The present study was designed to determine the relative importance of individual characteristics such as maximal oxygen uptake (Vo(2max)), adiposity, DuBois body surface area (A(D)), surface to mass ratio (A(D): mass) and body mass, for the individual's reaction to humid heat stress. For this purpose 27 subjects (19 men: 8 women), with heterogeneous characteristics (Vo(2max) 1.86-5.28 1 . min(-1); fat% 8.0%-31.9%; mass 49.8-102.1 kg; A(D) 1.52-2.33 m(2)) first rested (30 min) and then exercised (60 W for 1 h) on a cycle ergometer in a warm humid climate (35 degrees C, 80% relative humidity). Their physiological responses at the end of exercise were analysed to assess their relationship with individual characteristics using a stepwise multiple regression technique. Dependent variables (with ranges) included final values of rectal temperature (T-re 37.5-39.0 degrees C), mean skin temperature (T-sk 35.7-37.5 degrees C), body heat storage (S 3.2-8.1 J . g(-1)), heart rate (HR 100-172 beat . min(-1)), sweat loss (397-1403 g), mean arterial blood pressure (BPa, 68-96 mmHg), forearm blood flow (FBF, 10.1-33.9 ml . 100ml(-1). min(-1)) and forearm vascular conductance (FVC=FBF/BPa, 0.11-0.49 ml . 100ml(-1). min(-1). mmHg(-1)). The T-re, T-sk and S were (34%-65%) determined in the main by Vo(2max) or by exercise intensity expressed as a percentage of Vo(2max) (%Vo(2max)). For T-re, A(D):mass ratio also contributed to the variance explained, with about half the effect of Vo(2max). For T-sk, fat% contributed to the variance explained with about two-third the effect of Vo(2max). Total body sweat loss was highly dependent (50%) on body size (AD or mass) with regular activity level having a quarter of the effect of body size on sweat loss. The HR, similar to T-re, was determined by Vo(2max) (48%-51%), with less than half the effect of A(D) or A(D):mass (20%). Other circulatory parameters (FBF, BPa, FVC) showed little relationship with individual characteristics (< 36% of variance explained). In general: the higher the Vo(2max) and/or the bigger the subject, the lower the heat strain observed. The widely accepted concept: that body core temperature is determined by exercise intensity expressed as % Vo(2max) and sweat loss by absolute heat load, was only partially supported by the results. For both variables, other individual characteristics were also shown to contribute.