Reply to 'Pliocene warmth and gradients'

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Cool La Niña during the warmth of the Pliocene?

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Reply to "Comment on 'Dynamically maintained steady-state pressure gradients' "

A reply is made to Duncan's Comment [T. L. Duncan, Phys. Rev. E 61, 4661 (2000)] on my earlier paper [D. P. Sheehan, Phys. Rev. E 57, 6660 (1998)] in which he raises an apparent second-law paradox arising from dynamically maintained, steady-state pressure gradients. Resolutions to this paradox are considered in light of current theoretical and experimental understanding.

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ژورنال

عنوان ژورنال: Nature Geoscience

سال: 2015

ISSN: 1752-0894,1752-0908

DOI: 10.1038/ngeo2445