Progress Article in 2013

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  • A 500,000-year-long period of warmth in the middle Eocene was marked by high atmospheric carbon dioxide concentrations and prolonged dissolution of carbonate in the deep oceans. Numerical simulations attempting to capture these features identify gaps in our understanding of the causes of this and similar perturbations.

    • Appy Sluijs
    • Richard E. Zeebe
    • Steven M. Bohaty
    Progress Article
  • Temperature change over the past 2,000 years has shown pronounced regional variability. An assessment of all available continental temperature reconstructions shows a clear twentieth century warming trend, but no evidence of a coherent Little Ice Age or Medieval Warm Period.

    • Moinuddin Ahmed
    • Kevin J. Anchukaitis
    • Eduardo Zorita
    Progress Article