A high resolution AGCM study of the El Niño impact on the North Atlantic/European sector

Geophysical Research Letters

Volumn 29, Issue 9, 2002, Pages 5-1-5-4

  Merkel, Ute ^a   Latif, Mojib ^a  

^a MAX PLANCK INSTITUTE FOR METEOROLOGY   (Germany)

Author keywords

[No Author keywords available]

Indexed keywords

ATMOSPHERIC PRESSURE; ATMOSPHERIC TEMPERATURE;

STATIONARY WAVE ACTIVITIES;

GEOPHYSICS;

CYCLONE; EL NINO-SOUTHERN OSCILLATION; GENERAL CIRCULATION MODEL; SEA SURFACE TEMPERATURE;

(NORTH); ATLANTIC OCEAN; EUROPE;

EID: 0036558552     PISSN: 00948276     EISSN: None     Source Type: Journal    
DOI: 10.1029/2001GL013726     Document Type: Article

References (21)

1. 1996: Climate predictability experiments with a general circulation model
2. Identification of cyclone-track regimes in the North Atlantic
3. Impact of horizontal resolution on seasonal integrations
4. High resolution climate simulation over Europe
5. Predictable winter climate in the North Atlantic sector during the 1997-1999 ENSO cycle
6. Impact of localized tropical and extratropical SSt anomalities in ensembles of seasonal GCM integrations
7. Climate anomalies in Europe associated with ENSO extremes
8. An ENSO impact on Europe?
9. Atmospheric response to sea surface temperature anomalies during El Niño 1997/98 as simulated by ECHAM4
10. A detailed examination of the extratropical response to tropical El Niño/Southern oscillation events
11. On the existence of storm-tracks
12. Decadal variations in climate associated with the North Atlantic Oscillation
13. Interpretation and implications of the observed Inter-El Niño variability
14. On the three-dimensional propagation of stationary waves
15. North Atlantic decadal regimes in a coupled GCM simulation
16. Improved global sea surface temperature analyses using optimal interpolation
17. Progress during TOGA in understanding and modelling global teleconnections associated with tropical sea surface temperatures
18. On the El Niño teleconnection to spring precipitation in Europe
19. On the role of barotropic energy conversions in the general circulation