Heat Index
Calculator
Calculate the real feels-like temperature using the official NWS Rothfusz formula. Enter temperature with relative humidity or dew point — get heat index and danger level instantly.
Heat Index Risk Levels
Official NWS heat danger categories and recommended precautions.
| Heat Index (°F) | Heat Index (°C) | Category | Health Effects | Action |
|---|---|---|---|---|
| 80–90°F | 27–32°C | Caution | Fatigue possible with prolonged activity | Stay hydrated; take breaks in shade |
| 91–103°F | 33–39°C | Extreme Caution | Heat cramps & heat exhaustion possible | Limit strenuous activity; monitor closely |
| 103–124°F | 40–51°C | Danger | Heat exhaustion likely; heat stroke possible | Avoid strenuous outdoor activity |
| 125°F+ | 52°C+ | Extreme Danger | Heat stroke highly likely | Stay indoors in AC; call 911 if symptoms appear |
⚠️ Direct sunlight can add up to 15°F (8°C) above the calculated heat index. Values shown are for shade with light wind.
Heat Index Chart (°F)
Temperature (columns) × Relative Humidity (rows) = Heat Index °F. Color = risk category.
Direct Sun Adds Up to 15°F More
The NWS heat index is calculated for shady, light-wind conditions. In direct sunlight, add up to 15°F (8°C) to the heat index value. A 100°F heat index in the shade could feel like 115°F in the sun — potentially life-threatening.
Heat exhaustion: Heavy sweating, cool pale clammy skin, fast weak pulse, nausea, dizziness, muscle cramps. Move to cool area, apply cold wet cloths, sip water.
Heat stroke (emergency): Body temp ≥104°F (40°C), hot dry skin OR profuse sweating, confusion, rapid strong pulse, loss of consciousness. Call 911 immediately — do not give fluids. Cool the person by any means available.
Hydration: Drink water before you feel thirsty — 1 cup (8 oz) every 20 minutes during activity in heat. Avoid caffeine and alcohol which accelerate dehydration.
Acclimatization: It takes 10–14 days for the body to adjust to working in heat. Limit strenuous outdoor activity during heat waves, especially in the first 2 weeks. Schedule activity for early morning or after sunset when heat index is lowest.
How the Heat Index Is Calculated
The heat index was developed by Robert G. Steadman in 1979 and later adapted by the National Weather Service using the Rothfusz regression equation. It quantifies how hot it feels to the human body when relative humidity is factored in alongside the actual air temperature — because humidity directly impairs the body's primary cooling mechanism: sweat evaporation.
The NWS Rothfusz Equation (°F)
The Metric Version (°C)
When the Formula Applies
The Rothfusz equation is valid when air temperature is at or above 80°F (27°C) and relative humidity is at or above 40%. At lower temperatures or very low humidity, the simplified Steadman formula or a straight temperature reading is more appropriate. The formula also assumes shady conditions with light wind — direct sun or strong wind will alter the perceived temperature.
Converting Dew Point to Relative Humidity
If you have the dew point temperature instead of relative humidity, our calculator converts it automatically using the Magnus formula:
Why Humidity Makes Heat More Dangerous
The human body regulates core temperature primarily through sweat evaporation. When sweat evaporates from skin, it carries heat away — a process called evaporative cooling. This mechanism is highly efficient in dry air but fails progressively as humidity rises.
The Dew Point Threshold
Dew point is a more reliable discomfort indicator than relative humidity because it measures absolute moisture in the air rather than how saturated the air is relative to temperature. A dew point below 55°F (13°C) feels comfortable to most people. Between 60–65°F (16–18°C) it feels humid. Above 70°F (21°C) it feels oppressive, and above 75°F (24°C) it becomes dangerous — the body's cooling system struggles to keep up even at rest.
Heat Acclimatization
The human body can adapt to working in heat through a process called heat acclimatization, which takes 10–14 days of gradual exposure. Acclimatized individuals sweat more efficiently, earlier, and in greater volume — lowering core temperature more effectively. Newcomers to a heat wave are at significantly higher risk than acclimatized individuals even at the same heat index level.
The Urban Heat Island Effect
Urban areas can experience heat index values significantly higher than surrounding rural areas due to the urban heat island effect — dark asphalt and concrete absorb and re-radiate heat, reducing nighttime cooling and elevating daytime temperatures by 2–10°F (1–6°C) above rural surroundings. This compounds the heat index risk for urban populations during heat waves.