Sentence examples for a second velocity from inspiring English sources

From the end of this velocity vector a second velocity vector was drawn in the direction toward which the wind was blowing, its length being proportional to the wind speed.

Since after 60 s of continued constant angular velocity (90°/s) rotation, there is no longer any vestibular activation (i.e. there is no VOR response and subjects feel that they are no longer turning), a second velocity step can be obtained by rapidly stopping the subject (from 90°/s to 0°/s over 0.5 s).

Because phase shifts can arise from other factors (e.g., field inhomogeneity), a second velocity-compensated phase image is acquired and subtraction yields the actual phase relationship of the protons [ 14].

Phase 1 consists of an initial velocity peak, decreasing transiently to 0 at the end of phase 1 before a second angular velocity peak of opposite sign associated with phase 2, again decreasing to 0 at the completion of this phase (Domenici and Blake, 1997; Tytell et al., 2008).

Thisflow characteristics around the NACA 65-410 series airfoils are calculated and comethodons are made wish results available in the literature.

The second velocity (v2).

The effects of a second order velocity-slip and temperature-jump on basic gaseous fluctuating micro-flows were analyzed by Hamdan et al. [19].

Moreover, they located the foci of low-frequency earthquakes (deep low-frequency earthquakes, DLFEs) that cluster just below the sill-like deformation source; finally they inferred the existence of a second low-velocity zone extends in and around the caldera at a depth of 15 23 km.

In this work, a combined discontinuous Galerkin (DG) method, which is a hybridized mixed discontinuous Galerkin (HMDG) method combined with the direct discontinuous Galerkin (DDG) method, is proposed to compute ground states and dynamics of dipolar Bose Einstein condensates (BECs) described by a multi-dimensional Gross Pitaevskii equation (GPE) coupled with a first-order velocity system.

For anisotropy measurements a second direction for velocity measurements preferably perpendicular to the axial direction is necessary.

A fourth-order velocity-stress finite difference method is used to perform numerical simulations of S-wave testing in earth models with lateral variation.