Skip to main content

Heat Transfer Calculator

Our thermodynamics & heat calculator computes heat transfer accurately. Enter measurements for results with formulas and error analysis.

Skip to calculator
Physics

Heat Transfer Calculator

Calculate heat transfer rate (W) and thermal resistance for conduction, convection, and radiation. Enter temperature, area, and material properties.

Last updated: December 2025

Calculator

Adjust values & calculate
Understand the Math

Formula

Q = kAΔT/L (conduction) | Q = hAΔT (convection) | Q = εσA(T₁⁴-T₂⁴) (radiation)

Heat conduction rate depends on thermal conductivity, area, temperature difference, and thickness (Fourier's Law). Convection depends on the heat transfer coefficient. Radiation follows the Stefan-Boltzmann law with the fourth power of absolute temperature.

Last reviewed: December 2025

Worked Examples

Example 1: Wall Insulation Heat Loss

Calculate heat loss through a 150mm fiberglass-insulated wall (k = 0.04 W/m·K), area = 20m², with 20°C inside and -10°C outside.
Solution:
k = 0.04 W/(m·K), A = 20 m², ΔT = 30°C, L = 0.15m Q = kA(ΔT)/L = 0.04 × 20 × 30 / 0.15 = 160W Thermal Resistance = L/(kA) = 0.15/(0.04×20) = 0.1875 °C/W R-value = L/k = 0.15/0.04 = 3.75 m²·K/W Heat Flux = 160/20 = 8 W/m²
Result: Q = 160W | R_th = 0.1875 °C/W | R-value = 3.75

Example 2: Cooling Electronics with Forced Convection

A 50W processor has a heatsink with 0.02m² surface area. Air is forced over it with h = 150 W/(m²·K). What is the temperature rise?
Solution:
Q = hA(ΔT), so ΔT = Q/(hA) ΔT = 50 / (150 × 0.02) = 16.7°C If ambient = 25°C, heatsink temp = 41.7°C Thermal Resistance = 1/(hA) = 1/(150×0.02) = 0.333 °C/W
Result: ΔT = 16.7°C | T_surface = 41.7°C | R_th = 0.333 °C/W
Expert Insights

Background & Theory

The Heat Transfer Calculator applies the following established principles and formulas. Physics is the fundamental natural science concerned with matter, energy, and the interactions between them. Classical mechanics, founded on Newton's three laws of motion, provides the framework for analyzing the motion of objects. The first law states that an object remains at rest or in uniform motion unless acted upon by a net external force. The second law quantifies this relationship: F = ma, where force equals mass times acceleration in SI units of newtons (N = kg·m/s²). The third law establishes that every action produces an equal and opposite reaction. Kinematics describes motion without reference to its causes. The four fundamental equations relate displacement s, initial velocity u, final velocity v, acceleration a, and time t: v = u + at, s = ut + ½at², v² = u² + 2as, and s = ½(u + v)t. These assume constant acceleration and are foundational for solving projectile motion, free fall, and linear dynamics problems. Energy conservation underpins much of physics. Kinetic energy is KE = ½mv², where m is mass in kilograms and v is speed in meters per second. Gravitational potential energy is PE = mgh, where g ≈ 9.81 m/s² near Earth's surface and h is height in meters. The work-energy theorem states that the net work done on an object equals its change in kinetic energy: W = ΔKE. Electricity and circuits rely on Ohm's law: V = IR, where voltage V is in volts, current I in amperes, and resistance R in ohms. Electrical power is P = IV = I²R = V²/R, measured in watts. Wave mechanics connects frequency f, wave speed v, and wavelength λ through f = v/λ, with frequency in hertz (Hz). Pressure is defined as force per unit area, P = F/A, in pascals (Pa = N/m²). The ideal gas law PV = nRT links pressure, volume, moles n, the gas constant R = 8.314 J/(mol·K), and absolute temperature in kelvin. Gravitational force between two masses follows Newton's law of universal gravitation: F = Gm₁m₂/r², where G = 6.674×10⁻¹¹ N·m²/kg² is the gravitational constant.

History

The history behind the Heat Transfer Calculator traces back through the following developments. The history of physics spans over two millennia, beginning with the natural philosophy of ancient Greece. Aristotle (384–322 BCE) proposed that all matter consisted of four elements and that objects moved toward their natural place, with heavier objects falling faster than lighter ones. While largely incorrect, his systematic approach to explaining nature dominated Western thought for nearly 2,000 years. The Scientific Revolution overturned Aristotelian physics. Galileo Galilei (1564–1642) performed groundbreaking experiments on inclined planes and falling bodies, demonstrating that all objects fall with the same acceleration regardless of mass, and established the principle of inertia. His use of mathematics to describe motion was revolutionary. Isaac Newton synthesized these developments in his landmark Principia Mathematica (1687), laying out the three laws of motion and the law of universal gravitation. Newton's framework unified terrestrial and celestial mechanics, explaining planetary orbits with the same equations governing a falling apple. His calculus provided the mathematical language for expressing rates of change. The 19th century brought two major theoretical achievements. James Clerk Maxwell formulated his equations of electromagnetism between 1861 and 1862, unifying electricity, magnetism, and optics, and predicting the existence of electromagnetic waves traveling at the speed of light. Thermodynamics was developed by Carnot, Clausius, and Kelvin, establishing the laws governing heat, work, and entropy. The 20th century produced two revolutions that fundamentally altered the classical picture. Albert Einstein published the special theory of relativity in 1905, showing that space and time are not absolute but relative to the observer, and that mass and energy are equivalent via E = mc². His general theory of relativity in 1915 reinterpreted gravity as the curvature of spacetime. Simultaneously, quantum mechanics emerged from the work of Planck, Bohr, Heisenberg, and Schrödinger, revealing that at atomic scales energy is quantized and particles exhibit wave-particle duality. These developments culminated in the Standard Model of particle physics, which describes all known fundamental particles and three of the four fundamental forces.

Share this calculator

Explore More

Frequently Asked Questions

Heat transfers through three fundamental mechanisms: (1) Conduction — heat flows through a solid material or between materials in direct contact, driven by a temperature gradient. Rate depends on thermal conductivity, area, temperature difference, and material thickness. (2) Convection — heat transfer between a surface and a moving fluid (liquid or gas). Can be natural (driven by buoyancy) or forced (driven by fans/pumps). Rate depends on the convection coefficient, area, and temperature difference. (3) Radiation — heat transfer via electromagnetic waves (infrared). Does not require a medium and can occur through vacuum. Rate depends on emissivity, temperature, and area.
The convection heat transfer coefficient (h) quantifies how effectively heat transfers between a surface and a fluid. It depends on fluid properties, flow velocity, geometry, and whether convection is natural or forced. Typical values: Natural convection in air = 5-25 W/(m²·K). Forced convection in air = 25-250 W/(m²·K). Natural convection in water = 100-900 W/(m²·K). Forced convection in water = 250-12,000 W/(m²·K). Boiling water = 3,000-100,000 W/(m²·K). The coefficient is often determined empirically using dimensionless correlations involving Nusselt, Reynolds, and Prandtl numbers.
You may use the results for reference and educational purposes. For professional reports, academic papers, or critical decisions, we recommend verifying outputs against peer-reviewed sources or consulting a qualified expert in the relevant field.
All calculations use established mathematical formulas and are performed with high-precision arithmetic. Results are accurate to the precision shown. For critical decisions in finance, medicine, or engineering, always verify results with a qualified professional.
No. All calculations run entirely in your browser using JavaScript. No data you enter is ever transmitted to any server or stored anywhere. Your inputs remain completely private.
The Formula section on this page shows the equation used. You can reproduce the calculation manually or in a spreadsheet using those steps. Compare your answer against the worked examples in the Examples section, which use known reference values so you can confirm the calculator is behaving as expected.
Educational Note: This calculator is provided for educational and informational purposes. Results are based on the formulas and inputs provided. Always verify important calculations independently. NovaCalculator processes calculator inputs client-side; optional analytics follow visitor consent settings. © 2024–2026 NovaCalculator.

Share this calculator

Formula

Q = kAΔT/L (conduction) | Q = hAΔT (convection) | Q = εσA(T₁⁴-T₂⁴) (radiation)

Heat conduction rate depends on thermal conductivity, area, temperature difference, and thickness (Fourier's Law). Convection depends on the heat transfer coefficient. Radiation follows the Stefan-Boltzmann law with the fourth power of absolute temperature.

Worked Examples

Example 1: Wall Insulation Heat Loss

Problem: Calculate heat loss through a 150mm fiberglass-insulated wall (k = 0.04 W/m·K), area = 20m², with 20°C inside and -10°C outside.

Solution: k = 0.04 W/(m·K), A = 20 m², ΔT = 30°C, L = 0.15m\nQ = kA(ΔT)/L = 0.04 × 20 × 30 / 0.15 = 160W\nThermal Resistance = L/(kA) = 0.15/(0.04×20) = 0.1875 °C/W\nR-value = L/k = 0.15/0.04 = 3.75 m²·K/W\nHeat Flux = 160/20 = 8 W/m²

Result: Q = 160W | R_th = 0.1875 °C/W | R-value = 3.75

Example 2: Cooling Electronics with Forced Convection

Problem: A 50W processor has a heatsink with 0.02m² surface area. Air is forced over it with h = 150 W/(m²·K). What is the temperature rise?

Solution: Q = hA(ΔT), so ΔT = Q/(hA)\nΔT = 50 / (150 × 0.02) = 16.7°C\nIf ambient = 25°C, heatsink temp = 41.7°C\nThermal Resistance = 1/(hA) = 1/(150×0.02) = 0.333 °C/W

Result: ΔT = 16.7°C | T_surface = 41.7°C | R_th = 0.333 °C/W

Frequently Asked Questions

What are the three modes of heat transfer?

Heat transfers through three fundamental mechanisms: (1) Conduction — heat flows through a solid material or between materials in direct contact, driven by a temperature gradient. Rate depends on thermal conductivity, area, temperature difference, and material thickness. (2) Convection — heat transfer between a surface and a moving fluid (liquid or gas). Can be natural (driven by buoyancy) or forced (driven by fans/pumps). Rate depends on the convection coefficient, area, and temperature difference. (3) Radiation — heat transfer via electromagnetic waves (infrared). Does not require a medium and can occur through vacuum. Rate depends on emissivity, temperature, and area.

What is the convection heat transfer coefficient?

The convection heat transfer coefficient (h) quantifies how effectively heat transfers between a surface and a fluid. It depends on fluid properties, flow velocity, geometry, and whether convection is natural or forced. Typical values: Natural convection in air = 5-25 W/(m²·K). Forced convection in air = 25-250 W/(m²·K). Natural convection in water = 100-900 W/(m²·K). Forced convection in water = 250-12,000 W/(m²·K). Boiling water = 3,000-100,000 W/(m²·K). The coefficient is often determined empirically using dimensionless correlations involving Nusselt, Reynolds, and Prandtl numbers.

Why might my result differ from another tool or reference?

Differences typically arise from rounding conventions, the specific version of a formula (for example, simple vs compound interest), or unit inconsistencies between inputs. Check that both tools are using the same formula variant and the same units. The References section links to the authoritative source behind the formula used here.

What inputs do I need to use Heat Transfer Calculator accurately?

Each field is labelled with the required unit (metric or imperial). Gather your source values before starting — for example, a weight measurement in kilograms, a distance in metres, or a dollar amount — and enter them exactly as measured. The formula section on this page lists every variable and explains what each represents.

How do I get the most accurate result?

Enter values as precisely as possible using the correct units for each field. Check that you have selected the right unit (e.g. kilograms vs pounds, meters vs feet) before calculating. Rounding inputs early can reduce output precision.

Can I use the results for professional or academic purposes?

You may use the results for reference and educational purposes. For professional reports, academic papers, or critical decisions, we recommend verifying outputs against peer-reviewed sources or consulting a qualified expert in the relevant field.

References

Reviewed by Manoj Kumar, Mathematics Educator · Editorial policy