Sentence examples for outer rotation from inspiring English sources

For the case of hydrodynamic spherical Couette flow, generally three limits can be distinguished (see Fig. 5): the case of outer stationary (the limit |Ro|→∞) and the case of rapid outer rotation with either the inner sphere sub-rotating (Ro →−0) or with it super-rotating (Ro →+0).

The system can be characterized by the difference in inner and outer rotation rates Δ Ω and, if the outer sphere is rotating, by the overall system rotation Ω (i.e., the outer sphere rotation rate).

Starting with weak fields, the introduction of magnetic fields generally modifies the Stewartson layer (in the case of rapid overall rotation) or the equatorial jet (in the case of outer stationary or slow outer rotation); as the applied field gets stronger, it can eventually dominate rotational effects, with field lines structuring the flow.

With outer rotation, the critical Pm was reduced by a factor of two (indicating overall rotation is more favorable for dynamo action), and for intermediate values of rotation (E=10−3), a favorable window for dynamo action was found, with a critical Rm of 300.

Two other patients had relevant outer rotation deficits.

Additionally, the outer rotation deficit and operative complications were analysed.

The rotation axis of the inner rotator is supported by the two blue stands on the outer rotator.

The study varied both outer sphere rotation (i.e., E) and the amount of differential rotation (i.e., Ro) over a wide range.

Driven by diverging inner and outer cone rotation speeds, collagen fibrils from bovine skin were extruded and precipitated onto mandrels as tubes with oriented fibers and bundles, as examined by second harmonic generation microscopy and quantitative image analysis.

Finally, when a belt collides with an obstacle in the foreland oblique to the shortening direction the outer front displays rotations opposite in sign to oroclinal-type rotations, whereas the internal fronts seem to assume an "oroclinal type" rotational pattern.

Mobile low-latitude flux patches are seen in numerical dynamos without boundary heterogeneity when a strong enough influence of rotation on outer core convection is present (Wicht et al. 2011).