • HS+Advanced high-school content, or a textbook sidebar topic
  • UnivNot covered in high school — a university specialist subject (fluid dynamics)
  • ResearchNot yet settled even at university level — something researchers are actively studying

MSTerms: this phenomenon has names

MSHSChecking with a formula: how thick is the stream 20cm down?

Let's find the thickness of a thin stream, 1cm thick at the spout with a speed of 0.5m per second there, after falling 20cm.

⓪ The base formulas
In symbolsA₀ × v₀ = A × v ,  v = √( v₀² + 2 × g × h ) ,  d = d₀ × √( v₀ ÷ v )
In words(Cross-sectional area × speed) is the same at every height. The speed after falling is set by the speed at the spout and the height fallen. The thickness (diameter) shrinks in proportion to the square root of the speed ratio.
Where it comes fromThe first comes from water neither gaining nor losing volume along the way (conservation of mass = the continuity equation). The second comes from potential energy turning into kinetic energy while falling (conservation of energy). Since cross-sectional area is proportional to the square of the diameter, the third formula follows.
SymbolMeaning and unit
A₀, ACross-sectional area of the stream at the spout, and after falling (square metres)
v₀, vSpeed of the water at the spout, and after falling (m/s)
d₀, dThickness (diameter) of the stream at the spout, and after falling (cm)
gGravitational acceleration (about 9.8 m/s²)
hHeight fallen from the spout (m)
① Starting values
Thickness at spout1 cm
Speed at spout0.5 m/s
Height fallen20 cm (0.2 m)
Gravitational acceleration9.8 m/s²
② Working it out
2 × gravitational acceleration2 × 9.8 = 19.6
Multiply by height fallen19.6 × 0.2 = 3.92
Speed at spout, squared0.5 × 0.5 = 0.25
Add together0.25 + 3.92 = 4.17
Speed after fallingthe square root of 4.17 is about 2.04 (about 2 m/s)
How many times faster2.04 ÷ 0.5 ≒ 4.1
Fraction of original cross-section1 ÷ 4.1 ≒ 0.24
Thickness ratiothe square root of 0.24 is about 0.49
Thickness 20cm down1 × 0.49 = 0.49 (cm)

Falling just 20cm roughly quadruples the speed, cuts the cross-section to about a quarter, and nearly halves the thickness to about 5mm. That's why the stream visibly thins over the short drop to the sink.

HSHS+One step further on speed and thickness

HSThe falling-speed formula is exactly the constant-acceleration equation "v² − v₀² = 2gh". Air resistance is considered negligible at this speed and distance. Each part of the stream is simply doing the same free-fall motion, just starting at a different moment.

HS+The smaller the spout speed, the bigger the speed ratio after falling, and the thinner the stream becomes. Conversely, if the spout speed is large, the ratio stays close to 1 and the stream barely narrows. The difference you see with Figure 1's slider is exactly this ratio. Bernoulli's principle also applies directly to the flow inside the pipe and near the spout.

UnivHow the column snaps into drops: the Plateau–Rayleigh instability

In fluid dynamics, the way a liquid column pinches and breaks into drops is called the Plateau–Rayleigh instability, studied experimentally by Plateau and theoretically by Lord Rayleigh in the 19th century. Only ripples with a wavelength longer than the column's circumference grow, and the fastest-growing wavelength is about 9 times the column's radius. As a result, the size of the resulting drops is largely set by the column's thickness, with a diameter a little under twice that of the column. The "Weber number", which compares surface tension against inertia, and the "Ohnesorge number", which captures the effect of viscosity, are used to classify how the breakup happens.

📖 For the derivation and further reading: Continuity equation (Japanese Wikipedia) / Plateau–Rayleigh instability (English Wikipedia)

ResearchWhat's still not fully understood

In other words, even this article is only "the explanation as far as we currently understand it." Even the water in your everyday sink still holds unanswered questions.

Links to textbooks (by level)

LevelSubject / unitWhere in this article
MSScience, "Motion and energy"Falling faster as it goes down
HSPhysics, "Uniformly accelerated linear motion" / "Conservation of mechanical energy"Calculating the speed 20cm down
HS+Physics (advanced), "Fluids / Bernoulli's principle"The continuity equation and stream thickness
UnivFluid dynamics, "Interface instability"How the column breaks into drops
ResearchInterfacial fluid dynamics / droplet formationWhere it breaks, satellite droplets
―Everyday connectionsHow far you open the tap, ink droplets, sprays

※This article is a general-audience science explainer. The figures given are approximations to help build understanding. The actual stream thickness and breakup point depend on the shape of the tap and the water pressure.