Heat index
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Heat Index (HI) is an index that combines air temperature and relative humidity to determine an apparent temperature — how hot it actually feels. The human body normally cools itself by perspiration, or sweating, in which the water in the sweat evaporates and carries heat away from the body. However, when the relative humidity is high, the evaporation rate of the water is reduced. This means heat is removed from the body at a lower rate, causing it to retain more heat than it would in dry air. Measurements have been taken based on subjective descriptions of how hot subjects feel for a given temperature and humidity, allowing an index to be made which corresponds a temperature and humidity combination to a higher temperature in dry air.
At high temperatures, the level of relative humidity needed to make the Heat Index higher than the actual temperature is lower than at cooler temperatures. For example, at 80°F (approximately 27°C), the Heat Index will agree with the actual temperature if the relative humidity is 45%, but at 110°F (roughly 43°C), any relative-humidity reading above 17% will make the Heat Index higher than 110. Humidity is deemed not to raise the apparent temperature at all if the actual temperature is below approximately 68°F (20°C) — essentially the same temperature colder than which wind chill is thought to commence.
As relative humidity increases, however, first haze and ultimately thicker cloud cover must develop, reducing the amount of direct sunlight reaching the surface; thus there is an inverse relationship between maximum potential temperature and maximum potential relative humidity, therefore making, say, a simultaneous temperature of 50 °C (122 °F) and 90 per cent relative humidity physically impossible. Because of this factor, it is believed that the highest heat-index reading actually attainable anywhere on Earth is approximately 70 °C (158 °F).
A good example of the difference between heat index and true temperature would be comparing the climates of New Orleans, Louisiana and Bakersfield, California. New Orleans has lower heat temperatures due to being closer to the Gulf of Mexico, yet the city has a higher heat index because it is a humid heat. Likewise, while Bakersfield actually has hotter daytime temperatures, Bakersfield has a dry heat, so it doesn't feel as hot.
Sometimes the heat index and the wind chill factor are denoted collectively by the single terms "apparent temperature" or "relative outdoor temperature."
In Canada the term humidex is used for the heat index developed by Environment Canada.
See also
External links
- National Science Digital Library - Heat Index (http://www.nsdl.arm.gov/Library/glossary.shtml#Heat_index)
- An Introduction to Heat Index (http://avc.comm.nsdlib.org/cgi-bin/wiki_grade_interface.pl?An_Introduction_To_Heat_Index). A lesson plan that deals with heat index.
- Heat Index Calculator (http://avc.comm.nsdlib.org/java/heatindex/heatindex.html)
- Wind Chill and Humidex (http://ptaff.ca/humidex/?lang=en_CA) Criticism about the use of Wind chill and humidex