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  • Freshening of the Adélie Land Bottom Water near 140°E

    • Shigeru Aoki
      Institute of Low Temperature Science Hokkaido University Sapporo Japan
    • Stephen R. Rintoul
      CSIRO Marine Research Hobart, Tasmania Australia
    • Shuki Ushio
      National Institute of Polar Research Tokyo Japan
    • Shuichi Watanabe
      Japan Agency of Marine‐Earth Science and Technology Yokosuka Japan
    • Nathaniel L. Bindoff
      Institute of Antarctic and Southern Ocean Studies University of Tasmania, and CSIRO Marine Research Hobart, Tasmania Australia

    書誌事項

    公開日
    2005-12
    権利情報
    • http://onlinelibrary.wiley.com/termsAndConditions#vor
    DOI
    • 10.1029/2005gl024246
    公開者
    American Geophysical Union (AGU)

    この論文をさがす

    説明

    <jats:p>Repeat summer hydrographic observations along 140°E are used to document significant changes in the properties of the Adélie Land Bottom Water (ALBW) between the mid‐1990s and 2002–2003. Water on the 28.35 kg·m<jats:sup>−3</jats:sup> neutral density surface cooled by 0.2°C and freshened by 0.03 psu between 1994 and 2002. By re‐occupying the same stations in the same season, the effects of seasonal variability and spatial variability were minimised allowing the signal of water mass changes to be clearly identified. Comparison of the recent data to high quality historical observations shows that the ALBW also freshened between the late 1960s and the mid‐1990s. Although there is insufficient data to construct a continuous time series, the simplest explanation of the observed changes is that there has been a long‐term (>30 year) and continuing freshening of the source waters supplying bottom water to the Australian‐Antarctic basin.</jats:p>

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