| OCR Text |
Show 9 41°C to 43 The °c on relatively central system. dissipation is the heat the deep body temperature. Heat progressively increase stimulate a thickness of the waste of heat of fat conditions. by drainage venous in rectal increase an temperature core during prolonged load to of subcutaneous is transported by storage and large enough threat primary effectiveness reflected core, naturally primarily by acclimatization influenced stress, high so inadequate dissipation The heat. Metabolic waste heat to from the making ambient environmental and layer, is actually able to tolerate most are balance internally produced to the of body's thermoregulatory the ambient conditions, thermoregulatory body of temperature regulation efficient that humans occurring system. efficiency low muscular dissipation capacity Human nervous is counterbalanced by the relatively exercising body heat the in order to drive heat to error exercise loss • mechanisms stabilize (Gisolfi production. heat production, °c 4 or exercise session temperature work is load and cutaneous Wenger, When heat rectal loss higher during vasodilation a the to storage will then keep pace with able to is unable to keep pace with has been strenuous This rise 1977). proportional provides are temperature (Nadel, Heat 1984). if heat loss mechanisms heat increase & shown to 90-minute in rectal relative rather than absolute central (Gisolfi, stimulus to 1983). sweating Because heat and |
