Article · Wikipedia archive · Last revised May 31, 2026

Clebsch representation

In physics and mathematics, the Clebsch representation of an arbitrary three-dimensional vector field is:

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In physics and mathematics, the Clebsch representation of an arbitrary three-dimensional vector field v ( x ) {\displaystyle {\boldsymbol {v}}({\boldsymbol {x}})} is:12

v = φ + ψ χ , {\displaystyle {\boldsymbol {v}}={\boldsymbol {\nabla }}\varphi +\psi \,{\boldsymbol {\nabla }}\chi ,}

where the scalar fields φ ( x ) {\displaystyle \varphi ({\boldsymbol {x}})} , ψ ( x ) {\displaystyle ,\psi ({\boldsymbol {x}})} and χ ( x ) {\displaystyle \chi ({\boldsymbol {x}})} are known as Clebsch potentials3 or Monge potentials,4 named after Alfred Clebsch (1833–1872) and Gaspard Monge (1746–1818), and {\displaystyle {\boldsymbol {\nabla }}} is the gradient operator.

Background

In fluid dynamics and plasma physics, the Clebsch representation provides a means to overcome the difficulties to describe an inviscid flow with non-zero vorticity – in the Eulerian reference frame – using Lagrangian mechanics and Hamiltonian mechanics.567 At the critical point of such functionals the result is the Euler equations, a set of equations describing the fluid flow. Note that the mentioned difficulties do not arise when describing the flow through a variational principle in the Lagrangian reference frame. In case of surface gravity waves, the Clebsch representation leads to a rotational-flow form of Luke's variational principle.8

For the Clebsch representation to be possible, the vector field v {\displaystyle {\boldsymbol {v}}} has (locally) to be bounded, continuous and sufficiently smooth. For global applicability v {\displaystyle {\boldsymbol {v}}} has to decay fast enough towards infinity.9 The Clebsch decomposition is not unique, and (two) additional constraints are necessary to uniquely define the Clebsch potentials.1 Since ψ χ {\displaystyle \psi {\boldsymbol {\nabla }}\chi } is in general not solenoidal, the Clebsch representation does not in general satisfy the Helmholtz decomposition.10

Vorticity

The vorticity ω ( x ) {\displaystyle {\boldsymbol {\omega }}({\boldsymbol {x}})} is equal to2

ω = × v = × ( φ + ψ χ ) = ψ × χ , {\displaystyle {\boldsymbol {\omega }}={\boldsymbol {\nabla }}\times {\boldsymbol {v}}={\boldsymbol {\nabla }}\times \left({\boldsymbol {\nabla }}\varphi +\psi \,{\boldsymbol {\nabla }}\chi \right)={\boldsymbol {\nabla }}\psi \times {\boldsymbol {\nabla }}\chi ,}

with the last step due to the vector calculus identity × ( ψ A ) = ψ ( × A ) + ψ × A . {\displaystyle {\boldsymbol {\nabla }}\times (\psi {\boldsymbol {A}})=\psi ({\boldsymbol {\nabla }}\times {\boldsymbol {A}})+{\boldsymbol {\nabla }}\psi \times {\boldsymbol {A}}.} So the vorticity ω {\displaystyle {\boldsymbol {\omega }}} is perpendicular to both ψ {\displaystyle {\boldsymbol {\nabla }}\psi } and χ , {\displaystyle {\boldsymbol {\nabla }}\chi ,} while further the vorticity does not depend on φ . {\displaystyle \varphi .}

Notes

Notes

References

References