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Barometric Tendency |
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barometric tendency [bar·ə′met·rik ′ten·dən·sē]
(meteorology) Barometric Tendency in meteorology, the magnitude and character of a change in atmospheric pressure at a certain location during the three hours preceding an observation. The barometric tendency is determined by the curve recorded on a barograph. Data concerning the barometric tendency are plotted on surface weather maps used for forecasting. 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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