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Dynamics for El Niño-La Niña asymmetry constrain equatorial-Pacific warming pattern
The El Niño-Southern Oscillation (ENSO) results from the instability of and also modulates the strength of the tropical-Pacific cold tongue. While climate models reproduce observed ENSO amplitude relatively well, the majority still simulates its asymmetry between warm (El Niño) and cold (La Niña) ph...
| Autores principales: | , , |
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| Formato: | Online Artículo Texto |
| Lenguaje: | English |
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Nature Publishing Group UK
2020
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| Acceso en línea: | https://www.ncbi.nlm.nih.gov/pmc/articles/PMC7455730/ https://www.ncbi.nlm.nih.gov/pubmed/32859891 http://dx.doi.org/10.1038/s41467-020-17983-y |