Pliocene-Pleistocene evolution of sea surface and intermediate water temperatures from the Southwest Pacific
Over the last 5 million years, the global climate system has evolved toward a colder mean state, marked by large amplitude oscillations in continental ice volume. Equatorward expansion of polar waters and strengthening temperature gradients have been detected. However, the response of the mid- and h...
| Main Authors: | , , , , , |
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| Format: | Article |
| Published: |
Wiley-Blackwell
2016
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| Subjects: | |
| Online Access: | https://eprints.nottingham.ac.uk/33998/ |