Background InformationThe temperature of the air in winter is not always a reliable indicator of how cold you will feel outdoors. Wind speed, relative humidity, and sunshine also have an effect. What you are wearing, how healthy you are, and your metabolism all affect how cold you feel. "Coldness" is related to the loss of heat from exposed flesh. Hypothermia, a life-threatening condition caused by the lowering of a person's core body temperature, can be prevented by understanding the chilling effect of wind.In 1939, Paul Siple coined the term "wind chill" to describe the relative discomfort caused by a combination of wind and temperature, but his index did not work for temperatures above freezing or for high wind speeds. In 1941, Siple and Charles Passel developed a new formula to determine wind chill from experiments made at Little America, Antarctica. Experiments could not be conducted on human skin without permanent injury, so Siple and Passel measured how long it took to freeze 250 grams of water in a plastic cylinder during different combinations of wind and temperature. They assumed that the rate of heat loss was proportional to the difference in temperature between that of the cylinder and that of the surrounding air. They plotted results in kilogram calories per square meter per hour (kg cal/m2/h) against wind speed in meters per second (m/s) to create a nomogram. A nomogram is a graph that has several lines arranged so an unknown value can be read from the intersection of one of these lines and a known value. From the Wind Chill Index Nonogram, scientists create a wind chill table. The wind chill index or equivalent temperature is based on a neutral skin temperature of 33 Degrees C, or 91.4 Degrees Fahrenheit. It represents how cold the air feels to the skin, not how cold it is! Furthermore, the wind chill effect applies only to human flesh, not houses, cars, or clothing. The index does not take into account all possible heat losses of the body. With physical exertion, body heat production rises, perspiration begins, and evaporation removes heat from the body. A body can lose heat by contact with cold surfaces and by breathing cold air, which removes heat from the lungs. The next time you want to know how cold it is outdoors, check the thermometer. But keep in mind that other things, such as wind speed, body fat, individual metabolism, and protective clothing, all help to determine how "chilly" you feel. In the procedure for this activity, you will use the Wind Chill Index Nomogram to find the temperatures needed to complete a wind chill table. The line at four mph on the nomogram approximates the wind speed generated by someone walking briskly under calm conditions. This is the standard wind speed chosen for calculating wind chill equivalent temperatures. Wind chill refers to the temperature which, at a four mph wind speed, cools the skin at the same rate as the observed (ambient) temperature and wind speed. |
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ProcedureAssume that the air temperature is 20 Degrees Fahrenheit, and the wind speed is ten mph. You are walking to school. What temperature would you actually feel?To answer this question, perform the following steps.
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Questions
Print at 92% for use in this Activity. |
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Conclusionsat the top of this web page and write your conclusions here. Figure 4.4. Conclusions Sheet Print at 92% for use in this Activity. |
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Safety Information
Hypothermia
Furthermore, hypothermia occurs even more rapidly when the person is in the water. Often, drowning victims succumb to hypothermia before actually drowning. Whether in air or water, victims of hypothermia frequently do not realize what is happening. Everyone must be aware of hypothermia and help each other. These are the symptoms of hypothermia: To avoid hypothermia, follow these guidelines. Even mild symptoms should be treated immediately. Frostbite
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For Your InformationThe nomogram is based on a general formula for heat loss. Heat loss occurs by means of radiation, conduction, and convection. Combining all effects, the general formula for heat loss (H) is,where:
The values of the constants A, B, and C vary widely in formulas presented by different investigators. This is to be expected since heat loss (H) depends on certain properties of the body being cooled. This formula measures the cooling power of the wind and temperature in complete shade and does not consider the gain of heat from incoming radiation, either direct or diffuse. Under conditions of bright sunshine, the heat loss should be reduced by about 200 kg cal/m2/h. |