Abstract
El Niño events are characterized by surface warming of the tropical Pacific Ocean and weakening of equatorial trade winds that occur every few years. Such conditions are accompanied by changes in atmospheric and oceanic circulation, affecting global climate, marine and terrestrial ecosystems, fisheries and human activities. The alternation of warm El Niño and cold La Niña conditions, referred to as the El Niño–Southern Oscillation (ENSO), represents the strongest year-to-year fluctuation of the global climate system. Here we provide a synopsis of our current understanding of the spatio-temporal complexity of this important climate mode and its influence on the Earth system.
| Original language | English |
|---|---|
| Pages (from-to) | 535-545 |
| Number of pages | 11 |
| Journal | Nature |
| Volume | 559 |
| Issue number | 7715 |
| DOIs | |
| Publication status | Published - 26 Jul 2018 |
UN SDGs
This output contributes to the following UN Sustainable Development Goals (SDGs)
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SDG 13 Climate Action
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SDG 14 Life Below Water
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SDG 15 Life on Land
Keywords
- El Nino-Southern Oscillation
- westerly wind
- El Nino
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