Barry Saltzman (ed.)'s Advances in Geophysics, Vol. 31 PDF

By Barry Saltzman (ed.)

ISBN-10: 0120188317

ISBN-13: 9780120188314

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95, 241-261. Lilly. D. , and Zipser E. J. (1972). The Front Range windstorm of 11 January 1972-a meteorological narrative. Weatherwise 25(2), 56-63. Long, R. R. (1953). Some aspects of stratified fluids, I . A theoretical investigation. Tellus 5 , 32-58. Long, R . R. (1955). Some aspects of the flow of stratified fluids, 111. Continuous density gradients, Tellus 7 , 341-357. Long. R. R. (1970). Blocking effects in Row over obstacles. Tellus 22, 471-479. Long, R. R. (1972). Finite amplitude disturbances in the flow of inviscid rotating and stratified fluids over obstacles.

Academic Press, New York. Hoinka K. P. (1985). A comparison of numerical simulations of hydrostatic flow over mountains and observations. Mon. Weather Rev. 113, 719-735. Huppert, H. , and Miles J . W. (1969). Lee waves in a stratified flow Part 3, Semi-elliptical obstacles. J . Fluid Mech. 35, 481-496. Jusem. J. C . and Barcilon, A. (1981). Hydrostatic mountain waves produced by asymmetric ridges. Geophys. Astrophys. Fluid Dyn. 17, 3-14. Klemp, J. B.. and Lilly, D. K. (1975). The dynamics of wave induced downslope winds.

When b exceeds the half-width of the shear layer, then h > 1, and the breaking occurs below the shear layer. , far to the right in Fig. 12), the shear layer plays no role, and the discussion in Section 3 is fully applicable. The following points comprise a critique of local hydraulic theory as applied to the 2-D reversed shear problem: The theory uses an idealized configuration (Fig. 13) that is very close to the actual flow configuration (Durran and Klemp, 1987). It gives a solution curve f i ( h )that agrees well with numerical results and is entirely realizable because hydraulic flows exist even for low ridges (Bacmeister and Pierrehumbert, 1988).

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Advances in Geophysics, Vol. 31 by Barry Saltzman (ed.)


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