Changes to the tropical circulation in the mid-Pliocene and their implications for future climate
The two components of the tropical overturning circulation, the meridional Hadley circulation (HC) and the zonal Walker circulation (WC), are key to the re-distribution of moisture, heat and mass in the atmosphere. The mid-Pliocene Warm Period (mPWP; ∼ 3.3–3 Ma) is considered a very rough analogue o...
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| Hlavní autoři: | , |
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| Médium: | Artigo |
| Jazyk: | Inglês |
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Copernicus Publications
2017-02-01
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| Edice: | Climate of the Past |
| Témata: | |
| On-line přístup: | http://www.clim-past.net/13/135/2017/cp-13-135-2017.pdf |
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