0.0013g -- For dry air at STP which is 0C (273.15K) and 1 bar (100 kilopascals or 1 atmosphere))
Improved:
Air Weights can very at different temperatures and sea levels.
With different temperatures or pressure, the density of air is:
d = p/(R x T)
d is the calculated density of air (g/cm^3)
p is the pressure (kp or kilopascals)
R is the specific gas constant -- 287.05 Joules/(kg*K)
T is the Temperature (K or Kelvin)
With different altitudes and any water vapor (humidity), the weight of air varies in a much more complex fashion.
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