During exposure to high altitude, hypoxia develops because of reductions in barometric pressure and partial pressure of O-2. Although several studies have examined the effects of hypoxia on exercise performance and physiological responses, such as maximal minute ventilation (V center dot(Emax)) and maximal oxygen uptake (V center dot O-2max), how barometric pressure reduction (hypobaria) modulates them remains largely unknown. In this study, 11 young men performed incremental treadmill running tests to exhaustion under three conditions chosen at random: normobaric normoxia (NN; 763 +/- 5 mmHg of barometric pressure, equivalent to sea level), hypobaric hypoxia (HH; 492 +/- 1 mmHg of barometric pressure, equivalent to 3500 m above sea level (m a.s.l.)), and hypobaric normoxia (HN; 492 +/- 1 mmHg of barometric pressure while breathing 32.2 +/- 0.1% O-2 to match the inspiratory O-2 content under NN). V center dot(Emax) was higher in HN than in NN (160.9 +/- 10.7 vs. 150.7 +/- 10.0 L min(-1), P < 0.05). However, no differences in V center dot O-2max and arterial oxyhemoglobin saturation were observed between NN and HN (all P > 0.05). Time to exhaustion was longer in HN than in NN (932 +/- 83 vs. 910 +/- 79 s, P < 0.05). These results suggest that reduced air density during exposure to an altitude of 3500 m a.s.l. increases maximal ventilation and extends time to exhaustion without affecting oxygen consumption or arterial oxygen saturation.