Tropical atmosphere-ocean system are demonstrated with CGCMĪ slow vacillation of jetstram/stormtrack location and strength is Impacts of high-level clouds and marine boundary layer stratus on SST dipole off the coast of the California through surface heat flux. Įvidence is presented that ENSO in the tropics can force a anomaly (TIWs) and their coupling with the atmosphere.
Seasonal and interannual variations of Tropical Instability Waves īoth CGCM simulations and satellite observations are used to study the Pacific Decadal Oscillation (PDO) is believed to contribute to theĭecadal changes in ENSO activity. Mechanism of IOZM and its relationship with ENSO are studied. With and without ENSO events in the Pacific. We are able to simulate the Indian Ocean zonal mode (IOZM) in CGCM integrations Our investigations focus on how the mutual influences of ENSO andĪsian Monsoon are established and how the Indian Ocean might affect Variability with reasonable frequency and amplitude. Yu is one of the models able to produce ENSO-like climate GCM has been developed under a joint project between UC and Los AlamosĮNSO Simulation, Dynamics, and Prediction Ī New Global Parallel and Coupled Ocean-Atmosphere GCMĪ new global, high-resolution, and parallel coupled atmosphere-ocean Patterns, evolution, teleconnections, and generation mechanisms. The CP and EP El Nino/La Nina have different There are two types of El Nino/La Nina: an eastern-Pacific (EP) type and aĬentral-Pacific (CP) type. Two Types of El Nino: Central-Pacific El Nino and Eastern-Pacific El Nino SST Animations for CP and EP El Nino EventsĪnimations of SST anomalies are displayed and contratsed for Eastern-Pacific (EP) type andĬentral-Pacific (CP) type of El Nino and La Nina events.
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