The leading disturbance in sphere Stokes flow has size . Consequently viscous diffusion has size , background advection has size , and their ratio is . Even if the sphere Reynolds number is small, this ratio becomes order one at . Thus the Stokes approximation is nonuniform at distances of order . At that outer distance the disturbance itself is small relative to , so self-convection is smaller than background advection and the Oseen approximation is appropriate:
Write . It is sufficient outside the origin to impose and : these give zero divergence, and substitution into momentum gives . With , differentiation yields
A decaying radial choice is . Therefore
The exponent is nonpositive, so this scalar decays at infinity, including as directly downstream. In the overlap ,
Choosing cancels the first term's gradient in . The remaining leading velocity is
Matching fixes . Thus the potential-source and wake decomposition of sphere Oseen flow is
Its pressure is , the sign appropriate to a fixed sphere in an incident flow. The velocity decays in every direction and matches the requested leading inner disturbance; the sphere's potential-dipole term enters a higher matching order.
The scalar potential is a point source: , so integration over a centred sphere gives
To see the fluid wake, take downstream along and transverse radius . For , , giving
The fluid wake is concentrated within . Its integrated mass deficit is , balancing the outward potential-source mass flux. The corresponding momentum deficit is
which equals the leading sphere drag. The Gaussian integral used here is .
The PDF labels as the mass-source strength, but this has dimensions of force. The actual mass-source strength is ; is the momentum deficit or drag. The decomposition above supplies both quantities and identifies the printed normalization error.