Heat Transfer Explorer
Explore the three main modes of heat transfer and see how changing temperature, area, material properties and surface conditions changes the heat-transfer rate.
Open toolCalculators and interactive tools
The tools cover thermal physics, buildings, electronics, human thermal environments, cooking and heat perception. Calculations run locally in your browser and expose the method and assumptions where a numerical model is used.
Explore the three main modes of heat transfer and see how changing temperature, area, material properties and surface conditions changes the heat-transfer rate.
Open toolCalculate how much sensible thermal energy is required to raise or lower the temperature of a material without a phase change.
Open toolBreak a heating process into sensible-heating and phase-change energy steps.
Open toolEstimate steady conductive heat flow through a uniform flat layer and see the effect of material conductivity and thickness.
Open toolEstimate how an object approaches ambient temperature when internal temperature gradients are small enough for a lumped model.
Open toolEstimate net long-wave radiative heat transfer between a surface and large isothermal surroundings.
Open toolEstimate the temperature leaving an idealised direct evaporative cooler from entering dry-bulb conditions and cooler effectiveness.
Open toolBuild a simple hot-fluid-to-cold-fluid thermal path and see the heat rate and temperature drop across each resistance.
Open toolExplore how thickness, diffusivity and time control the temperature response inside a slab when its surfaces are suddenly held at a new temperature.
Open toolModel a wall made from several material layers and see how each layer contributes to total thermal resistance.
Open toolConvert R-values and U-factors between SI and imperial unit systems.
Open toolEstimate dew-point temperature and identify whether an entered surface temperature is at or below that dew point.
Open toolEstimate heat loss through a cylindrical insulation layer around a pipe.
Open toolEstimate solar heat gain through glazing and see the effect of area, solar irradiance and SHGC.
Open toolSee how a small area of more conductive material can increase whole-assembly heat transfer.
Open toolConnect wall heat transfer with indoor humidity by estimating the interior surface temperature and its margin above or below dew point.
Open toolCombine envelope transmission and a simple air-exchange load into one room heating estimate instead of treating them as separate calculations.
Open toolCompare three common heating methods on one delivered-heat basis instead of relying on separate pairwise comparisons.
Open toolEstimate how much a solid changes length when its temperature changes.
Open toolSee how conductivity, density and heat capacity combine to determine how rapidly temperature disturbances spread through a material.
Open toolChoose a thermal goal and see which reference materials rank highly for that property, with condition notes kept visible.
Open toolEstimate junction temperature and temperature rise for an electronic component using a simple thermal-resistance model.
Open toolCalculate the maximum heat-sink-to-ambient thermal resistance that keeps an idealised component thermal path below a chosen junction-temperature limit.
Open toolBuild a simple series thermal path and inspect temperature drops across each thermal resistance.
Open toolSee how interface thickness, conductivity and contact area affect the temperature drop between a component and heat sink.
Open toolSee which thermal-design change produces the largest junction-temperature reduction in a simple series resistance model.
Open toolConvert temperature, energy and heat-rate units in one place.
Open toolApply a steady-flow energy balance to a two-stream sensible heat exchanger.
Open toolCompare parallel and counterflow temperature driving forces and connect heat duty with area and overall heat-transfer coefficient.
Open toolEstimate group-average thermal sensation using air temperature, mean radiant temperature, air speed, humidity, clothing insulation and metabolic rate.
Open toolConnect dry-bulb temperature and relative humidity with dew point, approximate wet-bulb temperature and moisture content in one air-state calculation.
Open toolCombine measured natural wet-bulb, globe and dry-bulb temperatures using standard WBGT weighting formulas.
Open toolConnect energy dissipation with temperature rise while keeping the conversion fraction and thermal storage assumptions explicit.
Open toolCompare representative chilli pungency ranges and see where an entered Scoville Heat Unit value sits on a descriptive scale.
Open toolEstimate why water boils below 100 °C at higher elevations as atmospheric pressure falls.
Open toolChoose a cooking method and see which heat-transfer mechanisms dominate, which are secondary and what changes the heating rate.
Open toolSee how mechanical compression can raise gas temperature even when the idealised process adds no heat from outside.
Open toolCompare thermal effusivity and estimate the ideal initial interface temperature when two materials at different temperatures touch.
Open toolConnect friction force and sliding speed to heat generation, then estimate an idealised temperature rise from energy, mass and specific heat.
Open toolConvert a change in vehicle speed into braking energy, then estimate how much an entered brake mass could heat in an idealised model.
Open toolCalculate electrical power dissipated as heat in a resistive element and see how current, resistance, voltage and time affect energy.
Open toolUse q = mcΔT to estimate solution heat and the opposite-sign reaction heat, with an optional molar heat result.
Open toolSubtract external mechanical work from metabolic power to estimate internal heat production, then calculate the corresponding thermal energy over time.
Open toolEstimate temperature with depth from a user-selected geothermal gradient and compare the result with the limits of a simple linear model.
Open toolCalculate the wavelength at which an ideal blackbody spectrum peaks and see how hotter objects shift toward shorter wavelengths.
Open toolBalance globally averaged absorbed stellar radiation against thermal emission to estimate an idealised effective temperature.
Open toolCalculate National Weather Service heat index and understand why humidity, sun, workload, clothing and acclimatisation make heat stress more complex than one apparent-temperature number.
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