For smooth radial variation on scale , , , and . The exact point-mass vertical gravity differs from by relative order . Radial pressure support changes the rotation and dominant shear heating by the same order. Meridional viscous forces, radial radiative-flux divergence, thermal advection and compressional work are at most order relative to their retained vertical terms for . These estimates require secular disk evolution and exclude sharp radial boundary layers or independently rapid vertical motion.

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