Abstract

The audience for this paper includes researchers, educators, and engineers in the fields of air conditioning, atmospheric physics, meteorology, psychrometrics, standards, and thermodynamics. This paper provides a brief history of the molar mass of dry air, Mda, followed by the composition of Earth's atmosphere for the year 2008 and the calculation of Mda. A single equation is given to calculate Mda based on the actual abundance of CO2 in the atmosphere, which is currently increasing at an annual rate of 1.9 ìmol·mol−1. This causes an increase in the value of Mda at a rate of 0.0001 kg·kmol−1 (lb·lbmol−1) for every 8.33 ìmol·mol−1 increase in the abundance of CO2. It is practical for many calculations to use the average projected Mda value over a period of a half-century, during which time the value of Mda will increase by approximately 0.0010 kg·kmol−1 (lb·lbmol−1). For most psychrometric calculations, the authors recommend an Mda value of 28.966 kg·kmol−1 (lb·lbmol−1), which is projected for the year 2036. This value will be correct when rounded to three decimal places through 2058 if CO2 increases at its current rate.

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