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searching for Forcing function (differential equations) 8 found (11 total)

alternate case: forcing function (differential equations)

Lyapunov stability (3,887 words) [view diff] no match in snippet view article find links to article

Various types of stability may be discussed for the solutions of differential equations or difference equations describing dynamical systems. The most important

Harmonic oscillator (4,562 words) [view diff] no match in snippet view article find links to article

[citation needed] This is done through nondimensionalization. If the forcing function is f(t) = cos(ωt) = cos(ωtcτ) = cos(ωτ), where ω = ωtc, the equation

Transfer function (2,498 words) [view diff] no match in snippet view article find links to article

ISBN 978-0-7506-6988-7. Birkhoff, Garrett; Rota, Gian-Carlo (1978). Ordinary differential equations. New York: John Wiley & Sons. ISBN 978-0-471-05224-1.[page needed]

Method of moments (electromagnetics) (4,006 words) [view diff] no match in snippet view article

application and sought variables, different integral or integro-differential equations are used in MoM. Radiation and scattering by thin wire structures

Stokes number (2,388 words) [view diff] no match in snippet view article find links to article

how a tracking delay arises could be drawn by simply defining the differential equations of a particle in the Stokes regime. A particle moving with the fluid

Vibration (7,227 words) [view diff] no match in snippet view article find links to article

t}} is a mathematical trick used to solve linear differential equations. Using Euler's formula and taking only the real part of the solution

Fourier optics (12,531 words) [view diff] no match in snippet view article find links to article

of differential equations, as in the case of matrix equations, whenever the right-hand side of an equation is zero (For example, a forcing function, forcing

Tide (13,077 words) [view diff] no match in snippet view article find links to article

the evening. Pierre-Simon Laplace formulated a system of partial differential equations relating the ocean's horizontal flow to its surface height, the