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    Fifty-Year Trends in Global Ocean Salinities and Their Relationship to Broad-Scale Warming 

    Source: Journal of Climate:;2010:;volume( 023 ):;issue: 016:;page 4342
    Author(s): Durack, Paul J.; Wijffels, Susan E.
    Publisher: American Meteorological Society
    Abstract: Using over 1.6 million profiles of salinity, potential temperature, and neutral density from historical archives and the international Argo Program, this study develops the three-dimensional field of multidecadal linear ...
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    Moving beyond the Total Sea Ice Extent in Gauging Model Biases 

    Source: Journal of Climate:;2016:;volume( 029 ):;issue: 024:;page 8965
    Author(s): Ivanova, Detelina P.; Gleckler, Peter J.; Taylor, Karl E.; Durack, Paul J.; Marvel, Kate D.
    Publisher: American Meteorological Society
    Abstract: eproducing characteristics of observed sea ice extent remains an important climate modeling challenge. This study describes several approaches to improve how model biases in total sea ice distribution are quantified, and ...
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    Impacts of Broad-Scale Surface Freshening of the Southern Ocean in a Coupled Climate Model 

    Source: Journal of Climate:;2018:;volume 031:;issue 007:;page 2613
    Author(s): Purich, Ariaan; England, Matthew H.; Cai, Wenju; Sullivan, Arnold; Durack, Paul J.
    Publisher: American Meteorological Society
    Abstract: AbstractThe Southern Ocean surface has freshened in recent decades, increasing water column stability and reducing upwelling of warmer subsurface waters. The majority of CMIP5 models underestimate or fail to capture this ...
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    Climate Drift in the CMIP3 Models 

    Source: Journal of Climate:;2012:;volume( 025 ):;issue: 013:;page 4621
    Author(s): Gupta, Alexander Sen; Muir, Les C.; Brown, Jaclyn N.; Phipps, Steven J.; Durack, Paul J.; Monselesan, Didier; Wijffels, Susan E.
    Publisher: American Meteorological Society
    Abstract: ven in the absence of external forcing, climate models often exhibit long-term trends that cannot be attributed to natural variability. This so-called climate drift arises for various reasons including the following: ...
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    Competing Influences of Anthropogenic Warming, ENSO, and Plant Physiology on Future Terrestrial Aridity 

    Source: Journal of Climate:;2017:;volume( 030 ):;issue: 017:;page 6883
    Author(s): Bonfils, Céline;Anderson, Gemma;Santer, Benjamin D.;Phillips, Thomas J.;Taylor, Karl E.;Cuntz, Matthias;Zelinka, Mark D.;Marvel, Kate;Cook, Benjamin I.;Cvijanovic, Ivana;Durack, Paul J.
    Publisher: American Meteorological Society
    Abstract: AbstractThe 2011?16 California drought illustrates that drought-prone areas do not always experience relief once a favorable phase of El Niño?Southern Oscillation (ENSO) returns. In the twenty-first century, such an ...
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    Challenges in Quantifying Changes in the Global Water Cycle 

    Source: Bulletin of the American Meteorological Society:;2014:;volume( 096 ):;issue: 007:;page 1097
    Author(s): Hegerl, Gabriele C.; Black, Emily; Allan, Richard P.; Ingram, William J.; Polson, Debbie; Trenberth, Kevin E.; Chadwick, Robin S.; Arkin, Phillip A.; Sarojini, Beena Balan; Becker, Andreas; Dai, Aiguo; Durack, Paul J.; Easterling, David; Fowler, Hayley J.; Kendon, Elizabeth J.; Huffman, George J.; Liu, Chunlei; Marsh, Robert; New, Mark; Osborn, Timothy J.; Skliris, Nikolaos; Stott, Peter A.; Vidale, Pier-Luigi; Wijffels, Susan E.; Wilcox, Laura J.; Willett, Kate M.; Zhang, Xuebin
    Publisher: American Meteorological Society
    Abstract: nderstanding observed changes to the global water cycle is key to predicting future climate changes and their impacts. While many datasets document crucial variables such as precipitation, ocean salinity, runoff, and ...
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