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<div class="definition"><div class="short_definition">Measures of the thermodynamic state of the air, similar to [[potential temperature]].</div><br/> <div class="paragraph">For example, the [[dry static energy]] (also known as the [[Montgomery streamfunction]]) is  <div class="display-formula"><blockquote>[[File:ams2001glos-Se58.gif|link=|center|ams2001glos-Se58]]</blockquote></div> where ''g'' is [[acceleration of gravity]], ''z'' is height above some reference level (often taken as the height  where the [[pressure]] is 100 kPa), ''C''<sub>''p''</sub> is [[specific heat]] at constant pressure, and ''T'' is [[absolute]]  temperature. Typical atmospheric values are on the order of 300 kJ kg<sup>&minus;1</sup>. Compare this [[static  energy]] to one definition for [[potential temperature]], <div class="display-formula"><blockquote>[[File:ams2001glos-Se59.gif|link=|center|ams2001glos-Se59]]</blockquote></div><br/>''See'' [[moist static energy]], [[liquid water static energy]], [[saturation static energy]].</div><br/> </div>
<div class="definition"><div class="short_definition">Measures of the thermodynamic state of the air, similar to [[potential temperature]].</div><br/> <div class="paragraph">For example, the [[dry static energy]] (also known as the [[Montgomery streamfunction]]) is  <div class="display-formula"><blockquote>[[File:ams2001glos-Se58.gif|link=|center|ams2001glos-Se58]]</blockquote></div> where ''g'' is [[acceleration of gravity]], ''z'' is height above some reference level (often taken as the height  where the [[pressure]] is 100 kPa), ''C''<sub>''p''</sub> is [[specific heat]] at constant pressure, and ''T'' is [[absolute]]  temperature. Typical atmospheric values are on the order of 300 kJ kg<sup>-1</sup>. Compare this [[static energy|static  energy]] to one definition for [[potential temperature]], <div class="display-formula"><blockquote>[[File:ams2001glos-Se59.gif|link=|center|ams2001glos-Se59]]</blockquote></div><br/>''See'' [[moist static energy]], [[liquid water static energy]], [[saturation static energy]].</div><br/> </div>
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Latest revision as of 16:58, 25 April 2012



static energies

Measures of the thermodynamic state of the air, similar to potential temperature.

For example, the dry static energy (also known as the Montgomery streamfunction) is
ams2001glos-Se58
where g is acceleration of gravity, z is height above some reference level (often taken as the height where the pressure is 100 kPa), Cp is specific heat at constant pressure, and T is absolute temperature. Typical atmospheric values are on the order of 300 kJ kg-1. Compare this static energy to one definition for potential temperature,
ams2001glos-Se59

See moist static energy, liquid water static energy, saturation static energy.


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