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Air Density Formula

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Air Density Formula


name         Scott
status       student
grade        9-12
location     NY

Question -   Hi there,
Do you know a formula that I could use to calculate air density 
using the 3 inputs from the instruments I have:
Temperture in Celsius?
Rh - relative humidity?
Barometric pressure ( from my barometer in inches of Mercury)?

I would like to put the formula in my programmable calculator to 
track changes in daily Air density. I know you have to allow for 
saturation pressure and water vapour pressure but I'm not sure how 
to go about it.
----------------------------------------------------------------
There are a number of websites that treat the properties of the 
atmosphere. They vary in complexity, because the atmosphere is a 
dynamic mixture of gases that is not constant. Some of the 
treatments get rather involved because of the intended applications 
of engine design and aircraft behavior. The most direct source I 
found for your needs is: http://www.aeromech.usyd.edu.au/aero/atmos/atmos.html
It may require some "number crunching" on your part to write an 
algorithm for a programmable calculator but I do not think it is out of reach.

Vince Calder
====================================================================
Scott,

It requires some equations, but it can be done.

First we need to convert your pressure (P) into
kPa (kiloPascals):

P(kPa) = P(in. Hg)*3.3864

Next we need to determine the vapor pressure (VP)
in kPa. To do this we first calculate the saturation
vapor pressure (SVP) in kPa from the temperature (T):

SVP = 0.61121*e^[17.67*T/(T+243.5)],

where e means exponential.

Then we can calculate VP from RH and SVP:

VP = RH*SVP/100

Now we calculate the mixing ratio (XM):

XM = 0.622*VP/(P-VP)

Finally, we calculate moist air density (RHO):

RHO = [P*(1+XM)]/[0.28703*(T+273.16)*(1+1.16078*XM)],

where the T+273.16 puts the temperature into Kelvin
degrees.

So, if T=26 deg. C, P=29.23 in. Hg (99 kPa), and
RH=40%, we get SVP=3.3615 kPa, VP=1.345 kPa,
XM=0.008564, and RHO=1.1514 kg m^-3
(or 1.1514 x 10^-3 g cm^-3).


David R. Cook
Climate Research Section
Environmental Science Division
Argonne National Laboratory
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