In previous studies based on the heat balance theory, we derived two formulae that expressed the heat balance equation of the human body standardized by skin temperature, in terms of the wet bulb temperature T
w, black globe temperature T
g, and air temperature T
a. On the basis of these formulae, we introduced WBGT* as a new thermal index. The WBGT* is of the same form as the original WBGT formulae empirically established by Yaglou et al. The differences between these two sets of formulae are as follows:
1. The WBGT* for an environment devoid of solar radiation, WBGT*=0.85T
w+0.20T
g, is different from the original WBGT proposed by Yaglou et al., WBGT=0.7T
w+0.3T
g, in terms of the coefficients.
2. The WBGT* for an environment with solar radiation is WBGT*=0.84T
w+0.30T
g−0.08T
a; the WBGT derived by Yaglou et al. is WBGT=0.7T
w+0.2T
g+0.1T
a. The WBGT* is characterized by a negative coefficient of T
a.
The purpose of the present study was to examine the significance of the difference between the WBGT derived by Yaglou et al. and the WBGT* introduced by us and to interpret the thermophysical meaning of the negative coefficient of T
a in the WBGT*. The following conclusions were drawn:
1. In the case of a highly humid environment, the difference between the values calculated using Yaglou’s WBGT and our WBGT* was found to be 1.5°C. This difference corresponds to a difference of almost 4∼5°C in the air temperature. Thus, in a humid environment, the values obtained by using Yaglou’s WBGT are less than those obtained by using our WBGT*.
2. The negative coefficient of T
a can be explained in terms of the difference between the operative temperature of humans and T
g and the negative correlation between T
a and the environmental water vapor pressure P
a at a constant T
w. This negative correlation indicates that for a constant T
w, an increase in T
a leads to a decrease in P
a.
View full abstract