Phase-Locking of El Niño and La Niña Events in CMIP6 Models
El Niño–Southern Oscillation (ENSO) usually peaks in the boreal winter—November to January of the following year. This particular feature of ENSO is known as the seasonal phase locking of ENSO. In this study, based on 34 climate models from the Coupled Model Intercomparison Project Phase 6 (CMIP6),...
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| Médium: | Artigo |
| Jazyk: | Inglês |
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MDPI AG
2024-07-01
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| Edice: | Atmosphere |
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| On-line přístup: | https://www.mdpi.com/2073-4433/15/8/882 |
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