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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...
Tallennettuna:
| Päätekijät: | , , , , |
|---|---|
| Aineistotyyppi: | Artigo |
| Kieli: | Inglês |
| Julkaistu: |
Stockholm University Press
2019-01-01
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| Sarja: | Tellus: Series B, Chemical and Physical Meteorology |
| Aiheet: | |
| Linkit: | http://dx.doi.org/10.1080/16000889.2019.1633848 |
| Tagit: |
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