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      Long eccentricity forcing Asian dust input into the northwestern Pacific during the early Pleistocene

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          Trends, rhythms, and aberrations in global climate 65 Ma to present.

          Since 65 million years ago (Ma), Earth's climate has undergone a significant and complex evolution, the finer details of which are now coming to light through investigations of deep-sea sediment cores. This evolution includes gradual trends of warming and cooling driven by tectonic processes on time scales of 10(5) to 10(7) years, rhythmic or periodic cycles driven by orbital processes with 10(4)- to 10(6)-year cyclicity, and rare rapid aberrant shifts and extreme climate transients with durations of 10(3) to 10(5) years. Here, recent progress in defining the evolution of global climate over the Cenozoic Era is reviewed. We focus primarily on the periodic and anomalous components of variability over the early portion of this era, as constrained by the latest generation of deep-sea isotope records. We also consider how this improved perspective has led to the recognition of previously unforeseen mechanisms for altering climate.
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            A Pliocene-Pleistocene stack of 57 globally distributed benthic δ18O records

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              Pacific–East Asian Teleconnection: How Does ENSO Affect East Asian Climate?

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                Author and article information

                Journal
                Palaeogeography, Palaeoclimatology, Palaeoecology
                Palaeogeography, Palaeoclimatology, Palaeoecology
                Elsevier BV
                00310182
                June 2022
                June 2022
                : 596
                : 110963
                Article
                10.1016/j.palaeo.2022.110963
                12179741-6a76-480e-89db-84d962a5030b
                © 2022

                https://www.elsevier.com/tdm/userlicense/1.0/

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