Dynamic-height anomaly: Difference between revisions

Latest revision as of 14:06, 20 February 2012

dynamic-height anomaly[edit | edit source]

(Also called anomaly of geopotential differences.) In oceanography, the excess of the actual geopotential difference, between two given isobaric surfaces, over the geopotential difference in a homogeneous water column of salinity of 35 psu and temperature 0°C.

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-<div class="definition"><div class="short_definition">(<br/>''Also called'' anomaly of geopotential differences.) In [[oceanography]], the  excess of the actual [[geopotential]] difference, between two given [[isobaric surfaces]], over the geopotential  difference in a homogeneous water column of [[salinity]] of 35 psu and [[temperature]] 0&deg;C.</div><br/> </div>
+<div class="definition"><div class="short_definition">(''Also called'' anomaly of geopotential differences.) In [[oceanography]], the  excess of the actual [[geopotential]] difference, between two given [[isobaric surfaces]], over the geopotential  difference in a homogeneous water column of [[salinity]] of 35 psu and [[temperature]] 0&#x000b0;C.</div><br/> </div>
 </div>