Source: http://en.wikipedia.org/wiki/Barometric_formula#Pressure_equations

The value of subscript b ranges from 0 to 6 in accordance with each of seven successive layers of the atmosphere shown in the table below. In these equations, g0, M and R* are each single-valued constants, while P, L, T, and h are multivalued constants in accordance with the table below. The values used for M, g0, and R* are in accordance with the U.S. Standard Atmosphere, 1976, and the value for R* in particular does not agree with standard values for this constant. The reference value for Pb for b = 0 is the defined sea level value, P0 = 101325 pascals or 29.92126 inHg. Values of Pb of b = 1 through b = 6 are obtained from the application of the appropriate member of the pair equations 1 and 2 for the case when h = hb+1.

 

Subscript bHeight above sea levelStatic pressureStd. temperature
(K)
Temperature lapse rate
(m)(ft)(pascals)(inHg)(K/m)(K/ft)
0 0 0 101325.00 29.92126 288.15 -0.0065 -0.0019812
1 11,000 36,089 22632.10 6.683245 216.65 0.0 0.0
2 20,000 65,617 5474.89 1.616734 216.65 0.001 0.0003048
3 32,000 104,987 868.02 0.2563258 228.65 0.0028 0.00085344
4 47,000 154,199 110.91 0.0327506 270.65 0.0 0.0
5 51,000 167,323 66.94 0.01976704 270.65 -0.0028 -0.00085344
6 71,000 232,940 3.96 0.00116833 214.65 -0.002 -0.0006096