Thermodynamics

Thermodynamics Formulas Cheat Sheet: 7 Key Equations

By Saurabh

Thermodynamics formulas cover a wide range of practical territory - sizing an AC unit, rating a heat engine, predicting condensation, and estimating a building's heating load are all governed by a small set of relationships. These seven cover cooling loads, engine efficiency, heat transfer, and weather comfort indices, the ones that show up constantly in HVAC and thermal-design work generally. Every one links to a calculator that runs the numbers with proper units, so you can check your own work against a real example.

BTU Cooling Load: Q = 25 BTU/hr per ft² (adjusted)

Oversizing an air conditioner past what this formula recommends doesn't just waste money - it actively makes a room feel worse. A too-large unit cools the air to the thermostat setpoint quickly, shuts off, and starts short-cycling, which means it never runs long enough in one stretch to pull much moisture out of the air.

The result is a room that reads the right temperature on a thermostat but still feels clammy, because dehumidification happens gradually as air keeps passing over a cold coil - a correctly sized unit that runs in longer, less frequent cycles actually removes more humidity than an oversized one chasing the same temperature.

Try the BTU Calculator.

Carnot Efficiency: η = 1 − Tc/Th

Because the cold reservoir Tc is usually bounded near ambient temperature or the temperature of available cooling water, there's only so much room to push it lower - a power plant can't meaningfully drop its condenser temperature far below the local river or air temperature it's rejecting heat into.

That's why real efficiency gains in heat-engine design come overwhelmingly from raising the hot reservoir Th instead - it's the main lever actually available, which is exactly why steam power plants keep pushing boiler temperatures and pressures higher, and why a jet or gas turbine engine's efficiency improves as materials advance enough to tolerate a hotter combustion temperature.

Try the Carnot Efficiency Calculator.

Convective Heat Transfer: Q̇ = h A ΔT

A fan blowing across a hot object cools it noticeably faster without changing the room's air temperature at all - what the fan actually changes is h, the convective heat transfer coefficient, which rises sharply once air is forced to move instead of drifting past by natural convection alone.

That's why h for forced convection in air is typically many times higher than for still air, and why a liquid like water forced across a surface transfers heat faster still - h isn't a fixed property of the fluid, it depends heavily on how fast that fluid is actually moving across the surface.

Try the Convective Heat Transfer Calculator.

Dew Point

A cold soda can sweating on a warm day is dew point made visible: condensation forms whenever a surface's own temperature drops below the surrounding air's dew point, regardless of what the air temperature itself happens to read.

That same mechanism is why an air conditioner has to run its evaporator coil colder than the room's dew point to pull moisture out of the air at all - any coil warmer than that just cools the air without condensing anything, which is the direct physical reason a short-cycling, oversized system can drop temperature while barely touching humidity.

Try the Dew Point Calculator.

Heat Conduction: Q̇ = k A ΔT / L

A metal doorknob and a wooden door in the same room are at the identical temperature, yet the metal feels distinctly colder to the touch - metal's thermal conductivity k is far higher than wood's, so it conducts heat away from a warm hand much faster, which is what skin actually senses as "cold," not a lower true temperature.

That same k is the reason cookware handles are made from wood, plastic, or hollow steel rather than solid metal, and why a heat sink is machined from aluminum or copper specifically for their high k - conductivity, not thickness or temperature alone, sets how quickly heat moves through a given material.

Try the Heat Conduction Calculator.

Heat Loss: Q = U × A × ΔT (+ infiltration)

A wall's U-value isn't a single material property the way k is for one layer - it's the combined effect of every layer in the assembly acting in series: siding, sheathing, insulation, drywall, and the thin air films on both surfaces, each contributing its own resistance to the total.

That's exactly why 1/U equals the sum of each layer's individual R-value: a whole-room heat loss estimate is really a stack of Heat Conduction-style calculations for every layer of the envelope, added together and then multiplied by the exposed area and the indoor-outdoor temperature difference all at once.

Try the Heat Loss Calculator.

Wind Chill: WC = 35.74 + 0.6215T − 35.75V^0.16 + 0.4275TV^0.16

Skin at rest keeps a thin layer of air warmed by body heat clinging close to its surface, acting like a built-in insulating blanket a fraction of an inch thick - that boundary layer is what actually slows heat loss on a calm, cold day more than the surrounding air temperature alone would suggest.

Wind's entire effect is stripping that boundary layer away faster than the body can rebuild it, forcing skin to continuously warm a fresh supply of cold air instead of coasting on one warmed layer - which is also why the formula needs a wind-speed floor: below about 3 mph there's too little airflow to meaningfully disrupt that layer in the first place.

Try the Wind Chill Calculator.

Quick Reference - All 7 Formulas

FormulaExpressionPrimary Use
BTU Cooling LoadQ = 25 BTU/hr·ft² (adjusted)Sizing a room air conditioner
Carnot Efficiencyη = 1 − Tc/ThMaximum theoretical heat-engine efficiency
Convective Heat TransferQ̇ = h A ΔTHeat transfer between a surface and a moving fluid
Dew PointAlduchov–Eskridge (Magnus) approximationTemperature at which air becomes saturated
Heat ConductionQ̇ = k A ΔT / LHeat transfer through a single material layer
Heat LossQ = U A ΔT + infiltrationWhole-room or building design heating load
Wind ChillWC = 35.74 + 0.6215T − 35.75V^0.16 + 0.4275TV^0.16Cold felt-temperature from air and wind

Part of the Thermodynamics calculators collection.

Frequently Asked Questions

Why isn't Heat Energy (Q = mcΔT) or the Ideal Gas Law on this list?

Both are covered in this site's companion piece, "15 Essential Engineering Formulas Every Student Should Know" - this list deliberately covers seven different Thermodynamics relationships instead of repeating those two.

What about Thermal Resistance (R-value) - where's that?

It has its own dedicated article, "How Thermal Resistance Determines a Wall's R-Value." It's closely related to the Heat Loss formula above: a wall's U-value used in Q = UAΔT is just 1/R, the inverse of the total thermal resistance across every layer of the assembly.

Convective Heat Transfer, Heat Conduction, and Heat Loss all look like some form of coefficient × Area × ΔT - what's actually different between them?

They're the same general heat-transfer-rate pattern applied at three different scales. Convective Heat Transfer uses h, a film coefficient describing one fluid moving past one surface. Heat Conduction uses k/L, the conductivity of one solid material divided by its thickness. Heat Loss uses U, which isn't one material's property at all - it's 1/U = ΣR, the combined resistance of every conductive and convective layer in a whole wall or building assembly added together, scaled up to a room- or building-level design calculation.

Can a real heat engine actually reach its Carnot efficiency?

No. Carnot efficiency is a theoretical upper bound assuming a perfectly reversible engine with no friction, no heat leaks, and infinitely slow (hence lossless) heat transfer. Every real engine has irreversibilities that fall short of that limit - Carnot efficiency tells you the ceiling a design is working toward, not a number any actual machine achieves.

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