Why does tap water sometimes come out cloudy white — then clear on its own?

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tl;dr
The white haze is millions of microscopic air bubbles. Cold, pressurized pipe water holds extra dissolved air; at the open tap the pressure vanishes, the surplus air un-dissolves as fog, and the bubbles rise and pop — clearing the glass from the bottom up in a minute or two.
Show the written answerThe written answer
That white, milky glass of tap water is not chlorine, minerals, or anything leaching from the pipes. It is air — millions of bubbles so small they hang in the water like fog. Water arrives at your faucet cold and under pressure, and both conditions let it carry extra air in solution — a taught term meaning the air is fully dissolved into the water itself, invisible. The instant the water leaves the tap, the pressure is gone. The USGS puts it plainly: the water is no longer under pressure, so the air comes out of solution as bubbles, much like a freshly opened soft drink. The bubbles rise, reach the surface, and pop. Within a minute or two the glass is clear again.
Air under pressure
A municipal system pushes water to your house at real force — a typical home plumbing line runs around 40 to 60 psi. Pressure is one of the two dials that control how much gas a liquid can hold: squeeze harder, and more air stays dissolved. Your glass, sitting open on the counter, is at roughly zero. Cross that gap in a fraction of a second and the water suddenly holds far more air than it can keep. The surplus has nowhere to go but out — as a burst of microscopic bubbles, everywhere at once. That is the cloud.
Why winter makes it worse
Temperature is the second dial, and it turns the same direction. Cold water holds more dissolved gas than warm water — near-freezing water can carry roughly twice the dissolved oxygen of warm water (about 14.6 milligrams per liter at 0°C, versus around 7 in the mid-30s °C). So in winter, the water reaching your house is loaded to the brim. Then it warms in your pipes and glass, which lowers what it can hold just as the pressure release does. Two dials, both dropping at once: that is why the milky-glass effect shows up mostly in cold months and often after the utility has worked on the lines, which can stir extra air into the mains.
The bottom-up test
Here is the field check, straight off the drafting table: fill a glass and set it down. If the haze is air, the glass clears from the bottom up — bubbles rise, so the clear zone grows upward as they escape at the surface. Total clearance time: a minute or two, no residue. If instead the water clears from the top down, or particles settle on the bottom, that is not air — that is sediment, and it is worth a call to your water utility. Air clouds are cosmetic. The plumbing is performing exactly as built.
cited
Sources
- [01]USGS Water Science School — Why is my drinking water cloudy?
“Once the water comes out of your tap, the water is no longer under pressure and the air comes out of solution as bubbles (similar to a carbonated soft drink).”
- [02]USGS Water Science School — Dissolved Oxygen and Water
“Cold water can hold more dissolved oxygen than warm water.”
people also ask
Keep asking
Is cloudy white tap water safe to drink?
Yes. When the haze clears on its own from the bottom up, it is plain air coming out of the water — harmless and tasteless. Utilities and the USGS class it as a cosmetic effect, not a contamination issue.
Why does my water turn cloudy mostly in winter?
Cold water can hold roughly twice the dissolved gas of warm water, so winter mains arrive loaded with air. When that water warms in your pipes and loses pressure at the tap, the extra air escapes as a fog of tiny bubbles.
How do I tell harmless air from actual sediment?
Fill a glass and watch. Air bubbles rise, so the water clears from the bottom up within a minute or two, leaving nothing behind. Particles that settle downward or leave residue are sediment — that is the case worth reporting to your utility.
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