Effects of a three-dimensional mean flow on intraseasonal Kelvin waves in the equatorial Pacific Ocean

Author:

Johnson Eric S.,McPhaden Michael J.

Publisher

American Geophysical Union (AGU)

Subject

Paleontology,Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Atmospheric Science,Earth-Surface Processes,Geochemistry and Petrology,Soil Science,Water Science and Technology,Ecology,Aquatic Science,Forestry,Oceanography,Geophysics

Reference15 articles.

1. Estimating vertical velocity on the equator;Brady;Oceanol. Acta, Special Vol.,1987

2. Geostrophic comparisons from moored measurements of current and temperature during the Mid-Ocean Dynamics Experiment;Bryden;Deep Sea Res.,1977

3. Diagnostic model of the three-dimensional circulation in the upper equatorial Pacific;Bryden;J. Phys. Oceanogr.,1985

4. The intraseasonal oscillation in eastern Pacific sea levels: how is it forced?;Enfield;J. Phys. Oceanogr.,1987

5. Equatorial wind, current, and temperature data: 108W to 140W; April 1983 to October 1987;Freitag,1991

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