In a system of differential equations used to describe a time-dependent process, a forcing function is a function that appears in the equations and is only a function of time, and not of any of the other variables. In effect, it is a constant for each value of t.
In the more general case, any nonhomogeneous source function in any variable can be described as a forcing function, and the resulting solution can often be determined using a superposition of linear combinations of the homogeneous solutions and the forcing term.
For example, f ( t ) {\displaystyle f(t)} is the forcing function in the nonhomogeneous, second-order, ordinary differential equation: a y ″ + b y ′ + c y = f ( t ) {\displaystyle ay''+by'+cy=f(t)}
References
"How do Forcing Functions Work?". University of Washington Departments. Archived from the original on September 20, 2003. https://web.archive.org/web/20030920030857/http://depts.washington.edu/rfpk/training/tutorials/modeling/part8/10.html ↩
Packard A. (Spring 2005). "ME 132" (PDF). University of California, Berkeley. p. 55. Archived from the original (PDF) on September 21, 2017. https://web.archive.org/web/20170921193859/http://jagger.berkeley.edu/~pack/me132/Section7.pdf ↩
Haberman, Richard (1983). Elementary Applied Partial Differential Equations. Prentice-Hall. p. 272. ISBN 0-13-252833-9. 0-13-252833-9 ↩