Momentum transfer and surface pressure

Main Article Content

C. K. Stidd

Abstract

The mechanism by which the exchange of momentum, UV, in the atmosphere leads to surface pressure changes is explained and demonstrated. The mechanism is shown to govern the meridional profile of mean sea-level-pressure and the strenght of the Hadley and Ferrel cells. Implications with respect to ocean circulations and the Ekman drift equation are discussed.

Article Details

How to Cite
Stidd, C. K. (1974). Momentum transfer and surface pressure. Geofisica Internacional, 14(3), 207–221. https://doi.org/10.22201/igeof.00167169p.1974.14.3.996
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References

CRAIG, R. A., 1960. Meteorology in Fundamental Formulas of Physics, D. A. Menzel (Ed.) V. 2, Dover Pubs., Inc., NY, p. 702.

GREEN, J. S. A., 1970. Transfer properties of the large-scale eddies and the general circulation of the atmosphere. Quart. four. Royal Meteor. Soc., 96 : 157-185. DOI: https://doi.org/10.1002/qj.49709640802

HELLERMAN, S., 1967. An updated estimate of the wind stress on the world ocean, Monthly Weather Review, 95 (9): 607-611, with corrected tables from vol. 96 (1) : 63-74. DOI: https://doi.org/10.1175/1520-0493(1967)095<0607:AUEOTW>2.3.CO;2

JEFFREYS, H., 1919. On traveling atmospheric disturbances, Phil. Mag., 6 ser., 37 : 1-8. DOI: https://doi.org/10.1080/14786440108635861

JEFFREYS, H., 1926. On the dynamics of geostrophic winds, Quart. four, Royal Meteor. Soc., 52 : 85-101. DOI: https://doi.org/10.1002/qj.49705221708

JEFFREYS, H., 1933. The function of cyclones in the general circulation, reprinted in Theory of Thermal Convection, Dover, 1962, pp. 200-211.

NEWTON, C. W., 1971. Global Angular Momentum Balance: Earth Torques and Atmospheric Fluxes. J. Atmos. Sci., 38 : 1329-1341. DOI: https://doi.org/10.1175/1520-0469(1971)028<1329:GAMBET>2.0.CO;2

OORT, A. H. and E. M. RASMUSSON, 1971. Atmospheric Circulation Statistics, NOAA Prof. Pap. 5, Supt. Doc., Washington, D. C. 323 pp.

PRIESTLY, C. H. B., 1951. A survey of the stress between the ocean and atmosphere, Australian J. Sci. Res., A4 : 315-328. DOI: https://doi.org/10.1071/CH9510315

PALMEN, E. and M. A. ALAKA, 1952. On the budget of angular momentum in the zone between equator and 30 N. Tellus, 4 : 324-331. DOI: https://doi.org/10.1111/j.2153-3490.1952.tb01020.x

STARR, V. P., 1968. Physics of Negative Viscosity Phenomena, McGraw Hill, New York, 256 pp.

STARR, V. P., An essay on the general circulation of the earth's atmosphere, Jour. Meteor., 5 : 39-43, 1948. DOI: https://doi.org/10.1175/1520-0469(1948)005<0039:AEOTGC>2.0.CO;2

STARR, V., J. P. PEIXOTO and J. E. SIMS, 1970. A method for the study of the zonal kinetic energy balance in the atmosphere. Pure and Appl. Geophys. 80 : 346-358. DOI: https://doi.org/10.1007/BF00880219

SVERDRUP, H. U., 1947. Wind-driven currents in a baroclinic ocean; with application to the equatorial currents of the Eastern Pacific. Proc. N.A.S., 33 : 318-326. DOI: https://doi.org/10.1073/pnas.33.11.318

TUCKER, G. 8., 1960. The atmospheric budget of angular momentum, Tellus, 12 : 134-144. DOI: https://doi.org/10.1111/j.2153-3490.1960.tb01291.x

WHITE, R. M., 1949. The role of mountains in the regular momentum balance of the atmosphere. Jour. Meteor. 6 : 353-355. DOI: https://doi.org/10.1175/1520-0469(1949)006<0353:TROMIT>2.0.CO;2

WIDGER, W. K., 1949. A study of the flow of angular momentum in the atmosphere. Jour. Meteor. 6 : 291-299. DOI: https://doi.org/10.1175/1520-0469(1949)006<0292:ASOTFO>2.0.CO;2