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  1. Article

    Open Access

    Antarctic ice sheet discharge driven by atmosphere-ocean feedbacks at the Last Glacial Termination

    Reconstructing the dynamic response of the Antarctic ice sheets to warming during the Last Glacial Termination (LGT; 18,000–11,650 yrs ago) allows us to disentangle ice-climate feedbacks that are key to improv...

    C. J. Fogwill, C. S. M. Turney, N. R. Golledge, D. M. Etheridge in Scientific Reports (2017)

  2. No Access

    Article

    Low atmospheric CO2 levels during the Little Ice Age due to cooling-induced terrestrial uptake

    Land carbon uptake reduced atmospheric CO2 levels during the Little Ice Age. Numerical simulations of atmospheric carbonyl sulfide levels and ice-core carbon isotope data reveal that temperature change, not land-...

    M. Rubino, D. M. Etheridge, C. M. Trudinger, C. E. Allison in Nature Geoscience (2016)

  3. No Access

    Article

    Trends and seasonal cycles in the isotopic composition of nitrous oxide since 1940

    The atmospheric nitrous oxide concentration has increased by 20% since 1750. Analyses of Antarctic firn and archived air samples reveal seasonal cycles in the isotopic signature of nitrous oxide, which can hel...

    S. Park, P. Croteau, K. A. Boering, D. M. Etheridge, D. Ferretti in Nature Geoscience (2012)

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    Article

    Strategic Planning of Information Communications Systems (SPICS)

    D M Etheridge, R Moreton in Journal of Information Technology (1987)