Consequences of partial body warming and cooling for the drives to local sweat rates

Climatic chamber experiments were carried out on young, healthy male students. The ambient temperature was 36 degrees C, while local warming of one extremity was compensated for by heatflow-equivalent cooling of the ipsilateral extremity by on-line calculation of the heat balance. When warming the arm and cooling the leg (type 1 experiments), a slight, but not statistically significant increase of local sweat rates at these extremities was recorded. However, when cooling the arm and warming the leg (type 2 experiments), both corresponding local sweat rates declined. The divergent results are interpreted in terms of previously reported different central weighting factors for skin temperatures as determined: (1) by the weighting for the area, or (2) by the weighting for the area and the sensitivity of the local sweat rate to warming and cooling. This means that the central processing of the mean skin temperature may be different for cooling and warming and that in both cases values can be different from recorded (area weighted) skin temperature. Calculating this modified mean skin temperature, we conclude that type 1 experiments may be interpreted by the hypothesis that the central regulator has a status very near an overall heat-balance, whereas type 2 experiments, although also carried out at heat-balance, may be centrally evaluated as predominant cooling. In these experiments again the central drives representing the whole body thermal state seem to override both the direct and centrally mediated local drives.