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Isobaric Surfaces |
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Isobaric Surfaces
surfaces of equal air pressure in the atmosphere. The relative location of isobaric surfaces gives an idea of the spatial distribution of air pressure. In a cyclone (that is, an area of reduced pressure) an isobaric surface is a concave surface and in an anticyclone (that is, an area of increased pressure) it is convex. The slope of isobaric surfaces determines wind speed: the greater the slope of the isobaric surfaces, the greater the wind speed, all other conditions being equal. The intersection of isobaric surfaces with a horizontal plane (at sea level and other level surfaces) produces isobars. Want to thank TFD for its existence? Tell a friend about us, add a link to this page, add the site to iGoogle, or visit the webmaster's page for free fun content. |
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