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- ... northward, and vertically upward directions, respectively. The first two terms compose the [[horizontal advection]] and the last term is the [[vertical a2 KB (249 words) - 00:22, 27 January 2012
- ... streamlines diverge asymptotically. A pure shearing deformation field (''u'' = ''a''′<sub>0</sub>''y'', ''v'' = ''a''′<sub>0</sub>''x'') i2 KB (266 words) - 22:02, 20 February 2012
- ...]] of the vector [[equations of motion|equation of motion]]. When the two terms in the divergence are neglected, this equation becomes the [[balance equati1 KB (159 words) - 23:49, 25 April 2012
- ...l temperature]], ''T''<sub>''v''</sub> is the [[virtual temperature]], (''U'', ''V'') are the horizontal Cartesian [[wind]] components from the west an2 KB (232 words) - 23:59, 25 April 2012
- ...(ADTIC) Research Studies Institute 1955. Glossary of Arctic and Subarctic Terms. ADTIC Pub. A-105, Maxwell AFB, AL, . 90 pp. </div><br/>1 KB (201 words) - 22:16, 20 February 2012
- ...''y'' in terms of a parameter ''u'': ''x'' = ''g''(''u''); ''y'' = ''G''(''u''). The parameter may or may not have a useful geometric or physical inter704 B (98 words) - 01:39, 27 January 2012
- ....gif|link=|ams2001glos-Pex02]]</div>). The remaining [[nonlinear]] terms (terms that have products of two or more perturbation quantities, such as <div cl2 KB (241 words) - 00:35, 26 April 2012
- ...ts terms involving the [[vertical velocity]] ''w'', neglects the Coriolis terms proportional to the cosine of the latitude, and makes selective use of ''r2 KB (322 words) - 22:53, 20 February 2012
- ...average. The ratio of the buoyant to the negative of the shear production terms is also known as the [[flux Richardson number]] and is a measure of [[dynam2 KB (212 words) - 00:52, 26 April 2012
- ...ure due to vertical motion through the level ''h''. In general, these two terms balance one another so that the pressure tendency is obtained as a small d2 KB (350 words) - 01:04, 26 April 2012
- ...ition vector of a given point in space and ''t'' is time, the velocity, '''u''', is given by <div class="display-formula"><blockquote>[[File:ams2001gl690 B (96 words) - 02:17, 27 January 2012
- ...mponent of the [[relative vorticity]]; ''f'' the [[Coriolis parameter]]; ''u'', ''v'', and ''w'' the components of the [[wind]] velocity toward the eas3 KB (400 words) - 01:13, 26 April 2012