An air-source heat pump absorbs heat from outdoor air at its evaporator coil. Whenever the coil surface runs below 0 °C — which happens once ambient air drops below roughly +5 °C, because the evaporating refrigerant sits well under the air temperature — airborne moisture condenses and freezes onto the fins as frost.
Coefficient of performance (Carnot limit):
COP_carnot = T_hot / (T_hot − T_evap) [temperatures in kelvin]
Real system:
COP = η · COP_carnot η ≈ 0.45 (compressor + duct losses)
Frost penalty:
T_evap = T_out − ΔT_approach − k_frost · d_frost
(frost insulates the fins and blocks airflow, pulling T_evap down further)
Frost accumulates fastest not at the coldest temperatures but in a narrow band around 0–4 °C, because very cold air simply holds less moisture to deposit — this simulator's growth curve peaks near +2 °C and fades out below about −10 °C, matching real frosting data for air-source units.
Once frost thickness crosses the trigger threshold, the reversing valve flips the cycle: hot, high-pressure discharge gas is routed backward to the outdoor coil to melt the frost, while the indoor coil briefly stops delivering useful heat. This reverse-cycle defrost costs energy twice — the compressor keeps drawing power with no heat delivered, and (in real units) a booster or resistance element often runs to offset the cold blast indoors. The tracked "cumulative defrost energy penalty" is the running share of total compressor + auxiliary energy spent on defrost cycles rather than on space heating.
- Outdoor temperature / humidity — set the weather; together they drive how fast frost grows and how low the COP is even before frost forms.
- Defrost trigger — the frost thickness (mm) that forces a defrost; a lower threshold defrosts more often (cleaner coil, more energy lost to defrost cycles) while a higher one lets COP degrade further between defrosts.
- Force defrost now — starts a defrost immediately, useful for comparing thin-frost vs thick-frost defrost cost.