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Inclination Change Delta V⚠ unverified

Aerospace / Orbital · Compute the delta-v required for an orbital plane change

Parameters

InputSymbolUnitDefaultDescription
vvm/s1.0Orbital speed at the manoeuvre point
ii1.0Inclination change angle, in degrees
OutputSymbolUnitDescription
resultdvm/sDelta-v required for the plane change, in metres per second (m/s)

The science & history

Understanding the Parameters

Derivation (Approaching a Proof)

A pure plane change rotates the velocity vector through the angle $i$ while preserving its length. This is a problem of vector subtraction: the required $\Delta v$ is the difference between the new velocity $\mathbf{v}_2$ and the old $\mathbf{v}_1$, both of magnitude $v$, with an angle $i$ between them.

By the law of cosines on the isoceles triangle formed by $\mathbf{v}_1$, $\mathbf{v}_2$, and $\Delta\mathbf{v}$:

$$|\Delta v|^2 = v^2 + v^2 - 2\,v\,v\cos i = 2v^2(1 - \cos i).$$

Use the half-angle identity $1 - \cos i = 2\sin^2(i/2)$:

$$|\Delta v|^2 = 2v^2\cdot 2\sin^2\!\left(\frac{i}{2}\right) = 4v^2\sin^2\!\left(\frac{i}{2}\right).$$

Take the square root:

$$\Delta v = 2\,v\,\sin\!\left(\frac{i}{2}\right). \qquad\blacksquare$$

Geometrically, this is the base of an isoceles triangle with two equal sides $v$ and apex angle $i$ — the chord subtended, which is exactly $2v\sin(i/2)$. The factor of 2 and the half-angle are the signature of this rotate-a-fixed-length-vector geometry, the same form as the phasing and rendezvous velocity triangles.

Dimensional check. $2v\sin(i/2)$: $\sin(i/2)$ is dimensionless (with $i$ in radians after conversion), so $\Delta v$ carries the m/s of $v$ ✓.

History and Development

Related Concepts: Hohmann Transfer Dv1, Hohmann Transfer Dv2, Orbital Velocity, Vis Viva Energy, Delta V Rendezvous, Nodal Precession, Circular Orbit Velocity

Notes: Pure plane change — rotates velocity by $i$ at constant magnitude, so it adds no energy (same $a$, period). Cost $\propto v$ → very expensive ($30^\circ$ in LEO ≈ 3985 m/s; $60^\circ$ ≈ full $v$). Do it where $v$ is least (apogee), or combine with an altitude burn. Must be applied at a node. $i$ in degrees (mislabelled dimensionless).

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