| description abstract | he presence of the latitudinal variation of the Coriolis parameter serves as a mechanical barrier that causes a mass convergence for the poleward geostrophic flow and divergence for the equatorward flow, just as a sloped bottom terrain does to a crossover flow. Part of the mass convergence causes pressure to rise along the uphill pathway, while the remaining part is detoured to cross isobars out of the pathway. This mechanically excited cross-isobar flow, being unbalanced geostrophically, is subject to a ?half-cycle? Coriolis force that only turns it to the direction parallel to isobars without continuing to turn it farther back to its opposite direction because the geostrophic balance is reestablished once the flow becomes parallel to isobars. Such oscillation, involving a barrier-induced mass convergence, a mechanical deflection, and a half-cycle Coriolis deflection, is referred to as a mechanical?Coriolis oscillation with a ?barrier-induced half-cycle Coriolis force? as its restoring force. Through a complete cycle of the mechanical?Coriolis oscillation, a new geostrophically balanced flow pattern emerges to the left of the existing flow when facing the uphill (downhill) direction of the barrier in the Northern (Southern) Hemisphere. The ? barrier is always sloped toward the pole in both hemispheres, responsible for the westward propagation of Rossby waves. The ?-induced mechanical?Coriolis oscillation frequency can be succinctly expressed as , where , and ? is the angle of a sloped surface along which the unbalanced flow crosses isobars, α is the angle of isobars with the barrier?s slope, and k is the wavenumber along the direction of the barrier?s contours. | |
