Unraveling the mystery of recent shortened response time of ENSO to Atlantic forcing
Abstract The El Niño-Southern Oscillation (ENSO) is known to respond to tropical Atlantic (TA) sea surface temperature (SST) forcing. However, the response time of ENSO to the TA SST forcing is not stationary but varies over decades, the reasons for which remain poorly understood. Here we show that...
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| Hlavní autoři: | , , , , , , |
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| Médium: | Artigo |
| Jazyk: | Inglês |
| Vydáno: |
Nature Portfolio
2025-07-01
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| Edice: | Nature Communications |
| On-line přístup: | https://doi.org/10.1038/s41467-025-61130-4 |
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