FIRE WEATHER · DEAD FUEL MOISTURE
Equilibrium Moisture Content Calculator
Translate air temperature and relative humidity into the moisture level dead wildland fuel tends toward. Then explore an idealized response over a selected fuel timelag.
CALCULATED EQUILIBRIUM
Simard middle-RH equation · 10–50% RH
At constant conditions, the idealized 10-hour fuel estimate moves from 12.0% toward 5.8%.
PIECEWISE MODEL
One atmosphere.
Three humidity ranges.
The calculator uses the Simard (1968) equilibrium-moisture functions reproduced by the USDA Forest Service. Temperature is evaluated in degrees Fahrenheit and RH as percent.
E = 0.03229 + 0.281073H − 0.000578HTE = 2.22749 + 0.160107H − 0.014784TE = 21.0606 + 0.005565H² − 0.00035HT − 0.483199Hm(t) = E + [m(0) − E]e−t/τThe optional time response is an idealized exponential approximation. E is equilibrium moisture, m(0) is initial moisture and τ is the selected timelag.
INTERPRETATION
Dead fuels follow weather—with delay.
Relative humidity is the dominant atmospheric driver of EMC, while temperature has a smaller effect. Fine fuels respond faster than larger woody fuels. A current temperature/RH pair cannot reconstruct the fuel’s previous weather exposure.
Timelag classes are modelling categories, not exact drying times for every particle.
Sources and limits
This tool estimates EMC under constant ambient conditions. It does not estimate live fuel moisture, rain wetting, solar-heated fuel temperature, local fire danger or probability of ignition.
USDA Forest Service: moisture calculations and Simard equations · NWCG: Weather and Fuel Moisture · NWCG: fuel timelag training
Quick answers
Is EMC the same as actual fuel moisture?
No. EMC is the level approached if atmospheric conditions remain constant long enough.
Can this predict fire behaviour?
No. Fuel moisture is only one input among fuels, wind, slope and other factors.
Does it apply to live vegetation?
No. Live fuel moisture is governed by plant physiology as well as weather.