On the Slow Mode of a Simple Air-sea Coupled Model
Author:
Affiliation:
1. International Pacific Research Center, SOEST, University of Hawaii at Manoa
Publisher
Meteorological Society of Japan
Subject
Atmospheric Science
Link
https://www.jstage.jst.go.jp/article/jmsj1965/78/2/78_2_159/_pdf
Reference21 articles.
1. An, S. -I., F. -F. Jin and I. -S. Kang, 1999: The role of zonal advection feedback in phase transition and growth of ENSO in the Cane-Zebiak model. J. Meteor. Soc. Japan, 77, 1151-1160.
2. Anderson, D. L. T. and J. P. McCreary, 1985: Slowly propagating disturbances in a coupled ocean-atmosphere model. J. Atmos. Sci., 42, 615-629.
3. Battisti, D. S. and A. C. Hirst, 1989: Interannual variability in the tropical atmosphere/ocean system: Influence of the basic state and ocean geometry. J. Atmos. Sci., 46, 1687-1712
4. Chen, D., M. A. Cane, S. E. Zebiak and A. Kaplan, 1998: The impact of sea level data assimilation on the Lamont model prediction of the 1997/98 El Niño. Geophys. Res. Lett., 25, 2837-2840.
5. Hirst, A. C., 1986: Unstable and damped equatorial modes in simple coupled ocean-atmosphere models. J. Atmos. Sci., 43, 606-630.
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