Wind chill - AbsoluteAstronomy.com

Wind chill is the felt air temperature

Felt air temperature

Felt air temperature is a quantitative measure that indicates the amount of heat the human body loses outdoors in a given time and place....

on exposed skin

Human skin

The human skin is the outer covering of the body. In humans, it is the largest organ of the integumentary system. The skin has multiple layers of ectodermal tissue and guards the underlying muscles, bones, ligaments and internal organs. Human skin is similar to that of most other mammals,...

due to wind. The wind chill temperature is always lower than the air temperature, and the windchill is undefined at the higher temps (above 10 °C [50 °F]). Humidity on the skin can result in a higher felt air temperature, which is accurately termed the heat index

Heat index

The heat index is an index that combines air temperature and relative humidity in an attempt to determine the human-perceived equivalent temperature — how hot it feels, termed the felt air temperature. The human body normally cools itself by perspiration, or sweating, which evaporates and carries...

(or humidex

Humidex

The humidex is an index number used by Canadian meteorologists to describe how hot the weather feels to the average person, by combining the effect of heat and humidity. The humidex is a unit-less number based on the dew point, but it is equivalent to dry temperature in degrees Celsius...

), and is used instead.

Explanation

The human body loses heat through convection

Convection

Convection is the movement of molecules within fluids and rheids. It cannot take place in solids, since neither bulk current flows nor significant diffusion can take place in solids....

, evaporation

Evaporation

Evaporation is a type of vaporization of a liquid that occurs only on the surface of a liquid. The other type of vaporization is boiling, which, instead, occurs on the entire mass of the liquid....

, conduction, and radiation

Radiation

In physics, radiation is a process in which energetic particles or energetic waves travel through a medium or space. There are two distinct types of radiation; ionizing and non-ionizing...

. The rate of heat loss by a surface through convection depends on the wind speed above that surface: the faster the wind speed, the more readily the surface cools. For inanimate objects, the effect of wind chill is to reduce any warmer objects to the ambient temperature more quickly. It cannot, however, reduce the temperature of these objects below the ambient temperature, no matter how great the wind velocity. For most biological organisms, the physiological response is to maintain surface temperature in an acceptable range so as to avoid adverse effects. Thus, the attempt to maintain a given surface temperature in an environment of faster heat loss results in both the perception of lower temperatures and an actual greater heat loss increasing the risk of adverse effects such as frostbite

Frostbite

Frostbite is the medical condition where localized damage is caused to skin and other tissues due to extreme cold. Frostbite is most likely to happen in body parts farthest from the heart and those with large exposed areas...

and death.

Formulae and tables

Many formulae exist for wind chill because, unlike temperature, there is no universally agreed standard for what the term should mean. All the formulae attempt to provide the ability to qualitatively predict the effect of wind on the temperature humans perceive. Within different countries weather services use a standard for their country or region. U.S. and Canadian weather services use a model accepted by the National Weather Service

National Weather Service

The National Weather Service , once known as the Weather Bureau, is one of the six scientific agencies that make up the National Oceanic and Atmospheric Administration of the United States government...

. That model has evolved over time.

The first wind chill formulae and tables were developed by Paul Allman Siple and Charles Passel working in the Antarctic before the Second World War, and were made available by the National Weather Service

National Weather Service

by the 1970s. It was based on the cooling rate of a small plastic bottle as its contents turned to ice while suspended in the wind on the expedition hut roof, at the same level as the anemometer. The so-called Windchill Index provided a pretty good indication of the severity of the weather. In the 1960s, wind chill began to be reported as a wind chill equivalent temperature

Equivalent temperature

Equivalent temperature is the temperature of an air parcel from which all the water vapor has been extracted by an adiabatic process.Air contains water vapor that has been evaporated into it from liquid sources . The energy needed to do that has been taken from the air...

(WCET), which is theoretically less useful. The author of this change is unknown, but it was not Siple and Passel as is generally believed. At first, it was defined as the temperature at which the windchill index would be the same in the complete absence of wind. This led to equivalent temperatures that were obviously exaggerations of the severity of the weather. Charles Eagan realized that people are rarely still and that even when it was calm, there was some air movement. He redefined the absence of wind to be an air speed of 1.8 metres per second (4 mph), which was about as low a wind speed as a cup anemometer could measure. This led to more realistic (warmer-sounding) values of equivalent temperature

Equivalent temperature

Original model

Equivalent temperature

was not universally used in North America until the 21st century. Until the 1970s, the coldest parts of Canada reported the original Wind Chill Index, a three or four digit number with units of kilocalories/hour per square meter. Each individual calibrated the scale of numbers personally, through experience. The chart also provided general guidance to comfort and hazard through threshold values of the index, such as 1400, which was the threshold for frostbite

Frostbite

. The change in the 1970s to the metric system units in Canada changed all the numbers, making it confusing and requiring that everyone recalibrate their personal wind chill scale. It should never have had units in the first place, as Siple later pointed out for it was not a measure of human heat loss but simply a number proportional to human heat loss.

The original formula for the index was:

Where:

= Wind chill index, kcal/m²/h

= Wind velocity, m/s

= Air temperature, °C

The general public seems to have been put off by the strange sounding units, either the old ones or the newer watts per square metre, and developed a strong preference for equivalent temperature

Equivalent temperature

, a deceptive simplification that only seems to be easier to understand. Even in the cold areas of Canada, broadcast media began to switch to the newer method of reporting after metrification.

North American wind chill index

In November 2001 the National Weather Service

National Weather Service

implemented the new wind chill index, used by the U.S. and Canadian weather services, which is determined by iterating a model of skin temperature under various wind speeds and temperatures. The model used standard engineering correlations of wind speed and heat transfer rate. Heat transfer was calculated for a bare face in wind, facing the wind, while walking into it at 1.4 metres per second (3.1 mph). The model corrects the officially measured wind speed to the wind speed at face height, assuming the person is in an open field. The results of this model may be approximated, to within one degree, from the following formula:

where

is the wind chill index based on the Celsius scale,

is the air temperature in °C, and

is the air speed in km/h measured at 10 metres (32.8 ft), standard anemometer

Anemometer

An anemometer is a device for measuring wind speed, and is a common weather station instrument. The term is derived from the Greek word anemos, meaning wind, and is used to describe any airspeed measurement instrument used in meteorology or aerodynamics...

height).

The equivalent formula in US customary units is:

where

and

are measured in °F, and

in mph.

Click here http://www.weather.gov/os/windchill/index.shtml for a chart of windchills based on this formula.

Windchill Temperature is only defined for temperatures at or below 10 °C (50 °F) and wind speeds above 4.8 kilometres per hour (3 mph).

As the air temperature falls, the chilling effect of any wind that is present increases. For example, a 16 km/h (9.9 mph) wind will lower the apparent temperature by a wider margin at an air temperature of -20 °C, than a wind of the same speed would if the air temperature were -10 °C.
The method for calculating wind chill has been controversial because experts disagree on whether it should be based on whole body cooling either while naked or while wearing appropriate clothing, or if it should be based instead on local cooling of the most exposed skin, such as the face. The internal thermal resistance is also a point of contention. It varies widely from person to person. Had the average value for the subjects been used, calculated WCET's would be a few degrees more severe.

The 2001 WCET is a steady state calculation (except for the time to frostbite estimates). There are significant time-dependent aspects to wind chill because cooling is most rapid at the start of any exposure, when the skin is still warm.

The exposure to wind depends on the surroundings and wind speeds can vary widely depending on exposure and obstructions to wind flow.

Australian Apparent Temperature

The Australian Bureau of Meteorology uses a different formula for cooler temperatures.

The formula is:
AT = Ta + 0.33e − 0.70ws − 4.00

Where:
Ta = Dry bulb temperature (°C)
e = Water vapour pressure (hPa)
ws = Wind speed (m/s) at an elevation of 10 meters

The vapour pressure can be calculated from the temperature and relative humidity using the equation:
e = rh / 100 * 6.105 * 2.718281828 ^ ( 17.27Ta / ( 237.7 + Ta ) )

Ta = Dry bulb temperature (°C)
rh = Relative Humidity [%]
^ = means to the power of

The Australian formula includes the important factor of humidity

Humidity

Humidity is a term for the amount of water vapor in the air, and can refer to any one of several measurements of humidity. Formally, humid air is not "moist air" but a mixture of water vapor and other constituents of air, and humidity is defined in terms of the water content of this mixture,...

and is somewhat more involved than the simpler North American model. However humidity can be a significant factor. The North American formula is designed mainly on the basis that it is expected to be applied at low temperatures, when humidity levels are also low, and also for much colder temperatures (as low as -50F). As these are qualitative models this is not necessarily a major failing.

A more exhaustive model (which factors in Wind Speed) was developed for the US Navy stationed in Parris Island in South Carolina. It was developed with a consideration for Heat Stroke due to the high humidity off the Island during summer months. It utilized three specialized thermometers. This research is what the Australian Apparent Temperature formula was derived from.

Clothing, wet-cold and exposure duration

Wet clothing and the duration of a person's exposure to wind also affect the felt air temperature. The wind chill formulae do not take account of the variation of clothing worn and how wet or dry a person is. The typical assumption is that a person will be properly dressed and dry. Models generally also assume that thermodynamic equilibrium

Thermodynamic equilibrium

In thermodynamics, a thermodynamic system is said to be in thermodynamic equilibrium when it is in thermal equilibrium, mechanical equilibrium, radiative equilibrium, and chemical equilibrium. The word equilibrium means a state of balance...

exists, something that might not be the case if a person quickly run outdoors and back indoors, for example.

External links

National Weather Service Wind Chill Temperature Index Table of wind chill temperatures
National Science Digital Library - wind chill Temperature
Environment Canada - Wind Chill
Weather Images Wind Chill Chart and Introduction
An Introduction to Wind Chill A lesson plan on wind chill
A Cold Wind Blowing An article on wind chill and tables in SI units
Wind Chill and Humidex Criticism about the use of wind chill and humidex
An article about wind chill from The Canadian Encyclopedia

The source of this article is wikipedia, the free encyclopedia. The text of this article is licensed under the GFDL.