- Hypsometric equation
The hypsometric equation relates the
atmospheric pressure ratio to the thickness of an atmospheric layer under the assumptions of constanttemperature andgravity . It is derived from thehydrostatic equation and theideal gas law .It is expressed as:
:
where:
: = thickness of the layer
[m] : =geopotential height [m] : =gas constant for dry air : =temperature inkelvin s[K] : =gravitational acceleration [m/s 2] : =pressure [Pa] In
meteorology and areisobaric surfaces and T is the average temperature of the layer between them. Inaltimetry with theInternational Standard Atmosphere the hypsometric equation is used to compute pressure at a givengeopotential height inisothermal layers in the upper and lowerstratosphere .Derivation
The hydrostatic equation:
:
where is the
density [kg/m 3] , is used to generate the equation forhydrostatic equilibrium , written in differential form::
This is combined with the
ideal gas law ::
to eliminate :
:
This is integrated from to :
:
Integration gives:
:
simplifying to:
:
Rearranging:
:
or, eliminating the logarithm:
:
References
* [http://amsglossary.allenpress.com/glossary/search?id=hypsometric-equation1 AMS Glossary of Meteorology]
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