It remains unclear whether aerobic fitness, as defined by the maximum rate of oxygen consumption (V O 2 max), independently improves heat dissipation in uncompensable environments, or whether the thermoregulatory adaptations associated with heat acclimation are due to repeated bouts of exercise-induced heat stress during regular aerobic training. The present analysis sought to determine ifV O 2 max independently influences thermoregulatory sweating, maximum skin wettedness (max) and the change in rectal temperature (ΔT re) during 60 min of exercise in an uncompensable environment (37.0 ± 0.8 • C, 4.0 ± 0.2 kPa, 64 ± 3% relative humidity) at a fixed rate of heat production per unit mass (6 W kg −1). Retrospective analyses were performed on 22 participants (3 groups), aerobically unfit (UF; n = 7;V O 2 max : 41.7 ± 9.4 ml kg −1 min −1), aerobically fit (F; n = 7;V O 2 max : 55.6 ± 4.3 ml kg −1 min −1 ; P < 0.01) and aerobically unfit (n = 8) individuals, before (pre;V O 2 max : 45.8 ± 11.6 ml kg −1 min −1) and after (post; V O 2 max : 52.0 ± 11.1 ml kg −1 min −1 ; P < 0.001) an 8-week training intervention. max was similar between UF (0.74 ± 0.09) and F (0.78 ± 0.08, P = 0.22). However, max was greater post-(0.84 ± 0.08) compared to pre-(0.72 ± 0.06, P = 0.02) training. During exercise, mean local sweat rate (forearm and upper-back) was greater post-(1.24 ± 0.20 mg cm −2 min −1) compared to pre-(1.04 ± 0.25 mg cm −2 min −1 , P < 0.01) training, but similar between UF (0.94 ± 0.31 mg cm −2 min −1 , P = 0.90) and F (1.02 ± 0.30 mg cm −2 min −1). The ΔT re at 60 min of exercise was greater pre-(1.13 ± 0.16 • C, P < 0.01) compared to post-(0.96 ± 0.14 • C) training, but similar between UF (0.85 ± 0.29 • C, P = 0.22) and F (0.95 ± 0.22 • C). Taken together, aerobic training, notV O 2 max per se, confers an increased max , greater sweat rate, and smaller rise in core temperature during uncompensable heat stress in fit individuals.