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<a accesskey="3" href="page.php?w=Baroclinity&amp;p=2">3.Next</a>
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<p><a href="page.php?w=Image%3ABaroclinic_Fluid_Diagram.svg">thumb</a><a href="page.php?w=Image%3ABarokline_Atmosph%C3%A4re.svg">thumb</a>In <a href="page.php?w=fluid_dynamics">fluid dynamics</a>, the <b>baroclinity</b> (often called <b>baroclinicity</b>) of a stratified fluid is a measure of how misaligned the gradient of pressure is from the gradient of density in a fluid. In <a href="page.php?w=meteorology">meteorology</a>, a baroclinic flow is one in which the density depends on both  temperature and pressure (the fully general case). A simpler</p><p>
<a accesskey="3" href="page.php?w=Baroclinity&amp;p=2">3.Next</a>
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