The effect of low ancient greenhouse climate temperature gradients on the ocean's overturning circulation

We examine whether the reduced meridional temperature gradients of past greenhouse climates might have reduced oceanic overturning, leading to a more quiescent subsurface ocean. A substantial reduction of the pole-to-Equator temperature difference is achieved in a coupled climate model via an altere...

Full description

Bibliographic Details
Main Authors: W. P. Sijp, M. H. England
Format: Article
Language:English
Published: Copernicus Publications 2016-02-01
Series:Climate of the Past
Online Access:http://www.clim-past.net/12/543/2016/cp-12-543-2016.pdf