ET0 Calculator — Reference Evapotranspiration (FAO-56 Penman-Monteith)

This ET0 calculator (also written ET₀) estimates reference evapotranspiration using the FAO-56 Penman-Monteith equation, the international standard for estimating atmospheric water demand. As a reference evapotranspiration calculator, it takes your local temperature, humidity, wind speed, and solar radiation and determines how much water a standardized grass surface loses per day. ET0 is the foundation of all irrigation scheduling — multiply it by a crop coefficient (Kc) to convert reference ET0 into actual crop ET for your field.

Inputs Explained

Temperature (Min / Max)
Daily minimum and maximum air temperature. Drives saturation vapor pressure — warmer air holds more moisture, increasing evaporative demand.
Relative Humidity (Min / Max)
Daily minimum and maximum relative humidity. Determines the vapor pressure deficit: drier air pulls more water from the soil and crop canopy.
Wind Speed
Average daily wind speed at 2 m height. Wind replaces moist air near the crop with drier air, accelerating transpiration.
Solar Radiation
Incoming shortwave radiation in MJ/m²/day. Provides the energy that powers evaporation from the soil and plant surfaces.
Elevation & Latitude
Site elevation adjusts atmospheric pressure; latitude adjusts extraterrestrial radiation for your location on the globe.

How This Calculator Works

Based on: FAO-56 Penman-Monteith equation
Best for: Daily or weekly ET₀ estimation for irrigation planning in any climate
Check locally: Compare results with your regional agricultural weather network (CIMIS, CoAgMet, FAWN, etc.)
Units supported: Metric (mm/day, °C, m/s, MJ/m²/day), Imperial (in/day, °F, mph, Langleys)

Worked Example

Mid-summer irrigation planning in a temperate inland valley

  1. 1. Enter temperatures

    Min 18 °C, Max 34 °C — gives a mean of 26 °C and high saturation vapor pressure.

  2. 2. Enter humidity

    Min RH 30%, Max RH 75% — yields a significant vapor pressure deficit.

  3. 3. Enter wind speed

    2.5 m/s at 2 m height — moderate wind enhances turbulent transfer.

  4. 4. Enter solar radiation

    24 MJ/m²/day — typical clear-sky mid-summer value at 38° latitude.

  5. 5. Set location

    Elevation 150 m, latitude 38° N — adjusts pressure and extraterrestrial radiation.

ET₀ ≈ 6.3 mm/day — multiply by crop Kc (e.g., 1.15 for mid-season corn) to get crop ET of about 7.2 mm/day.

How to Interpret Your Results

ConditionWhat It Means
ET₀ < 2 mm/dayLow atmospheric demand — cool, humid, or overcast conditions. Irrigation frequency can be reduced.
ET₀ 2–4 mm/dayModerate demand — typical of spring/autumn or coastal climates. Standard irrigation scheduling applies.
ET₀ 4–6 mm/dayHigh demand — warm, sunny conditions. Most irrigated crops need daily or every-other-day watering.
ET₀ > 6 mm/dayVery high demand — hot, dry, windy conditions. Irrigation systems must run at near-full capacity.

Common Mistakes to Avoid

Using air temperature from a non-standard location (e.g., direct sun)

Always use shaded, ventilated temperature readings at standard height (1.5–2 m) per WMO guidelines.

Entering wind speed measured at 10 m height without converting

Convert 10 m wind to 2 m using the logarithmic profile: u₂ = u₁₀ × 4.87 / ln(67.8 × 10 − 5.42).

Confusing ET0 with actual crop ET

ET0 is the reference rate for grass. Multiply by the crop coefficient (Kc) to get actual crop ET for irrigation scheduling.

Mixing metric and imperial units between inputs

Keep temperature, wind speed, and solar radiation in one unit system (metric mm/°C/m/s or imperial in/°F/mph) — the calculator converts internally, but mismatched manual entries produce a wrong ET0.

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