Weather calculator

Calculate the Heat Index From Temperature and Humidity

Heat index 105°F (41°C)
NWS category Danger

How the heat index calculator works

The heat index is how hot humid air feels to the body, because sweat evaporates more slowly when the air is already moist. This calculator uses the same regression the US National Weather Service uses for its heat advisories, including its corrections for very dry and very humid air.

NWS Rothfusz regression (T ≥ 80°F) Steadman simple formula below 80°F Dew point converted to RH with the Magnus formula

Quick tips

  • It assumes shade and a light breeze. In full sun the felt heat can run up to 15°F (8°C) higher than the heat index.
  • Below 80°F (27°C) it barely matters. Humidity only starts to add real heat stress once the air is warm.
  • Dew point is the steadier input. Relative humidity swings through the day as the temperature changes; dew point does not.

NWS heat index categories

Heat indexCategoryWhat can happen with prolonged exposure
80-90°F (27-32°C)CautionFatigue is possible with prolonged exposure or activity
90-103°F (32-39°C)Extreme cautionHeat cramps and heat exhaustion are possible
103-124°F (39-51°C)DangerHeat cramps and heat exhaustion are likely; heat stroke is possible
125°F (52°C) and aboveExtreme dangerHeat stroke is highly likely

Frequently asked questions

Is a heat index of 105°F dangerous?
Yes. 105°F (41°C) falls in the NWS "Danger" band, where heat exhaustion is likely with prolonged activity and heat stroke is possible. Many NWS offices issue a heat advisory from a heat index of about 100-105°F.
Why does the calculator ask for dew point as an option?
Forecasts and weather stations often quote dew point, and it is a more stable measure of moisture than relative humidity. The calculator converts it to relative humidity first, then applies the heat index formula.
Does the heat index work in cool weather?
Not meaningfully. Below about 80°F (27°C) the formula is outside the range it was fitted for, so the calculator falls back to the simpler Steadman approximation, which stays close to the air temperature.