Laundry Drying Time Estimator
Introduction: what really sets laundry air-drying time
Washing that comes out of the machine is carrying water, and air drying is simply the business of persuading that water to leave as vapour. This estimator does that calculation the way a psychrometric textbook does it, rather than with a made-up fudge factor: it works out how much water the spin cycle left behind, how much vapour the surrounding air can still absorb, and how fast moving air can carry vapour away from the fabric surface.
Four physical levers control the answer, and they are not equally powerful:
- Spin speed sets the starting water. Residual moisture content after spinning falls steeply with drum speed because the centrifugal field grows with the square of the rotation rate. The old EU energy label graded washing machines into spin-drying efficiency classes A to G on exactly this number, and moving from a 600 rpm machine to a 1400 rpm machine cuts the water a load starts with by roughly a third. This is the single biggest lever available, and it is paid for in seconds of motor time rather than hours of weather.
- The vapour-pressure deficit sets the driving force. Evaporation is proportional to the difference in water-vapour density between the saturated fabric surface and the ambient air. Warm air can hold far more vapour than cold air, so the deficit widens with temperature and narrows as relative humidity rises, reaching zero when the air is saturated.
- Airflow sets how fast vapour is carried off. Wind or a fan raises the convective mass-transfer coefficient, thinning the saturated boundary layer that otherwise sits against the cloth. A 1 m/s breeze roughly doubles the rate compared with still indoor air.
- Sunshine heats the cloth above the wet-bulb temperature. Absorbed solar radiation raises the fabric surface temperature, which raises the saturation vapour pressure at the surface and therefore widens the deficit. In shade, evaporative cooling pins wet laundry close to the wet-bulb temperature of the air, which is usually several degrees colder than the air itself.
The calculator combines those four into a surface energy balance, solves it for the fabric temperature, and converts the resulting evaporation rate into hours. It then splits the drying into the two stages that real textile drying shows: a constant-rate stage while the cloth surface is still wet everywhere, and a slower falling-rate stage once the remaining water is bound inside fibres, hems and waistbands.
How to use this laundry drying time estimator
Work down the form in order. Every field has a physical meaning, and the two water-content routes give the same answer when your scale and your machine agree.
- Dry laundry mass. Enter the mass of the same garments when fully dry, in kilograms. If you have never weighed them, weigh the load once when it comes off the line and reuse that figure. A typical adult mixed wash is 4 kg to 6 kg dry.
- Fabric mix. Choose the group that dominates the load. This sets three things at once: how much water the fabric holds after spinning, how much surface area a kilogram of it exposes to the air, and how deeply water hides inside the fibre once the surface is dry.
- Water content from. Pick Measured wet and dry weights if you weighed the load straight out of the drum, or Estimated from final spin speed if you only know the machine setting. The unused field is ignored, so you never have to invent a number.
- Wet weight or spin speed. Wet weight is taken immediately after the spin, before anything drips away. Spin speed is the final spin in revolutions per minute, typically 400 rpm to 1600 rpm on a domestic front loader.
- Air temperature, relative humidity and air speed. Use the conditions where the laundry actually hangs, not the forecast for the region. Indoor air speed with the door shut is about 0.1 m/s to 0.2 m/s; a fan pointed across a rack gives 1 m/s to 2 m/s; a breezy garden line sees 2 m/s to 4 m/s.
- Sun exposure. Shade covers indoor racks and north-facing lines. Bright overcast is roughly 350 W/m² on the cloth; clear summer midday sun is roughly 800 W/m².
- Press Estimate drying time. The result panel gives the total hours, the split between the constant-rate and falling-rate stages, the peak evaporation rate, the fabric surface temperature, the ambient dew point, and the tumble-dryer energy the load avoids. The chart underneath sweeps relative humidity so you can see how close you are to the cliff, and the table shows the same sweep in numbers.
Change one input at a time and re-run to see which lever matters most for your situation. On a mild, humid day the spin speed usually wins; on a cold, damp day nothing outdoors wins and the honest answer is a rack indoors with a fan.
Drying-time formula: psychrometrics, spin speed and mass transfer
The calculation runs in five steps. Every constant below is used by the JavaScript on this page, so the numbers in the worked example can be reproduced by hand.
Step 1 — water left after the spin
If you measured the load, the water mass is simply the difference between wet and dry weights:
Formula: W = m_wet − m_dry, X_0 = W / m_dry
Here X0 is the initial moisture ratio, the mass of water carried per kilogram of bone-dry cloth. It is the same quantity the EU spin-drying efficiency classes are defined on: class A is below 45 %, class C spans 54 % to 63 %, and class G is 90 % or more.
If you only know the spin speed, the estimator predicts the residual moisture content from the centrifugal field G generated in the drum. With drum radius r = 0.24 m and rotation rate N in rpm:
Formula: G = (((2πN)/60)^2 r) / g, X_0 = k_f ⋅ 2.836 ⋅ G^−0.277
The exponent and coefficient are fitted so that the curve passes through the well-documented anchors of about 80 % residual moisture at 600 rpm and about 50 % at 1400 rpm for cotton, which places 1000 rpm at 60 % and 1600 rpm at 46 %. The fabric factor kf is 1.00 for a mixed cotton wash, 1.22 for terry towelling, 1.10 for denim, and 0.45 for synthetic base layers, which shed water far more readily.
Step 2 — how much vapour the air can still take
Saturation vapour pressure follows the Magnus form recommended by Alduchov and Eskridge and used throughout applied psychrometrics, with T in degrees Celsius and the result in pascals:
Formula: p_sat(T) = 610.94 ⋅ e^(17.625T)/(T+243.04)
Vapour density comes from the ideal gas law with the molar mass of water M = 0.018015 kg/mol and the universal gas constant R = 8.314 J/(mol·K):
Formula: ρ_v = (p ⋅ M) / (R ⋅(T + 273.15))
The ambient vapour density is ρa = RH · ρv(psat(Tair)). The dew point reported in the result is the temperature at which that same vapour density would saturate.
Step 3 — the fabric surface temperature
Wet cloth is not at air temperature. Evaporation removes latent heat, so the surface settles where absorbed sunlight balances the sensible heat gained from the air plus the latent heat carried away. Using the Chilton–Colburn analogy to link the heat-transfer coefficient to the mass-transfer coefficient (ρcpLe2/3 ≈ 1086 J/(m³·K) for air and water vapour), the balance solved by bisection on this page is:
Formula: (α ⋅ I ⋅ f) / h_m = 1086 ⋅(T_s − T_air) + h_fg ⋅(ρ_s(T_s) − ρ_a)
with solar absorptance α = 0.55 for mixed-colour laundry, irradiance I from the sun-exposure choice, a projection factor f that converts the load's 0.25 m² of sun-facing area per kilogram into a share of its total exposed area, and the latent heat of vaporisation hfg = 2.454 MJ/kg at 20 °C. Set I to zero and this equation returns the wet-bulb temperature: in shade at 20 °C and 60 % relative humidity, wet laundry sits near 14.8 °C.
Step 4 — the evaporation rate
Mass transfer from the wetted surface uses the standard convective form, with the exposed area A taken as the dry mass multiplied by a fabric-specific specific area (2.2 m²/kg for a mixed cotton wash, 1.5 for towelling, 1.2 for denim, 3.0 for thin synthetics):
Formula: m ˙ = h_m ⋅ A ⋅(ρ_s − ρ_a), h_m = 0.0025 + 0.0056 ⋅ v^0.8
The 0.0025 m/s floor is natural convection, so still air never gives a zero rate, and the 0.8 exponent on air speed v is the turbulent flat-plate dependence that the heat- and mass-transfer analogy predicts for flow along a hanging sheet.
Step 5 — hours, in two stages
While the whole surface is still wet the rate is constant, so the first stage takes the water above the critical moisture ratio Xc and divides it by the rate. Below Xc the wet patches shrink and the rate falls in proportion to the remaining free water, which gives the classical logarithmic falling-rate term down to a target ratio Xt:
Formula: t = (m_dry(X_0 − X_c)) / (m ˙) + (m_dry(X_c − X_e)) / (m ˙) ⋅ ln (X_c − X_e) / (X_t − X_e)
The equilibrium moisture ratio Xe is the regain the fabric settles at in that air, from the Henderson sorption isotherm fitted to published cotton regain data: 7.5 % at 65 % relative humidity, 10.5 % at 80 %, and 17 % at 95 %. The load is called dry when it reaches Xt = Xe + 0.03, which is the point at which cotton feels dry to the hand. Because Xe climbs steeply near saturation, the model correctly refuses to dry anything in air that is already at 100 % relative humidity.
Worked example: 5 kg cotton wash on a shaded, breezy line
These are the values the form loads with, so you can press Estimate drying time and compare every figure directly.
- Dry laundry mass: 5.0 kg
- Fabric mix: mixed cotton wash
- Water content from: measured wet and dry weights
- Wet weight after spin: 8.0 kg
- Air temperature: 20 °C
- Relative humidity: 60 %
- Air speed over the clothes: 1.0 m/s
- Sun exposure: shade or indoors
The load holds 8.0 − 5.0 = 3.0 kg of water, an initial moisture ratio of 60 %, which is EU spin-drying efficiency class C. Exposed area is 5.0 kg × 2.2 m²/kg = 11.0 m². Air speed gives a mass-transfer coefficient of 0.0025 + 0.0056 × 1.00.8 = 0.0081 m/s.
Formula: m ˙ = 0.0081 ⋅ 11.0 ⋅(0.012648 − 0.010349) = 2.048 × 10^−4 kg/s
Saturation at 20 °C is 2333 Pa by the Magnus form above, so the air at 60 % holds a vapour density of 0.010349 kg/m³. Solving the surface balance with no sun puts the cloth at 14.8 °C, where saturated vapour density is 0.012648 kg/m³. The deficit is therefore 0.0023 kg/m³ and the rate works out at 2.048 × 10⁻⁴ kg/s, which is 737 grams of water per hour.
The constant-rate stage runs from 60 % down to the critical ratio of 15 %, removing 5.0 × 0.45 = 2.25 kg and taking 3.05 hours. The falling-rate stage runs from 15 % down to the target of 9.8 %, with an equilibrium regain of 6.8 % in this air, and adds 0.56 hours. The calculator therefore reports 3.6 hours, or 3 h 36 min, together with a note that a tumble dryer would have spent about 2.9 kWh (vented or condenser) or 1.7 kWh (heat pump) removing the same 3.0 kg of water.
Now change one thing at a time. Selecting direct summer sun lifts the cloth to 16.8 °C and drops the estimate to 2.1 hours. Leaving it in shade but raising humidity to 80 % pushes it to 6.6 hours, and 90 % takes it to 12.5 hours. Switching the water source to a 1400 rpm spin instead of the measured weights starts the load at 2.50 kg of water rather than 3.00 kg and finishes in 2.9 hours — the same saving as an hour of sunshine, bought for a few watt-hours in the drum.
Reading the result and comparing typical drying situations
The headline number is the time to reach a hand-dry state, not the time until the last seam in the heaviest garment has given up its moisture. Treat it as a central estimate with roughly ±25 % of spread from garment spacing, thickness and the weather changing while the load hangs.
The rows below are produced by the same model, so you can enter any of them and reproduce the time exactly. They are useful as calibration points for judging your own conditions.
| Situation | Load | Air conditions | Estimated time |
|---|---|---|---|
| Indoor rack, door shut | 4 kg cotton, 2.18 kg water (1200 rpm) | 21 °C, 55 % RH, 0.15 m/s, shade | 6.2 h |
| Same rack with a fan across it | 4 kg cotton, 2.18 kg water (1200 rpm) | 21 °C, 55 % RH, 1.2 m/s, shade | 2.6 h |
| Sunny, breezy summer line | 5 kg cotton, 3.0 kg water | 24 °C, 45 % RH, 2.0 m/s, direct sun | 1.3 h |
| Mild shaded line | 5 kg cotton, 3.0 kg water | 20 °C, 60 % RH, 1.0 m/s, shade | 3.6 h |
| Cool, damp autumn day outdoors | 5 kg cotton, 3.0 kg water | 12 °C, 85 % RH, 0.8 m/s, shade | 12.0 h |
| Bath towels in full sun | 3 kg towelling, 3.66 kg water | 22 °C, 50 % RH, 2.0 m/s, direct sun | 4.1 h |
| Jeans on a shaded line | 2 kg denim, 1.2 kg water | 20 °C, 60 % RH, 1.0 m/s, shade | 7.0 h |
| Synthetic running kit indoors | 1 kg synthetic, 0.245 kg water | 21 °C, 55 % RH, 0.15 m/s, shade | 2.0 h |
Two patterns are worth noticing. Airflow is nearly free and very effective indoors, where a fan across a rack cuts the time by more than half. And thick, absorbent fabrics are slow not because they dry differently but because they start with far more water per kilogram and expose far less area per kilogram: towelling holds 22 % more water than a mixed cotton wash at the same spin speed and presents only two thirds of the surface.
Limitations and assumptions behind this drying model
This is an engineering estimate built from textbook relations, not a computational fluid dynamics simulation of your garden. The following assumptions matter enough to state plainly.
- One lumped load, not individual garments. The whole wash is treated as a single wetted surface at one temperature. In reality thin shirts finish hours before the waistband of a pair of jeans, and the estimate tracks the average.
- Effective area is a fabric-specific constant per kilogram. Garments crowded on a rack, folded double over a line, or hung inside each other expose far less than the assumed area, and the true time can be 50 % longer.
- Conditions are held steady. The entered temperature, humidity, air speed and irradiance apply for the whole drying period. Evening humidity rises sharply outdoors, so an estimate that runs past dusk is optimistic.
- Solar input is a flat-plate approximation. Absorptance is fixed at 0.55 and the sun-facing area at 0.25 m² per kilogram of dry laundry. Dark fabrics absorb more, white sheets much less, and no allowance is made for the sun moving behind a wall.
- The spin correlation assumes a 0.24 m drum radius. Compact and top-loading machines differ, and real residual moisture also depends on load size and how well the drum balances. Measuring the wet weight once is always more accurate than the spin-speed route.
- The sorption isotherm is fitted to cotton. The Henderson fit matches published regain well above 60 % relative humidity and understates it by one or two percentage points below 40 %, where the effect on total time is small.
- Below freezing is flagged, not modelled. The equations still run, but frozen laundry sublimates rather than evaporates and passes through a stiff stage the model does not represent.
- Saturated air is capped. At relative humidity above 99.5 % the driving deficit is effectively zero. Rather than printing an infinite or absurd number, the calculator caps the answer at 120 hours and says the air cannot accept more moisture.
- Tumble-dryer figures are test-standard averages. The 0.98 kWh and 0.55 kWh per kilogram of water are derived from certified test loads, not from your specific appliance, cycle or ambient temperature.
For anything time-critical, add a margin. Spreading the load out, opening a window and pointing a fan across the rack are the three actions that map directly onto the terms this model actually uses.
Sources checked for this laundry drying calculator
Sources: the psychrometric relations, mass-transfer analogy, spin-efficiency classes and dryer energy figures used above were checked against the following authorities.
- ASHRAE Handbook — Fundamentals, chapters on psychrometrics and on mass transfer, for saturation vapour pressure, vapour density, wet-bulb behaviour and the Chilton–Colburn analogy between heat and mass transfer. ashrae.org — ASHRAE Handbook
- US Department of Energy, Uniform Test Method for Measuring the Energy Consumption of Clothes Dryers, 10 CFR Part 430 Subpart B Appendix D2, for the standard test load, the 57.5 % initial moisture content and the Combined Energy Factor definition. ecfr.gov — 10 CFR Part 430
- ENERGY STAR product criteria and certified-product data for clothes dryers, for the Combined Energy Factor levels used to derive kilowatt hours per kilogram of water removed. energystar.gov — clothes dryers
- EU energy labelling for household washing machines and washer-dryers, Regulation (EU) 2019/2014 and its predecessor Directive 95/12/EC, for the spin-drying efficiency classes defined on remaining moisture content. eur-lex.europa.eu — Regulation (EU) 2019/2014
- NIST Chemistry WebBook, enthalpy of vaporisation of water, for the 2.454 MJ/kg at 20 °C and 2.257 MJ/kg at 100 °C used in the energy comparison. webbook.nist.gov
- Alduchov and Eskridge, Improved Magnus form approximation of saturation vapour pressure, Journal of Applied Meteorology 35, 601–609 (1996), for the coefficients 610.94 Pa, 17.625 and 243.04 °C. journals.ametsoc.org — Alduchov & Eskridge 1996
Frequently asked questions about laundry drying time
Does the spin speed matter more than the weather?
For the amount of water you start with, yes. Raising the final spin from 600 rpm to 1200 rpm roughly quadruples the centrifugal field in the drum and cuts residual moisture from about 80 percent of dry mass to about 55 percent, so a 5 kg cotton load starts with about 1.3 kg less water. The weather then decides how fast that remaining water leaves, but no amount of sunshine removes water that the spin cycle could have thrown out for a few watt-hours of extra motor work.
Why does drying almost stop as relative humidity approaches 100 percent?
Evaporation is driven by the difference in water-vapour density between the wet fabric surface and the surrounding air. As relative humidity rises the air already carries most of the vapour it can hold, that difference shrinks toward zero, and the drying rate collapses with it. The fabric also comes into equilibrium at a higher moisture regain, so there is less water it will ever give up. This estimator caps the answer at 120 hours and prints a saturated-air warning rather than an infinite time.
How much energy does line drying save against a tumble dryer?
Evaporating water costs about 2.45 megajoules per kilogram at room temperature, which is 0.68 kilowatt hours. A vented or condenser electric dryer needs roughly 0.98 kilowatt hours per kilogram of water removed on the United States Department of Energy test load, and a heat-pump dryer about 0.55 kilowatt hours because it recovers the heat released when the vapour condenses again. Line drying a load holding 3 kilograms of water therefore avoids roughly 1.7 to 2.9 kilowatt hours.
Will washing dry outdoors below freezing?
Slowly. The water in the fabric freezes and then sublimates, and the saturation vapour pressure over ice at minus 5 degrees Celsius is only about 400 pascals, so the vapour-pressure deficit that drives drying is very small. The estimator still returns a figure below zero degrees and flags it, because the freeze-then-sublimate stage and the stiff-then-thaw stage are not modelled separately.
Line Dry Race: beat the rain front
This is the same drying model, run forwards in time on individual garments. Every item on the washing line has its own moisture meter that falls at the rate this page calculates from the fabric, the local air speed, the local sunshine, the temperature and the humidity of the level. Positions along the line are not equal: the end by the hedge is sheltered and shaded, the middle catches the wind and the sun. Indoors there is a rack, which is windless but rain-proof and warmer, and a tumble dryer, which is fast but charges you energy. A rain front is closing in on a visible timer. Peg each garment where it will finish in time, re-spin the heavy ones to throw water out instead of waiting for it to evaporate, and get everything into the basket before the rain lands.
Level 1 / 5
Score 0
Dry 0 / 3
Rain in —
Dryer energy 0.00 kWh
Best 0
Selected: nothing yet. Press Start the race to hang the first load.
Press Start the race, then move garments between the five line pegs, the two indoor rack slots and the tumble dryer before the rain front arrives.
Keyboard (click or tab to the scene first): ← → choose a garment, ↑ ↓ move the chosen garment to the previous or next position, 1–8 send it straight to that position, S re-spin it at 1400 rpm, R send it to the indoor rack, D send it to the tumble dryer, Enter start the level or move on to the next one, P pause and resume. Pointer and touch: press on a garment and drag it to any peg, rack slot or the dryer, then release. A single tap selects without moving.
- Pegs 1 and 5 sit in the lee of the hedge and the house: little wind, little sun
- Peg 3 is the sweet spot, with the full level wind speed and full sunshine
- Rack slots 6 and 7 are indoors: warmer and rain-proof, but nearly still air
- Position 8 is the tumble dryer: about 2.6 g of water per second, at 0.98 kWh per kg
- Re-spinning throws water out instantly but the garment is out of the air for four seconds
- Towels and denim start wettest and expose the least area, so they need the best pegs
- Humidity haze whitens the scene: in saturated air nothing on the line will ever finish
- Scoring is 120 per dry garment plus a speed bonus, minus 70 per soaked item and 40 per kWh
