Transience, nonlinearity, and eddy feedback in the remote response to El Niño

Journal of the Atmospheric Sciences

Volumn 57, Issue 24, 2000, Pages 3992-4007

  Hall, N M J ^a   Derome, J ^a  

^a LEGI   (France)

Author keywords

[No Author keywords available]

Indexed keywords

AIR-SEA INTERACTION; ATMOSPHERIC FORCING; EDDY; EL NINO; HEAT SOURCE; NONLINEARITY; TRANSIENT FLOW;

PACIFIC OCEAN;

ATMOSPHERIC TEMPERATURE; COMPUTER SIMULATION; EARTH ATMOSPHERE; INTEGRATION; MATHEMATICAL MODELS; OCEANOGRAPHY; PERTURBATION TECHNIQUES;

DIRECT LINEAR RESPONSE; DRY PRIMITIVE EQUATION MODEL; EDDY FEEDBACK; EL NINO; EQUATORIAL HEATING; PACIFIC NORTH AMERICAN TYPE RESPONSE; REMOTE RESPONSE; TROPICAL HEAT SOURCE;

CLIMATOLOGY;

EID: 0034351752     PISSN: 00224928     EISSN: None     Source Type: Journal    
DOI: 10.1175/1520-0469(2001)058<3992:TNAEFI>2.0.CO;2     Document Type: Article

References (28)

1. Concerning the response of the atmosphere to a tropical sea surface temperature anomaly
2. Analysis of general circulation model sea-surface temperature anomaly simulations using a linear model. Forced solutions
3. Ensembles of AGCM two-tier predictions and simulations of the circulation anomalies during winter 1997-98
4. Some simple solutions for heat induced tropical circulation
5. Nonlinear response to anomalous tropical forcing
6. A simple GCM based on dry dynamics and constant forcing
7. Barotropic models of the extra-tropical response to El Niño
8. Transients and the extratropical response to El Niño
9. Organization of extratropical transients during El Niño
10. El Niño La Niña and the nonlinearity of their teleconnections
11. Planetary-scale atmospheric phenomena associated with the Southern Oscillation
12. A multi-layer spectral model and the semi-implicit method
13. The steady linear response of a spherical atmosphere to thermal and orographic forcing
14. The direct response to tropical heating in a baroclinic atmosphere
15. The diagnosis of mechanical dissipation in the atmosphere from large-scale balance requirements
16. Possible causes of anomalies in seasonal mean circulation patterns during the 1982-83 El Niño event
17. Changes in predictability associated with the PNA pattern
18. Toward a dynamical understanding of planetary-scale flow regimes
19. Quasigeostrophic motions in the equatorial area
20. A study of wintertime circulation anomalies during past El Niño events using a high-resolution general circulation model. I: Influence of model climatology
21. Predictability in the extended range
22. The generation of global rotational flow by steady idealized tropical divergence
23. The role of transient disturbances in the dynamics of the Pacific-North American pattern
24. The forcing of stationary wave motion by tropical diabatic heating
25. An energy and angular-momentum conserving vertical finite-difference scheme and hybrid vertical coordinates
26. The stationary wave response to a tropical SST anomaly in an idealized GCM
27. Factors determining the extratropical response to equatorial diabatic heating anomalies
28. Teleconnections in the geo-potential field during the Northern Hemisphere winter