Autobarotropy: Difference between revisions

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|Meaning=The state of a fluid that is characterized by both [[barotropy]] and [[piezotropy]], that  is, [[pressure]] and [[density]] surfaces coincide.
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|Explanation=This condition guarantees that the fluid will remain [[barotropic]] at all future times. Example:  an ideal homentropic fluid (i.e., a fluid with homogeneous [[potential temperature]]) with uniform  composition.<br/> Gill, A. E. 1982. Atmosphere&ndash;Ocean Dynamics. Academic Press, . p. 228.  
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== autobarotropy ==
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<div class="definition"><div class="short_definition">The state of a fluid that is characterized by both [[barotropy]] and [[piezotropy]], that  is, [[pressure]] and [[density]] surfaces coincide.</div><br/> <div class="paragraph">This condition guarantees that the fluid will remain [[barotropic]] at all future times. Example:  an ideal homentropic fluid (i.e., a fluid with homogeneous [[potential temperature]]) with uniform  composition.</div><br/> </div><div class="reference">Gill, A. E. 1982. Atmosphere&ndash;Ocean Dynamics. Academic Press, . p. 228. </div><br/>
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Latest revision as of 21:48, 13 January 2024

The state of a fluid that is characterized by both barotropy and piezotropy, that is, pressure and density surfaces coincide.

This condition guarantees that the fluid will remain barotropic at all future times. Example: an ideal homentropic fluid (i.e., a fluid with homogeneous potential temperature) with uniform composition.
Gill, A. E. 1982. Atmosphere–Ocean Dynamics. Academic Press, . p. 228.


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