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  • Chi-square test
    ...f'' - ''h'')<sup>2</sup>/''h'' where ''f'' is an observed frequency and ''h'' its hypothetical value.</div><br/> </div>
    903 bytes (120 words) - 13:49, 20 February 2012
  • Semi-implicit method
    ...tively higher frequencies or more rapid time changes in ''f'' than does ''h''. <br/>''See'' [[implicit time difference]].</div><br/> </div>
    1,022 bytes (139 words) - 15:05, 20 February 2012
  • Omega equation
    ...agraph">The right-hand side of the omega equation can also be expressed in terms of the [[divergence]] of the '''Q''' [[vector]].</div><br/> </div><div cla
    1 KB (168 words) - 16:32, 25 April 2012
  • Tendency equation
    ...dency and the advection.</div><br/> </div><div class="reference">Panofsky, H. 1956. Introduction to Dynamic Meteorology. 124&ndash;130. </div><br/>
    2 KB (350 words) - 17:04, 25 April 2012
  • Advective model
    |Meaning=A numerical forecast model based on discrete [[advection]] terms only, with less or no emphasis on forcing, [[dissipation]], and physics. ...he divergent [[anomaly]] vorticity [[advection]] model.<br/> Qin, J., and H. M. van den Dool 1996. Simple extensions of an NWP model. Mon. Wea. Rev.. 1
    783 bytes (108 words) - 21:00, 13 January 2024
  • Clo
    ...ts) of about 0.51 cm.</div><br/> </div><div class="reference">Newburgh, L. H., ed. 1949. Physiology of Heat Regulation and the Science of Clothing. pp.
    1 KB (243 words) - 13:52, 20 February 2012
  • Isallobaric wind
    ...eostrophic wind]], &#x003b1; the [[specific volume]], '''&nabla;'''<sub>''H''</sub> the horizontal [[del operator]], and ''p'' the [[pressure]]. The is
    1 KB (187 words) - 16:15, 25 April 2012
  • Thermal wind
    ...the thermal wind '''v'''<sub>''T''</sub> in terms of the [[thickness]] ''h'' of the layer: <div class="display-formula"><blockquote>[[File:ams2001glo
    1 KB (194 words) - 17:05, 25 April 2012
  • Linearized differential equation
    ...Meteorology. 401&ndash;420. </div><br/> <div class="reference">Panofsky, H. 1954. Introduction to Dynamic Meteorology. ch. 4. </div><br/>
    1 KB (177 words) - 17:26, 26 January 2012
  • Balance equation
    ...hic equilibrium]] to which it reduces in the absence of the [[nonlinear]] terms. In the case of circular contours, this nonlinear correction is the same a
    1 KB (194 words) - 21:53, 13 January 2024
  • Kurtosis
    ...(''x'') = 1 (0 &lt; ''x'' &lt; 1) has ''&#x003b2;''<sub>2</sub> = 1.8. The terms [[leptokurtic]], [[mesokurtic]], and [[platykurtic]] refer to curves for w Westfall, P. H., 2014: Kurtosis as peakedness, 1905&ndash;2014. RIP. ''Amer. Stat.'', '''6
    2 KB (260 words) - 06:45, 15 March 2019
  • Viscous fluid
    ...bulence length scales]].</div><br/> </div><div class="reference">Tennekes, H., and J. L. Lumley 1972. A First Course in Turbulence. MIT Press, . 256&nda
    2 KB (363 words) - 17:12, 25 April 2012
  • Radar equation
    ...of the [[snow]] and ice particles in a unit volume. It may be expressed in terms of the [[drop-size distribution|drop-size distribution]] as <div class="d
    3 KB (437 words) - 16:42, 25 April 2012
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