A linear stochastic dynamical model of ENSO. Part I: Model development

Journal of Climate

Volumn 13, Issue 15, 2000, Pages 2818-2832

  Thompson, C J ^a   Battisti, D S ^a  

^a UNIVERSITY OF WASHINGTON   (United States)

Author keywords

[No Author keywords available]

Indexed keywords

COMPUTER SIMULATION; RANDOM PROCESSES; VECTORS; WATER WAVES;

EL NINO SOUTHERN OSCILLATION; LINEAR STOCHASTIC DYNAMICAL MODEL;

CLIMATOLOGY;

ATMOSPHERE-OCEAN COUPLING; ATMOSPHERIC MODELING; EL NINO-SOUTHERN OSCILLATION; STOCHASTIC PROCESS;

EID: 0034253095     PISSN: 08948755     EISSN: None     Source Type: Journal    
DOI: 10.1175/1520-0442(2000)013<2818:ALSDMO>2.0.CO;2     Document Type: Article

References (34)

1. ENSO and ENSO-related predictability. Part I: Prediction of equatorial Pacific sea surface temperature with a hybrid coupled ocean-atmosphere model
2. The dynamics and thermodynamics of a warming event in a coupled tropical atmosphere-ocean model
3. Interannual variability in the tropical atmosphere-ocean system: Influence of the basic state, ocean geometry, and nonlinearity
4. The El Nino stochastic oscillator
5. Chaotic dynamic versus stochastic processes in ENSO in coupled ocean-atmosphere models
6. A study of the predictability of tropical Pacific SST in a coupled atmosphere-ocean model using singular vector analysis: The role of the annual cycle and the ENSO cycle
7. On the reflection and transmission of low-frequency energy at the irregular western Pacific Ocean boundary
8. Effects of low-latitude western boundary gaps on the reflection of equatorial motions
9. Predictability of a stochastically forced hybrid coupled model of El Nino
10. Optimal excitation of pertubations in viscous shear flow
11. Optimal excitation of neutral Rossby waves
12. Stochastically induced climate shift of El Nino-Southern Oscillation
13. Some simple solutions for heat-induced tropical circulation
14. Slow instabilities in tropical ocean basin-global atmosphere models
15. El Nino on the devil's staircase: Annual subharmonic steps to chaos
16. On the dependence of hindcast skill on ocean thermodynamics in a coupled ocean-atmosphere model
17. On the role of sea surface temperature gradients in forcing low-level winds and convergence in the tropics
18. Evidence for the delayed oscillator mechanism for ENSO: The 'observed' oceanic Kelvin mode in the western Pacific
19. Stochastic forcing of ENSO by the intraseasonal oscillation
20. Singular vectors, metrics, and adaptive observations
21. The optimal growth of tropical sea surface temperature anomalies
22. Dissipation in a Pacific equatorial long wave model
23. Variations in tropical sea surface temperatures and surface wind fields associated with the Southern Oscillation and El Nino
24. Initial conditions for optimal growth in a coupled ocean-atmosphere model of ENSO
25. A linear, stochastic, dynamical model of El Nino/Southern Oscillation
26. El Nino chaos: Overlapping of resonances between the seasonal cycle and the Pacific ocean-atmosphere oscillator
27. Stochastic dynamics of El Nino-Southern Oscillation
28. Predictability of a coupled model of ENSO using singular vector analysis. Part I: Optimal growth in seasonal background and ENSO cycles
29. Predictability of a coupled model of ENSO using singular vector analysis. Part II: Optimal growth and forecast skill
30. Tropical atmospheric-ocean interaction and the El Nino/Southern Oscillation phenomenon
31. Atmospheric convergence feedback in a simple model for El Nino
32. A model ENSO