Orbital forcing and its importance in understanding the warm Pliocene
The Pliocene is traditionally viewed as an epoch with a warm and stable climate. Data-Model comparisons for the mid-Pliocene (~3.3 – 3 Ma) have identified regions where models do not agree with geological proxies. Palaeoenvironmental syntheses used in these comparisons are time-averaged. It has been...
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University of Leeds
2017
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Online Access: | http://ethos.bl.uk/OrderDetails.do?uin=uk.bl.ethos.736480 |