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    Twentieth-Century Surface Temperature Trends in the Western Ross Sea, Antarctica: Evidence from a High-Resolution Ice Core 

    Source: Journal of Climate:;2012:;volume( 025 ):;issue: 010:;page 3629
    Author(s): Sinclair, Kate E.; Bertler, Nancy A. N.; van Ommen, Tas D.
    Publisher: American Meteorological Society
    Abstract: 125-yr ice core record of climate from the Whitehall Glacier ice divide provides exceptionally high-resolution stable isotope data from the northwest margin of the Ross Sea, Antarctica. This is the only proxy data available ...
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    A Millennial Proxy Record of ENSO and Eastern Australian Rainfall from the Law Dome Ice Core, East Antarctica 

    Source: Journal of Climate:;2012:;volume( 026 ):;issue: 003:;page 710
    Author(s): Vance, Tessa R.; van Ommen, Tas D.; Curran, Mark A. J.; Plummer, Chris T.; Moy, Andrew D.
    Publisher: American Meteorological Society
    Abstract: NSO causes climate extremes across and beyond the Pacific basin; however, evidence of ENSO at high southern latitudes is generally restricted to the South Pacific and West Antarctica. Here, the authors report a statistically ...
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    Paleoclimate Data–Model Comparison and the Role of Climate Forcings over the Past 1500 Years 

    Source: Journal of Climate:;2013:;volume( 026 ):;issue: 018:;page 6915
    Author(s): Phipps, Steven J.; McGregor, Helen V.; Gergis, Joëlle; Gallant, Ailie J. E.; Neukom, Raphael; Stevenson, Samantha; Ackerley, Duncan; Brown, Josephine R.; Fischer, Matt J.; van Ommen, Tas D.
    Publisher: American Meteorological Society
    Abstract: he past 1500 years provide a valuable opportunity to study the response of the climate system to external forcings. However, the integration of paleoclimate proxies with climate modeling is critical to improving the ...
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