Learn how to design heat pump systems that balance efficiency, reliability, and long‑term operating cost.
By Sahil Mahajan, PE, P.Eng., CPD, LEED Green Associate

Air Cooled vs. Water Cooled
Air‑cooled heat pumps reject heat directly to the outdoor environment, which means their performance is tied to fluctuating ambient conditions. As outdoor temperatures rise, condensing pressures increase, reducing efficiency and raising compressor lift. Water‑cooled heat pumps, by contrast, reject heat to a stable water loop maintained by a cooling tower, dry cooler, or geothermal field. Because water has higher thermal conductivity and a narrower temperature range, these systems operate at lower condensing temperatures and achieve higher COP and EER values. This thermodynamic advantage explains why water‑cooled systems are often favored in large commercial buildings and high‑rise structures where mechanical room space is available and long‑term operating cost is a priority.
The installation environment further differentiates the two systems. Air‑cooled units require outdoor placement with adequate airflow clearance, making them simple to install but more exposed to weather, debris, and acoustic concerns. Water‑cooled systems require pumps, piping, and a cooling tower, resulting in higher first cost but greater placement flexibility and quieter operation. Their indoor location also contributes to longer service life, while air‑cooled units typically experience more wear due to environmental exposure.
Capacity Derating
A critical performance factor for air‑source heat pumps is capacity derating at low ambient temperatures. As outdoor air becomes colder, the amount of usable heat available decreases, forcing the heat pump to operate with a higher temperature lift between the outdoor coil and the indoor conditioned space. This reduces both heating capacity and efficiency. Frost accumulation on the outdoor coil triggers periodic defrost cycles, during which the system temporarily reverses operation, further reducing net heating output. Standard air‑source heat pumps may lose 10 to 20 percent of capacity at 35°F, 30 to 50 percent at 17°F, and more than half of their output as temperatures approach 0°F. Below 10°F, the derating curve bends sharply downward as the system approaches the minimum allowable suction pressure and compressor operating limits.
The following numerical example illustrates this behavior: A nominal 3-ton (36,000-Btuh) heat pump rated at 47°F may deliver 31,000 Btuh at 35°F, 27,000 Btuh at 25°F, 22,000 Btuh at 17°F, and only 17,000 Btuh at 5°F. This corresponds to 100 percent, 86 percent, 75 percent, 61 percent, and 47 percent of nominal capacity, respectively. A cold‑climate inverter version of the same unit performs better, delivering 35,000 Btuh at 35°F, 34,000 Btuh at 25°F, 33,000 Btuh at 17°F, and 30,000 Btuh at 5°F, which corresponds to 100 percent, 97 percent, 94 percent, 92 percent, and 83 percent of the heat pump capacity—still derating, but far more gradually.
The following charts compare 3-ton (36,000 Btuh) nominal and cold-climate inverter air source heat pumps rated at 47ºF.
This derating behavior directly affects the building’s balance point, the temperature at which heat pump output equals the building’s heat loss. Consider a building with a heat loss of 10,000 Btuh at 60°F and 30,000 Btuh at 10°F. The slope of heat‑loss line would be:
Slope = (30,000 – 10,000)/(10 – 60) = 20,000/-50 = -400 Btuh per °F
So, the building load (Qload) at the outdoor temperature (Tout) is:
Qload = 10,000 + 400 · (60 – Tout)
Using heat pump derated capacity points from the standard 3-ton (36,000-Btuh) heat pump unit used in the previous example:
- 47°F → 36,000 Btuh
- 35°F → 31,000 Btuh
- 25°F → 27,000 Btuh
- 17°F → 22,000 Btuh
The building load (Qload) and heat pump capacity comparison at each temperature will be:
At 47°F:
Qload = 10,000 + 400 · (60 – 47) = 10,000 + 400 · 13 = 15,200 Btuh
Heat pump capacity = 36,000 Btuh (excess capacity)
At 35°F:
Qload = 10,000 + 400 · (60 – 35) = 10,000 + 400 · 25 = 20,000 Btuh
Heat pump capacity = 31,000 Btuh (excess capacity)
At 25°F:
Qload = 10,000 + 400 · (60 – 25) = 10,000 + 400 · 35 = 24,000 Btuh
Heat pump capacity = 27,000 Btuh (slight excess)
At 17°F:
Qload = 10,000 + 400 · (60 – 17) = 10,000 + 400 · 43 = 27,200 Btuh
Heat pump capacity = 22,000 Btuh (shortfall)
So, the balance point (Tbal) lies between 25°F and 17°F. To interpolate the balance point between 25°F and 17°F:
- Load: 24,000 → 27,200 Btuh (increase of 3,200)
- Capacity: 27,000 → 22,000 Btuh (decrease of 5,000)
We want Tbal where Qload(Tbal) = Qcap(Tbal). Approximated linearly:
Load at T:
Qload(T) = 24,000 + 400(25 – T)
Capacity at T:
Qcap(T) ≈ 27,000 – (5,000/25 – 17)(25 – T) = 27,000 – 625 · (25 – T)
Set equal:
24,000 + 400(25 – T) = 27,000 – 625(25 – T)
24,000 + 10,000 – 400T = 27,000 – 15,625 + 625T
34,000 – 400T = 11,375 + 625T
34,000 – 11,375 = 1,025T
22,625 = 1,025T
T = 22.1°F
So, the balance point is around 22°F. Below this, auxiliary heat is required.
Improving System Efficiency
Cold‑climate engineering requires careful consideration of envelope performance, emitter selection, and system configuration. A tighter building envelope reduces the slope of the heat‑loss curve, lowering the balance point and reducing reliance on auxiliary heat. Low‑temperature emitters such as radiant floors or oversized fan coils allow the heat pump to operate at lower supply temperatures, improving efficiency and reducing compressor lift. Reverse‑cycle defrost temporarily interrupts heating, and the frequency of these cycles increases as humidity rises and temperature falls. Demand‑based defrost strategies minimize unnecessary cycles and improve seasonal performance, which is especially important in humid continental climates.
System selection in cold climates depends heavily on design temperature. In regions with design temperatures above 20°F, standard air‑source heat pumps are often sufficient. In climates with design temperatures between 0°F and 20°F, cold‑climate inverter heat pumps are preferred, with auxiliary heat expected during the coldest hours. In regions where design temperatures fall below 0°F, water‑source or geothermal systems become increasingly attractive because they avoid low‑ambient derating entirely. Hybrid systems that combine a heat pump with a boiler or furnace can also optimize performance by allowing the heat pump to operate in its efficient range while the auxiliary system handles extreme conditions.
Ultimately, the derating curve is not merely a performance characteristic. It is a design tool that shapes equipment selection, auxiliary heat sizing, and overall system architecture. Air‑cooled systems offer simplicity and lower first cost, making them suitable for residential and light commercial applications. Water‑cooled systems deliver superior efficiency, quieter operation, and longer lifespan, aligning with the needs of large commercial buildings and district energy systems. In cold climates, the impact of low‑ambient derating often becomes the deciding factor, pushing designers toward water‑source or geothermal solutions that maintain stable capacity regardless of outdoor temperature. Understanding these relationships allows engineers to design systems that balance efficiency, reliability, and long‑term operating cost.
References
- ASHRAE Handbooks
- AHRI Standard 210/240: Performance Rating of Unitary Air‑Conditioning & Air‑Source Heat Pump Equipment
About the Author

The opinions expressed in this article are those of the authors and not the American Society of Plumbing Engineers.

