| OCR Text |
Show 18 temperature will drifts. rate will be with a Adams in higher enhanced require ale et still-air environment due to the a rectal McLellan, directly demand increase by the & Bainton, in breath A to thermoneutral other & conditions oxygen Fahey, the altered dissipation heat of hot a of be (Mitchell an uptake an dissipated et as alo, elevated requirements of thus and reduced metabolic 1984). heat transfer may simple addition also metabolic environment cardiovascular, by ambient conditions. waste & smaller a can metabolic response to prolonged exercise evaporative the in is apparent that thermoregulatory, significantly to heat waste ventilatory muscles, higher a efficiency (Brooks and assisted by and more (Skinner of excess increase the energy also and to contributing in ventilation rate due to higher diaphragm It ventilation inflated an Accomplished mainly by 1974). frequency however, body temperature will in elevated ventilation rate temperature will the general, elevation in tidal volume, compared 1972). In stimulate ventilation rate (Henry elevation vary with different elevate minute An 1980). dehydration during also may conditions. metabolic cost will exercise temperature. Pulmonary dynamics environmental heart as confirmed that heart rate (1989) skin circulation and rising rate work decreasing a be by enhanced can be contribution convective and significantly adjusted by ambient wind to the exercise |
