A disk warp is a radial change of the orbital plane of successive disk annuli. In the small-tilt approximation, a complex tilt records its magnitude and azimuth. Pressure and internal torques communicate the tilt through bending waves of a Keplerian disk in the inviscid thin-disk regime. A flat tilted disk has constant even though its absolute orientation differs from the reference equatorial plane.
Here is the complex internal horizontal torque, the vertically integrated pressure, and the approximate nodal precession and apsidal precession rates. In the exactly Keplerian case, local plane waves obey , so tilt disturbances propagate at . The secular thin-disk approximation requires wavelengths large relative to the height while the local approximation requires them small relative to the orbital radius.
For , , constant disk aspect ratio , and , the inviscid steady disk warp equation reduces to in the displayed coordinate. The vanishing inner torque gives ; the outer tilt gives . The displayed solution holds when . If , it is , with an aligned node at and opposite signed inner tilt. For negative spin the corresponding equation is hyperbolic, giving with .

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