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- W2011056056 abstract "Abstract Thermal discomfort, defined as an expression of man's dissatisfaction with his thermal environment and measured by the magnitude estimates method, has been observed: (1) during humidity transients, when the ambient temperature is held constant at 32, 36, and 40°C; (2) during transients of the ambient temperature at constant relative humidity; and (3) during transients caused by both radiant heat and humidity while the ambient temperature is held at 32°C. The best single physiological index of thermal discomfort, especially without the presence of thermal radiation, is skin wettedness, which is defined as the ratio of the observed skin evaporative heat loss to the maximum evaporative capacity of the environment for a completely wet skin surface. Radiant heat (RH), by raising mean skin temperature by 1.5–2°C, causes the rate of rise of thermal discomfort with skin wettedness to increase. A biophysical effective temperature (ET ), defined as the temperature of a black enclosure at 50% RH, in which man would exchange the same heat by radiation, convection, and evaporation as in the observed environment, correlates well with thermal discomfort regardless of the complexity of the thermal environment. The discomfort, caused by skin wettedness itself, may be attributed to the increasing strain caused first by the internal drive to secrete regulatory sweat, and second by the increased peripheral resistance at the skin surface." @default.
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- W2011056056 date "1974-04-01" @default.
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- W2011056056 title "Physiological and physical factors associated with warm discomfort in sedentary man" @default.
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- W2011056056 doi "https://doi.org/10.1016/0013-9351(74)90154-6" @default.
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