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  • Coherent structures
    ...ree-dimensional structure of convection in the atmospheric surface layer. J. Atmos. Sci.. p. 2424. </div><br/>
    2 KB (200 words) - 15:39, 25 April 2012
  • Triple scalar product
    .../sub>'''k''', and '''C''' = ''c''<sub>1</sub>'''i''' + ''c''<sub>2</sub>'''j''' + ''c''<sub>3</sub>'''k''', the triple scalar product is the determinan
    1 KB (170 words) - 17:08, 25 April 2012
  • Bemporad's formula
    ...001glos-Be10.gif|link=|center|ams2001glos-Be10]]</blockquote><br/>List, R. J., ed. 1951. Smithsonian Meteorological Tables. 6th rev. ed., . p. 422.
    597 bytes (82 words) - 22:02, 13 January 2024
  • Intensity
    ...as an "intense [[low]]."</div><br/> </div><div class="reference">Palmer, J. M. 1993. Metrologia. 30. 371&ndash;372. </div><br/>
    1 KB (138 words) - 14:29, 20 February 2012
  • Advective model
    |Meaning=A numerical forecast model based on discrete [[advection]] terms only, with less or no emphasis on forcing, [[dissipation]], and physics. ...del is the divergent [[anomaly]] vorticity [[advection]] model.<br/> Qin, J., and H. M. van den Dool 1996. Simple extensions of an NWP model. Mon. Wea.
    783 bytes (108 words) - 21:00, 13 January 2024
  • Vector
    ...ely; for example, '''A''' = ''a''<sub>1</sub>'''i''' + ''a''<sub>2</sub>'''j''' + ''a''<sub>3</sub>'''k'''. A vector drawn from a fixed origin to a giv
    2 KB (240 words) - 17:11, 25 April 2012
  • Einstein's summation notation
    ...erms. The key to this notation is the use of indices (subscripts) ''i'', ''j'', and ''k'', which can each take on the values of 1, 2, or 3 to represent
    1,004 bytes (139 words) - 16:56, 26 January 2012
  • Divergence equation
    ...]] of the vector [[equations of motion|equation of motion]]. When the two terms in the divergence are neglected, this equation becomes the [[balance equati
    1 KB (159 words) - 15:49, 25 April 2012
  • Omega equation
    ...of the '''Q''' [[vector]].</div><br/> </div><div class="reference">Holton, J. R. 1992. An Introduction to Dynamic Meteorology. 3d edition, Academic Pres
    1 KB (168 words) - 16:32, 25 April 2012
  • Receiver (noise) temperature
    ...where ''k'' denotes [[Boltzmann's constant]], 1.38 &times; 10<sup>-23</sup>J K<sup>-1</sup>. The receiver temperature is related to the receiver noise
    1 KB (165 words) - 16:45, 25 April 2012
  • Deformation
    ...sis]] and [[frontolysis]].</div><br/> </div><div class="reference">Holton, J. R. 1992. An Introduction to Dynamic Meteorology. 3d edition, Academic Pres
    2 KB (266 words) - 14:02, 20 February 2012
  • Viscous fluid
    ...length scales]].</div><br/> </div><div class="reference">Tennekes, H., and J. L. Lumley 1972. A First Course in Turbulence. MIT Press, . 256&ndash;262.
    2 KB (363 words) - 17:12, 25 April 2012
  • Vorticity equation
    ...s-Ve23]]</blockquote></div></div><br/></div><div class="reference">Holton, J. R. 1992. An Introduction to Dynamic Meteorology. 3d edition, Academic Pre
    3 KB (400 words) - 17:13, 25 April 2012
  • Bora
    ...ca]].<br/> Smith, R. B. 1987. Aerial observations of the Yugoslavian bora. J. Atmos. Sci.. 44. 269&ndash;297. <br/> Defant, F. 1951. Compendium of Meteo
    3 KB (477 words) - 22:16, 13 January 2024
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