Taylor–Proudman theorem

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The Taylor–Proudman theorem is a fundamental result in geophysical fluid dynamics stating that in a rapidly rotating, inviscid, incompressible fluid, steady flows tend to be uniform along the axis of rotation, leading to columnar motion.

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Predicate Object
instanceOf result in fluid dynamics
result in geophysical fluid dynamics
theorem
appliesTo incompressible fluids
inviscid fluids
rapidly rotating fluids
steady flows
assumes Coriolis force dominates inertial forces
Rossby number is small NERFINISHED
incompressibility
negligible viscosity
steady flow conditions
category theorems in fluid mechanics
theorems in geophysics
concernsQuantity velocity field
conclusion flow is invariant in the direction of the rotation vector
velocity does not vary along the rotation axis
describes constraint imposed by rapid rotation on fluid motion
field geophysical fluid dynamics
rotating fluid dynamics
holdsWhen Ekman number is small away from boundary layers NERFINISHED
implies columnar motion aligned with the rotation axis
two-dimensionalization of flow in planes perpendicular to the rotation axis
influences interpretation of large-scale atmospheric flows
interpretation of large-scale oceanic flows
mathematicalForm Coriolis term balances pressure gradient in the momentum equations
derivative of velocity along rotation axis is approximately zero
namedAfter Geoffrey Ingram Taylor NERFINISHED
Joseph Proudman NERFINISHED
relatedTo Coriolis effect NERFINISHED
Proudman–Taylor columns NERFINISHED
Taylor columns NERFINISHED
geostrophic balance
quasi-geostrophic theory
statesThat steady flow in a rapidly rotating inviscid incompressible fluid is uniform along the axis of rotation
usedIn atmospheric dynamics
laboratory rotating tank experiments
ocean dynamics
planetary core dynamics

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G. I. Taylor knownFor Taylor–Proudman theorem