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Why Does My Heat Pump Freeze Up in Winter?

Updated 8 October 20267 min readGeothermal & Heat Pumps

A heat pump in heating mode has to make one surface colder than the outdoors, because heat only flows from warm to cold. If that surface sits below both freezing point and the dew point of the air around it, moisture condenses onto it and freezes. Frost is therefore normal and designed for. The useful question is never whether the machine frosts, but whether it clears.

Key takeaways

  • The outdoor coil has to run colder than the outdoor air, so frost forms whenever the air is damp and the coil is below freezing.
  • Frost is worst in mild, damp conditions near freezing point, not in the deepest cold — cold air holds very little moisture to give up.
  • A defrost cycle reverses the refrigerant flow and heats the outdoor coil from inside, which is why the unit steams and briefly stops heating the house.
  • Solid ice, ice building at the base of the unit, or defrost cycles running back to back are faults; a light frost that clears is not.
  • Ground-loop systems freeze for a different reason — a loop asked for more heat than the ground can supply drifts colder each winter.
On this page
  1. Frost is the design working, not failing
  2. How the machine removes it
  3. Telling normal frost from a fault
  4. What you can do, and where to stop
  5. The ground-loop version of the same problem

Frost is the design working, not failing

An air-source heat pump collects heat from outdoor air. To do that, its outdoor coil — the evaporator in heating mode — has to be colder than the air it is collecting from, typically by a noticeable margin, because heat needs a temperature difference to flow across.

Cross-section through an outdoor heat pump coil with air flowing across it. The air arrives at outdoor temperature carrying water vapour. The coil surface sits several degrees below the air temperature and below freezing. Where the air meets the cold surface it is cooled past its dew point, the vapour condenses, and because the surface is below freezing the condensate freezes onto the fins rather than draining. A note states that frosting is worst in damp air near freezing point, because cold dry air carries little moisture to give up.Cross-section through an outdoor heat pump coil with air flowing across it. The air arrives at outdoor temperature carrying water vapour. The coil surface sits several degrees below the air temperature and below freezing. Where the air meets the cold surface it is cooled past its dew point, the vapour condenses, and because the surface is below freezing the condensate freezes onto the fins rather than draining. A note states that frosting is worst in damp air near freezing point, because cold dry air carries little moisture to give up.
The coil must be colder than the air to collect from it. Below freezing, the moisture the air gives up arrives as frost, not water.

So two conditions have to be met at once, and in heating weather they usually are: the coil is below the air's dew point, so moisture condenses out of the air onto it, and the coil is below freezing, so that moisture arrives as ice instead of draining away as water.

This is why frost appears far more aggressively in mild, damp weather than in a deep freeze. Air a few degrees above freezing holds a great deal of water vapour; air well below freezing holds very little. The worst frosting conditions are a damp day near the freezing mark, not the coldest night of the year.

Frost matters because it insulates the coil and blocks the gaps between the fins, choking the airflow — the same way debris on a micro-hydro intake screen starves a turbine of water. Both effects cut the heat the machine can collect, so left alone, frost makes itself worse.

How the machine removes it

The trick a heat pump uses is elegant: it runs itself backwards for a few minutes.

Two states of the same refrigerant circuit. In heating, the reversing valve directs hot refrigerant indoors to the condenser and the outdoor coil acts as the cold evaporator. In defrost, the reversing valve switches, sending hot gas from the compressor directly to the outdoor coil, which becomes the hot side and melts its frost from the inside; the indoor coil becomes cold, the outdoor fan usually stops, and backup heat is often engaged to cover the gap in indoor heating.Two states of the same refrigerant circuit. In heating, the reversing valve directs hot refrigerant indoors to the condenser and the outdoor coil acts as the cold evaporator. In defrost, the reversing valve switches, sending hot gas from the compressor directly to the outdoor coil, which becomes the hot side and melts its frost from the inside; the indoor coil becomes cold, the outdoor fan usually stops, and backup heat is often engaged to cover the gap in indoor heating.
The reversing valve makes the outdoor coil the hot side for a few minutes. The heat that melts the frost comes out of the house, which is the real reason defrost has a price.

A reversing valve sends hot compressor discharge gas to the outdoor coil instead of indoors. The coil becomes the hot surface, melts the ice from within, and the meltwater drains away — producing the cloud of steam that makes people think something has caught fire. The outdoor fan normally stops so the heat stays in the coil, and because the indoor side is now the cold side, many systems bring in a backup heater to prevent the house cooling during the cycle.

What triggers it matters. Older systems ran defrost on a timer whether or not frost had formed, spending energy on cycles nobody needed. Modern systems use demand defrost: sensors watch coil temperature, air temperature and the pressure difference a blocked coil produces, and call a cycle when the evidence says there is ice.

Each cycle takes heat back out of the building. Defrosting occasionally is normal; defrosting constantly means a large fraction of the machine's output is going into un-heating the house, which is a symptom rather than a quirk. In an off-grid system that waste lands in the weeks with the least solar energy to spare.

Telling normal frost from a fault

Here is the distinction that matters most, because almost every genuine problem announces itself in the same few ways.

Two outdoor units compared. The normal one carries an even white frost across the coil face, clears completely during a defrost cycle, and rebuilds slowly afterwards. The faulty one is encased in clear solid ice, has ice built up in the base pan and around the fan, shows ice that never fully clears after a defrost cycle, and runs defrost cycles one after another. A third panel lists what each pattern points to.Two outdoor units compared. The normal one carries an even white frost across the coil face, clears completely during a defrost cycle, and rebuilds slowly afterwards. The faulty one is encased in clear solid ice, has ice built up in the base pan and around the fan, shows ice that never fully clears after a defrost cycle, and runs defrost cycles one after another. A third panel lists what each pattern points to.
Even white frost that clears is the machine working. Clear solid ice, ice in the base pan, or defrost cycles running back to back are not.
What the ice pattern is telling you
What you seeWhat it usually meansWhat it points at
Even white frost, clears at each defrostNormal operation in damp cold weatherNothing — watch and leave it
Ice that never fully clearsDefrost is being cut short or not calledSensor, control board or reversing valve
Ice building in the base of the unitMeltwater is not draining awayBlocked drain, no clearance beneath, ground level too high
Solid clear ice over the coil faceRepeated melt-and-refreeze cyclesDrainage, or defrost ending too early
Frost returning within minutesThe coil is running colder than it shouldRestricted airflow, or low refrigerant charge
Defrost cycles back to backThe machine cannot win against the frostAirflow, charge, or a coil that needs cleaning
Ice only on one part of the coilUneven refrigerant distribution or airflowCharge, distributor, or a blocked section

Symptom patterns, not a repair procedure. Anything involving refrigerant, sealed components or electrical work belongs to a qualified technician; the value of reading the pattern is knowing what to describe when you call one.

Two patterns deserve particular attention. Ice in the base pan means meltwater has nowhere to go: the drain is blocked, the unit sits too close to the ground, or debris has filled the space beneath it. Each defrost cycle then adds to the ice instead of removing it. And frost that rebuilds almost immediately says the coil is running colder than design, which points either at airflow — a dirty coil, a failing fan, snow drifted against the unit, leaves in the fins — or at a low refrigerant charge, which is a technician's job.

What you can do, and where to stop

The safe interventions are all about giving the machine the conditions it was designed for.

An outdoor unit with the clearances it needs marked. Space beneath the unit so meltwater can drain and so it stands above expected snow depth. Open space in front of the coil face so air is not recirculated. Clearance above the fan discharge. Obstructions shown as problems: vegetation grown against the fins, stacked items blocking airflow, snow drifted against the coil, and a downspout discharging water onto the unit where it can refreeze.An outdoor unit with the clearances it needs marked. Space beneath the unit so meltwater can drain and so it stands above expected snow depth. Open space in front of the coil face so air is not recirculated. Clearance above the fan discharge. Obstructions shown as problems: vegetation grown against the fins, stacked items blocking airflow, snow drifted against the coil, and a downspout discharging water onto the unit where it can refreeze.
Drainage below, air in front, nothing dripping from above. Most base-pan icing traces back to one of these three being wrong at installation and never revisited.

Clear snow and leaves from the coil and the fan, and keep vegetation back from the fins. Make sure water from a roof or gutter is not landing on the unit, where it freezes in place and defeats every defrost cycle. Check that the unit stands clear of the ground and that the space beneath it drains, and keep the coil clean — a fouled coil runs colder for the same job.

What not to do: never chip ice off, because the fins and the tubing behind them puncture easily and a refrigerant leak is a far larger problem than the ice was. Do not switch off the defrost function. Do not block the unit to "keep it warm". And do not keep resetting a system that is defrosting continuously — it is reporting something, and continuing to run it in that state achieves nothing.

The ground-loop version of the same problem

A ground-source machine has no outdoor coil in the air, so it cannot frost in this way at all. It can still freeze, on the other side — and the cause is entirely different.

Chart of ground loop fluid temperature across several winters. In a correctly sized loop, the temperature falls through each heating season and recovers over the summer, returning to a similar starting point each year. In an undersized loop, the temperature falls further each winter and does not fully recover, so each season starts colder than the last and the minimum approaches the freezing point of the antifreeze mixture, marked as the limit below which ice can form in the heat exchanger.Chart of ground loop fluid temperature across several winters. In a correctly sized loop, the temperature falls through each heating season and recovers over the summer, returning to a similar starting point each year. In an undersized loop, the temperature falls further each winter and does not fully recover, so each season starts colder than the last and the minimum approaches the freezing point of the antifreeze mixture, marked as the limit below which ice can form in the heat exchanger.
Illustrative. A loop asked for more heat than the ground replaces does not fail in one cold week — it drifts colder year on year until it meets the antifreeze limit.

A closed loop extracts heat from the ground, and the ground replaces it slowly by conduction from the surrounding mass and from seasonal recovery in summer. If the loop is short for the load, extraction outruns replacement, and the fluid returns colder each year — the drift described in how geothermal heat pumps work. Should the entering fluid approach the freezing point of the antifreeze mixture, ice can form inside the heat exchanger, which restricts flow and can damage it.

Low flow does the same thing locally: a partly blocked strainer, trapped air or a failing circulator means each litre of fluid gives up more heat than intended, so it leaves colder even though the loop as a whole is fine. Open-loop systems have their own version, where the well water itself is the constraint — one of the differences between closed and open loops that only shows up under sustained load.

The diagnostic thread is the same in both families. A machine that frosts, clears and carries on is working. A machine drifting steadily colder — an outdoor coil losing ground to the frost, or a loop losing ground to the season — is being asked for more than its heat source can supply, which is also what settles how the two behave in extreme cold.

Frequently asked questions

Is frost on the outdoor unit normal?

Yes, in heating weather. The coil is deliberately colder than the air around it, so any moisture in that air condenses on it and freezes. A uniform white frost that disappears during a defrost cycle and rebuilds slowly is the machine working as designed.

Why does my heat pump steam and blow cold air sometimes?

That is a defrost cycle. The unit reverses its refrigerant flow so the outdoor coil becomes the hot side and melts its own ice, which is what steams. The indoor side is not being heated meanwhile, so many systems run a backup heater to cover the few minutes it takes.

Should I pour hot water on the ice or chip it off?

Never chip it — the fins and the tubing behind them are thin, and a puncture releases the refrigerant charge. Lukewarm water can clear ice from the base in an emergency, but ice that keeps returning is a symptom, and why it formed matters more than removing it.

Why is it worse in mild weather than in a hard freeze?

Because air near freezing point holds far more water vapour than air well below it. Just above freezing, damp air passing over a sub-zero coil deposits a great deal of moisture; in a hard dry freeze there is little to deposit. Frosting is a humidity problem before it is a temperature problem.

Can a ground-source heat pump freeze up?

Not in the same way — it has no outdoor coil in the air. It can freeze on the loop side, when the ground is asked for more heat than it replaces: the fluid returns colder each season, and if it approaches the antifreeze mixture's freezing point, ice can form in the heat exchanger. That is a sizing or flow problem, not weather.

Sources

Named organisations whose published material underpins this article. Where no link is given, the source is named rather than linked.

  • U.S. Department of EnergyHeat pump operation, defrost behaviour and system maintenance guidance.
  • National Renewable Energy Laboratory (NREL)Heat pump performance research, including cold-climate operation.
  • Equipment manufacturer installation and service manualsDefrost strategy, sensor placement, clearances and fluid specifications are set per machine and govern over any general guidance.

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Research, drafting and review

Articles are drafted from primary engineering and physics references with AI-assisted tools, then reviewed and fact-checked line by line by a human editor before publication. We publish explanations, not recommendations: no products, no pricing, no country-specific rules, and no invented author personas.

Last reviewed 8 October 2026. How we research and review