The effect of mountain uplift on eastern boundary currents and upwelling systems
<p>All major mountain ranges are assumed to have been subject to increased uplifting processes during the late Miocene and Pliocene. Previous work has demonstrated that African uplift is an important element to explain Benguela upper-ocean cooling in the late Miocene–Pliocene. According to pro...
| Main Authors: | , |
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| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2020-01-01
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| Series: | Climate of the Past |
| Online Access: | https://www.clim-past.net/16/161/2020/cp-16-161-2020.pdf |