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  1. No Access

    Article

    Increased glacial-age ventilation of the Chilean margin by Antarctic Intermediate Water

    Antarctic Intermediate Water is an oxygen-rich water mass that spreads throughout the Southern Hemisphere oceans. Marine sediment chemistry indicates that the water mass was produced at higher rates and had hi...

    J. M. Muratli, Z. Chase, A. C. Mix, J. McManus in Nature Geoscience (2010)

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    Chapter

    Climate Feedback and Pleistocene Variations in the Atlantic South Equatorial Current

    Ice-age cooling of the central equatorial Atlantic Ocean reflects both equatorial upwelling and advection of cool water off the southern-hemisphere eastern boundary, but the largest contribution appears to be ...

    A. C. Mix, A. E. Morey in The South Atlantic (1996)