[Estimation of gasometric values at different altitudes above sea level in Mexico]

We calculated reference values for arterial blood gases at different altitudes in Mexico assuming that sea level PaCO2 is 40 Torr, and in Mexico City (2.24 km. above the sea level) is 31.13 Torr, average of reported reference values. With the previous two points, it is possible to calculate a linear regression: PaCO2 = 40-3.96(altitude in km.). The equation is very similar to that calculated from reports in alveolar gas in North-Americans (Fitzgerald < 5 km): PACO2 = 39.3-3.11(altitude in km), and from subjects acclimatized to acute altitude exposure (< 5 km): PACO2 = 38.3-2.5 (altitude in km). It is also similar to a alinear equation that can be calculated assuming that hyperventilation in permanent habitants of moderate altitudes is inversely proportional to inspired molar concentration of O2: PaCO2 = PIO2/3.74. On the other hand, the equation is very different than that obtained from Andean natives (Hurtado): PaCO2 = 40.4-1.35(altitude in km). The proposed linear equation for Mexico gives very similar results (< 2 Torr difference) than a complex curvilinear equation by Morris et al. appropriate only up to 2.3 km. Evidence from acute exposure to altitude (acclimatized) and in North-Americans (alveolar gas) supports a reasonably accurate linear relationship up to 4 km. and also that the increase in ventilation in response to moderate altitudes in adult permanent residents is inversely proportional to molar concentration of O2. PAO2 was calculated with alveolar gas equation and resting the P(A-a)O2 we obtained PaO2. In conclusion, according to reference values in Mexico City, PaCO2 decreases about 4 Torr per km of altitude above the sea level. The decrease is similar to that reported in North-Americans and in acute exposure to altitude (acclimatized), but much less than that reported in native Peruvians. Ventilation is inversely proportional to the molar concentration of O2 at least up to an altitude where SaO2 is at or above 90%.