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2425Volcanic Eruptions Impact Global Sea Level

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  • Pat Neuman
    Nov 6, 2005
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      Volcanic Eruptions Impact Global Sea Level

      Canberra, Australia (SPX) Nov 07, 2005
      Clouds of gases and particles sprayed into the stratosphere by
      volcanic eruptions cool the oceans and temporarily offset the rise
      in global sea level caused by the greenhouse effect, according to
      research findings published today in Nature.
      Research team leader, Dr John Church from CSIRO and the Antarctic
      Climate & Ecosystems Collaborative Research Centre (ACECRC), says
      the study is the first to isolate and measure the effect of volcanic
      eruptions on sea level variations.

      "Using computer models and observations, we tracked sea level
      variations and temperatures in the upper 300 metres of the ocean
      recorded during and following major volcanic eruptions in the late
      20th century" Dr Church says. "What we have seen is a slowing in the
      rate of sea level rise immediately after volcanic eruptions followed
      by an acceleration over periods of a decade or more."

      This temporary slowing of sea level rise following a series of major
      eruptions occurring since 1960 (Mt Agung in Indonesia in 1963, El
      Chichon in Mexico in 1982 and Mt Pinatubo in the Philippines in
      1991) temporarily masked the acceleration of sea level rise that
      would otherwise have resulted from the effects of greenhouse gases
      in the atmosphere.

      Dr Church says although climate scientists generally agree the sea
      level has risen by an average of 1.8 mm a year over the last 50
      years, there has been little focus on the shorter term variability
      in this rate.

      "Scientists have known that volcanic aerosols cause a decrease in
      the global average surface temperature and other changes in Earth's
      climate system. However, until now there has been no study of how
      the aerosols impact on sea level and ocean temperatures," he says.

      The model results are confirmed by ocean observations. The effect
      persists for at least a decade because of the large heat capacity of
      the oceans compared to that of the atmosphere and the slow
      redistribution of heat by ocean circulation.

      Sea level rise occurs in two ways: expansion of the ocean as a
      result of ocean warming (thermal expansion); and, changes in the
      amount of water in the ocean due to melting glaciers and ice sheets.

      Other members of the team are: Dr Neil White of CSIRO and the
      ACECRC; and, Ms Julie Arblaster from the National Center for
      Atmospheric Research in the US and the Bureau of Meteorology
      Research Centre.

      The team's findings – from collaborative research involving the
      ACECRC, CSIRO's Wealth from Oceans Flagship and the Australian
      Climate Change Science Program – will be presented at a major
      international climate change conference, in Melbourne from 13-17
      November, Greenhouse 2005.

      http://www.terradaily.com/news/oceans-05y.html

      http://groups.yahoo.com/group/SeaLevelChange/

      Pat N