Yes, warm water can freeze before cold water in some setups, but evaporation, airflow, and supercooling decide whether it happens.
The reason people keep asking whether hot water freezes faster than cold water is simple: sometimes it does, and sometimes it doesn’t. That sounds slippery, but it’s the honest answer. The effect has a name, the Mpemba effect, and it has been argued over for decades because “freezes faster” can mean a few different things and tiny setup changes can flip the result.
If you want the plain takeaway early, here it is. Hot water is not always faster. Still, under the right conditions, a hotter sample can beat a colder one to ice. That can happen when the hot sample loses more mass to evaporation, mixes heat more quickly through convection, makes better contact with a cold surface, or avoids the deeper supercooling that can delay freezing in a colder sample.
Does Hot Water Freeze Faster In A Home Freezer?
Yes, it can. But a home freezer is full of little traps. Frost on the shelf, a fan near one cup, a door opened too often, or two cups with slightly different shapes can tilt the race before it starts.
That’s why one person swears the hotter cup won and another gets the opposite result on the same night. They may both be right inside their own setup. This is less a law of nature and more a setup-sensitive effect.
What has to stay the same
If you want a fair test, almost everything but starting temperature should match. Once one detail drifts, the result gets muddy fast.
- Use the same water source for both samples.
- Match the starting volume by weight, not by eye.
- Use the same cup shape and material.
- Place both cups on the same shelf, side by side.
- Leave the freezer door shut.
- Pick one definition of “frozen” before you start.
Why Warm Water Can Win
Warm water starts behind, so it needs a real edge to catch up. The odd part is that a few edges can stack together.
Evaporation can shrink the job
Hot water gives off vapor faster than cold water. If some of the water leaves the cup, there is simply less liquid left to freeze. Less mass means less heat to remove and less ice to make. In some tests, that alone is enough to swing the result.
Convection can move heat out faster
Hot water often circulates more strongly inside the container. Warmer water rises, cooler water sinks, and that motion can spread heat toward the surface and walls at a quicker rate. A colder sample may sit more still, which can slow that heat transfer.
Surface contact can change the race
Set a warm cup on a frosty freezer surface and it may melt the frost under it. That can improve contact with the cold shelf. A colder cup may rest on frost the whole time, and frost acts like insulation. Same freezer, same shelf, two different paths for heat to escape.
Supercooling can trip up colder water
Water does not always freeze the instant it hits 32°F or 0°C. It can stay liquid below that point for a while, then snap into ice once crystals begin to form. Some colder samples supercool more deeply than warmer ones. When that happens, the colder cup can spend extra time “waiting” before freezing starts.
The original classroom story from Erasto Mpemba and Denis Osborne is still worth reading, and the 1969 paper by Mpemba and Osborne remains the starting point for most modern write-ups.
| Factor | What It Changes | Which Sample It Often Favors |
|---|---|---|
| Evaporation | Reduces the mass that still needs to freeze | Hotter water |
| Convection | Moves heat to the cup wall and surface faster | Hotter water |
| Frost melting under the cup | Improves contact with the cold shelf | Hotter water |
| Supercooling depth | Can delay the moment freezing starts | Either one, often colder water loses here |
| Dissolved gases | Boiling or heating can change nucleation behavior | Depends on the water and test |
| Container shape | Changes surface area and cooling pattern | Either one |
| Freezer airflow | Raises or lowers heat loss at the surface | Either one |
| What “frozen” means | Can change the finish line by many minutes | Either one |
Why The Debate Never Fully Settles
People are often talking past each other. One test calls it frozen when the first ice film appears. Another waits until the whole cup turns solid. One test uses tap water, another uses distilled water, and another starts with water that has been boiled and cooled. Those are not the same experiment.
That’s why the literature reads like a long argument with several winners. A careful Royal Society paper on observing the Mpemba effect makes this point well: bias in setup and in deciding when freezing starts can bend the result more than people expect.
What “freezing faster” can mean
- Ice appears on top sooner.
- The sample hits 0°C sooner.
- The sample begins crystal formation sooner.
- The whole sample turns solid sooner.
Those finish lines sound close, but they are not equal. One cup may form the first ice earlier, then lose the full-solid race. Another may cool more slowly at first, then freeze all at once after less supercooling. That’s why two honest tests can tell different stories.
How To Try It At Home Without Fooling Yourself
You don’t need lab gear, but you do need discipline. A sloppy kitchen test can still be fun, yet it won’t tell you much.
- Weigh two empty, matching containers.
- Add the same mass of water to each one.
- Heat one sample well above the other. Leave the second cool, but not icy.
- Put both containers on the same shelf with space between them.
- Do not open the freezer door during the run.
- Use a fixed endpoint, such as “solid all the way through.”
- Run the test more than once.
If you want a cleaner read, use a kitchen scale before and after freezing. That shows whether evaporation changed the mass enough to matter. A recent Royal Society of Chemistry investigation also shows why clear definitions and repeated trials matter so much when people try to pin this effect down.
| Home Setup | What You May See | Why |
|---|---|---|
| Open cups on a frosty shelf | Warm water wins more often | Evaporation and better shelf contact can stack up |
| Covered cups with equal mass | Cold water often wins | Less evaporation removes one of hot water’s edges |
| Tall narrow cups | Mixed results | Cooling pattern shifts with depth and surface area |
| Repeated trials with tap water | Variable results | Minerals, gases, and nucleation sites may differ each time |
| Strict “solid all the way through” endpoint | Hot water wins less often | Early ice is not the same as full freezing |
What The Answer Means
If you were hoping for a clean schoolbook rule, you won’t get one here. Hot water can freeze faster than cold water, but only in setups that let one or more of those advantages show up. Change the cup, the shelf, the airflow, the lid, or the endpoint, and the winner can change too.
So the honest answer is not “always yes” or “always no.” It’s “yes, under some conditions.” That is still a neat result, because it tells you that freezing is not only about starting temperature. It is also about mass loss, fluid motion, nucleation, and the way a sample trades heat with its container and the air around it.
References & Sources
- Royal Society of Chemistry.“Cool?.”Records the 1969 paper by Erasto Mpemba and Denis Osborne that brought the effect into modern physics teaching.
- The Royal Society.“Observing the Mpemba effect with minimal bias and the value of the biogeography-based optimization.”Shows why setup choices and the way freezing is measured can change the result.
- Royal Society of Chemistry.“An experimental investigation of the Mpemba effect.”Gives a recent experimental view of when the effect appears and why repeated trials matter.

