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  • Vector product
    ...s is zero or the two are parallel. When '''A''' and '''B''' are written in terms of their components along the ''x'', ''y'', and ''z'' axes of the [[rectan
    2 KB (236 words) - 15:24, 20 February 2012
  • Triple scalar product
    ...'''k''', '''B''' = ''b''<sub>1</sub>'''i''' + ''b''<sub>2</sub>'''j''' + ''b''<sub>3</sub>'''k''', and '''C''' = ''c''<sub>1</sub>'''i''' + ''c''<sub>2<
    1 KB (170 words) - 17:08, 25 April 2012
  • Linear
    ...a'' sin ''x'' + ''b'' cos ''y'' is linear in the coefficients ''a'' and ''b'', but [[nonlinear]] in ''x'' and ''y''.</div><br/> </div>
    524 bytes (71 words) - 17:26, 26 January 2012
  • Perturbation technique
    ...Graw-Hill Pub. Co., . 256 pp. </div><br/> <div class="reference">Stull, R. B. 1988. An Introduction to Boundary Layer Meteorology. 666 pp. </div><br/>
    2 KB (241 words) - 16:35, 25 April 2012
  • Closure assumptions
    ...arameterization]] rules.</div><br/> </div><div class="reference">Stull, R. B. 1988. An Introduction to Boundary Layer Meteorology. 666 pp. </div><br/>
    1 KB (140 words) - 15:37, 25 April 2012
  • Velocity defect law
    ...R. A. 1974. Analytical Methods in PBL Modelling. Halsted Press, appendix B, . 148 pp. </div><br/>
    639 bytes (89 words) - 15:24, 20 February 2012
  • Intensity-modulated indicator
    ...ually show the position of a [[target]] in terms of spatial coordinates. [[B-scopes]], [[PPI]] scopes, and [[RHI]] scopes are intensity modulated. <br/
    719 bytes (93 words) - 17:19, 26 January 2012
  • Einstein's summation notation
    ...ternating unit tensor]].</div><br/> </div><div class="reference">Stull, R. B. 1988. An Introduction to Boundary Layer Meteorology. 57&ndash;63. </div><b
    1,004 bytes (139 words) - 16:56, 26 January 2012
  • Isallobaric wind
    ...wind is unsatisfactory.</div><br/></div><div class="reference">Haurwitz, B. 1941. Dynamic Meteorology. 155&ndash;159. </div><br/>
    1 KB (187 words) - 16:15, 25 April 2012
  • Receiver (noise) temperature
    ..."paragraph">It is given in terms of the power output ''P'' and bandwidth ''B'' of the receiver by ''T''<sub>''r''</sub> = ''P''/''kB'', where ''k'' den
    1 KB (165 words) - 16:45, 25 April 2012
  • Van der waal's equation
    ...perfect gases. When ''p'' is small and &#x003b1; is large, the correction terms are small and the two equations become identical.</div><br/> </div>
    1 KB (182 words) - 17:11, 25 April 2012
  • Linearized differential equation
    ...ver hills and mountains.</div><br/> </div><div class="reference">Haurwitz, B. 1951. Compendium of Meteorology. 401&ndash;420. </div><br/> <div class="r
    1 KB (177 words) - 17:26, 26 January 2012
  • Bora
    ...ategory or the other. <br/>''See'' [[Boreas]], [[borasca]].<br/> Smith, R. B. 1987. Aerial observations of the Yugoslavian bora. J. Atmos. Sci.. 44. 269
    3 KB (477 words) - 22:16, 13 January 2024
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