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		<summary type="html">&lt;p&gt;Rescuing 1 sources and tagging 0 as dead.) #IABot (v2.0.9.5) (&lt;a href=&quot;/wiki143/index.php?title=User:%D0%9B%D0%B8%D1%81%D0%B0%D0%BD_%D0%B0%D0%BB%D1%8C-%D0%93%D0%B0%D0%B8%D0%B1&amp;amp;action=edit&amp;amp;redlink=1&quot; class=&quot;new&quot; title=&quot;User:Лисан аль-Гаиб (page does not exist)&quot;&gt;Лисан аль-Гаиб&lt;/a&gt; - 17315&lt;/p&gt;
&lt;p&gt;&lt;b&gt;New page&lt;/b&gt;&lt;/p&gt;&lt;div&gt;{{Short description|Eigenfunctions of Laplace&amp;#039;s tidal equations which govern fluid motion on a rotating sphere}}&lt;br /&gt;
In [[applied mathematics]], the &amp;#039;&amp;#039;&amp;#039;Hough functions&amp;#039;&amp;#039;&amp;#039; are the [[eigenfunctions]] of [[Primitive equations|Laplace&amp;#039;s tidal equations]] which govern [[secondary circulation|fluid motion on a rotating sphere]]. As such, they are relevant in [[geophysics]] and [[meteorology]] where they form part of the solutions for [[tide|atmospheric and ocean waves]]. These functions are named in honour of [[Sydney Samuel Hough]].&amp;lt;ref&amp;gt;{{cite book|author=Cartwright, David Edgar|title=Tides: A Scientific History|year=2000|publisher=Cambridge University Press|pages=[https://archive.org/details/tidesscientifich0000cart/page/85 85]–87|isbn=9780521621458 |url=https://archive.org/details/tidesscientifich0000cart|url-access=registration}}&amp;lt;/ref&amp;gt;&amp;lt;ref&amp;gt;Hough, S. S. (1897). [https://babel.hathitrust.org/cgi/pt?id=coo.31924060893561;view=1up;seq=259 On the Application of Harmonic Analysis to the Dynamical Theory of the Tides. Part I. On Laplace&amp;#039;s&amp;#039; Oscillations of the First Species, and on the Dynamics of Ocean Currents]. Proceedings of the Royal Society of London, vol. 61, 201–257.&amp;lt;/ref&amp;gt;&amp;lt;ref&amp;gt;Hough, S. S. (1898). [https://babel.hathitrust.org/cgi/pt?id=coo.31924060893355;view=1up;seq=203 On the application of harmonic analysis to the dynamical theory of the tides. Part II. On the general integration of Laplace&amp;#039;s dynamical equations]. Philosophical Transactions of the Royal Society of London. Series A, Containing Papers of a Mathematical or Physical Character, vol. 191, 139–185.&amp;lt;/ref&amp;gt;&lt;br /&gt;
&lt;br /&gt;
Each Hough mode is a function of [[latitude]] and may be expressed as an infinite sum of [[associated Legendre polynomials]]; the functions are [[orthogonal]] over the sphere in the continuous case. Thus they can also be thought of as a [[generalized Fourier series]] in which the [[basis function]]s are the [[normal mode]]s of an atmosphere at rest.&lt;br /&gt;
&lt;br /&gt;
==See also==&lt;br /&gt;
*[[Secondary circulation]]&lt;br /&gt;
*[[Legendre polynomials]]&lt;br /&gt;
*[[Primitive equations]]&lt;br /&gt;
&lt;br /&gt;
==References==&lt;br /&gt;
{{reflist}}&lt;br /&gt;
&lt;br /&gt;
== Further reading ==&lt;br /&gt;
&lt;br /&gt;
* {{cite journal&lt;br /&gt;
|author=Lindzen, R.S.&lt;br /&gt;
|year=2003&lt;br /&gt;
|title=The Interaction of Waves and Convection in the Tropics&lt;br /&gt;
|journal=Journal of the Atmospheric Sciences&lt;br /&gt;
|volume=60&lt;br /&gt;
|issue=24&lt;br /&gt;
|pages=3009–3020&lt;br /&gt;
|url=http://eaps.mit.edu/faculty/lindzen/Waves_and_Convection031.pdf&lt;br /&gt;
|bibcode=2003JAtS...60.3009L&lt;br /&gt;
|doi=10.1175/1520-0469(2003)060&amp;lt;3009:TIOWAC&amp;gt;2.0.CO;2&lt;br /&gt;
|access-date=2009-03-22&lt;br /&gt;
|archive-date=2010-06-13&lt;br /&gt;
|archive-url=https://web.archive.org/web/20100613123012/http://eaps.mit.edu/faculty/lindzen/Waves_and_Convection031.pdf&lt;br /&gt;
|url-status=dead&lt;br /&gt;
}}&lt;br /&gt;
&lt;br /&gt;
[[Category:Atmospheric dynamics]]&lt;br /&gt;
[[Category:Physical oceanography]]&lt;br /&gt;
[[Category:Fluid mechanics]]&lt;br /&gt;
[[Category:Special functions]]&lt;/div&gt;</summary>
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