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applied mathematics Applied mathematics is the application of mathematical methods by different fields such as physics, engineering, medicine, biology, finance, business, computer science, and industry. Thus, applied mathematics is a combination of mathematical s ...
, the Hough functions are the eigenfunctions of
Laplace's tidal equations The theory of tides is the application of continuum mechanics to interpret and predict the tidal deformations of planetary and satellite bodies and their atmospheres and oceans (especially Earth's oceans) under the gravitational loading of anot ...
which govern fluid motion on a rotating sphere. As such, they are relevant in
geophysics Geophysics () is a subject of natural science concerned with the physical processes and physical properties of the Earth and its surrounding space environment, and the use of quantitative methods for their analysis. The term ''geophysics'' som ...
and
meteorology Meteorology is a branch of the atmospheric sciences (which include atmospheric chemistry and physics) with a major focus on weather forecasting. The study of meteorology dates back millennia, though significant progress in meteorology did not ...
where they form part of the solutions for atmospheric and ocean waves. These functions are named in honour of
Sydney Samuel Hough Sydney Samuel Hough Fellow of the Royal Society, FRS (11 June 1870, Stoke Newington – 8 July 1923, Gerrards Cross, Buckinghamshire) was a British applied mathematician and astronomer. Hough studied at Christ's Hospital and then obtained a schol ...
.Hough, S. S. (1898)
On the application of harmonic analysis to the dynamical theory of the tides. Part II. On the general integration of Laplace'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.
Each Hough mode is a function of
latitude In geography, latitude is a coordinate that specifies the north– south position of a point on the surface of the Earth or another celestial body. Latitude is given as an angle that ranges from –90° at the south pole to 90° at the north pol ...
and may be expressed as an infinite sum of
associated Legendre polynomials In mathematics, the associated Legendre polynomials are the canonical solutions of the general Legendre equation \left(1 - x^2\right) \frac P_\ell^m(x) - 2 x \frac P_\ell^m(x) + \left \ell (\ell + 1) - \frac \rightP_\ell^m(x) = 0, or equivalently ...
; the functions are
orthogonal In mathematics, orthogonality is the generalization of the geometric notion of ''perpendicularity''. By extension, orthogonality is also used to refer to the separation of specific features of a system. The term also has specialized meanings in ...
over the sphere in the continuous case. Thus they can also be thought of as a generalized Fourier series in which the
basis function In mathematics, a basis function is an element of a particular basis for a function space. Every function in the function space can be represented as a linear combination of basis functions, just as every vector in a vector space can be represen ...
s are the
normal mode A normal mode of a dynamical system is a pattern of motion in which all parts of the system move sinusoidally with the same frequency and with a fixed phase relation. The free motion described by the normal modes takes place at fixed frequencies. ...
s of an atmosphere at rest.


See also

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Secondary circulation In fluid dynamics, a secondary circulation or secondary flow is a weak circulation that plays a key maintenance role in sustaining a stronger primary circulation that contains most of the kinetic energy and momentum of a flow. For example, a tro ...
*
Legendre polynomials In physical science and mathematics, Legendre polynomials (named after Adrien-Marie Legendre, who discovered them in 1782) are a system of complete and orthogonal polynomials, with a vast number of mathematical properties, and numerous applicat ...
*
Primitive equations The primitive equations are a set of nonlinear partial differential equations that are used to approximate global atmospheric flow and are used in most atmospheric models. They consist of three main sets of balance equations: # A ''continuity equ ...


References


Further reading

* {{cite journal , author=Lindzen, R.S. , year=2003 , title=The Interaction of Waves and Convection in the Tropics , journal=Journal of the Atmospheric Sciences , volume=60 , issue=24 , pages=3009–3020 , url=http://eaps.mit.edu/faculty/lindzen/Waves_and_Convection031.pdf , bibcode = 2003JAtS...60.3009L , doi = 10.1175/1520-0469(2003)060<3009:TIOWAC>2.0.CO;2 Atmospheric dynamics Physical oceanography Fluid mechanics Special functions