Geophysical Fluid Dynamics Laboratory

1969 Citations

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1. Bryan, K., 1969: Climate and the ocean circulation climate and the ocean circulation III. The ocean model. Monthly Weather Review, 97(11), 806-827.
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2. Bryan, K., 1969. A numerical method for the study of the circulation of the World Ocean. Journal of Computational Physics, 4, 347-376.
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3. Manabe, S., 1969: Climate and the ocean circulation - 1. The atmospheric circulation and the hydrology of the earth's surface. Monthly Weather Review, 97(11), 739-774.
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4. Manabe, S., 1969: Climate and the ocean circulation - II. The atmospheric circulation and the effect of heat transfer by ocean currents. Monthly Weather Review, 97(11), 775-805.
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5. Manabe, S., and K. Bryan, 1969: Climate calculations with a combined ocean-atmosphere model. Journal of the Atmospheric Sciences, 26(4), 786-789.
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6. Miyakoda, K., J. Smagorinsky, R. F. Strickler, and G. D. Hembree, 1969: Experimental extended predictions with a nine-level hemispheric model. Monthly Weather Review, 97(1), 1-76.
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7. Oort, A. H., and A. Taylor, 1969: On the kinetic energy spectrum near the ground. Monthly Weather Review, 97(9), 623-636.
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8. Orlanski, I., 1969: The influence fo bottom topography on the stability of jets in a baroclinic fluid. Journal of the Atmospheric Sciences, 26, 1216-1232.
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9. Orlanski, I., and K. Bryan, 1969: Formation of the thermocline step structure by large-amplitude internal gravity waves. Journal of Geophysical Research, 74(28), 6975-6983.
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10. Smagorinsky, J., 1969: Numerical simulationof the global atmosphere. In The Global Circulation of the Atmosphere, London: Royal Meteorological Society, 24-41.
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11. Smagorinsky, J., 1969: Problems and promises of deterministic extended range forecasting. Bulletin of the American Meteorological Society, 50(5), 286-311.
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12. Williams, G. P., 1969: Numerical integration of the three-dimensional Navier-Stokes equations for incompressible flow. Journal of Fluid Mechanics, 37(4), 727-750.
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13. Yanai, M., and Y. Hayashi, 1969: Large-scale equatorial waves penetrating from the upper troposphere into the lower stratosphere. Journal of the Meteorological Society of Japan, 47(3),  167-182.
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