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dynamic-height anomaly |
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dynamic-height anomaly [dī¦nam·ik ¦hīt ə′näm·ə·lē] (oceanography) The excess of the actual geopotential difference, between two given isobaric surfaces, over the geopotential difference in a homogeneous water column of salinity 35 per mille and temperature 0°C. Also known as anomaly of geopotential difference. How to thank TFD for its existence? Tell a friend about us, add a link to this page, add the site to iGoogle, or visit webmaster's page for free fun content. |
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