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North Atlantic weather regimes in δ18O of winter precipitation: isotopic fingerprint of the response in the atmospheric circulation after volcanic eruptions
Equatorial volcanic eruptions are known to impact the atmospheric circulation on seasonal time scales through a strengthening of the stratospheric zonal winds followed by dynamic ocean-atmosphere coupling. This emerges as the positive phase of the North Atlantic Oscillation in the first 5 years afte...
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| Main Authors: | , , , , |
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| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado em: |
Stockholm University Press
2019-01-01
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| Colecção: | Tellus: Series B, Chemical and Physical Meteorology |
| Assuntos: | |
| Acesso em linha: | http://dx.doi.org/10.1080/16000889.2019.1633848 |
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