Loading ...
Sorry, an error occurred while loading the content.

Reconstructing the climate

Expand Messages
  • David
    Rob Gutro Goddard Space Flight Center, Greenbelt, Md. (Phone: 301/286-4044; at AGU: 415/905-1007) NOTE TO EDITORS: N03-138 SCIENTISTS RECONSTRUCT EARTH S
    Message 1 of 1 , Dec 11, 2003
    View Source
    • 0 Attachment
      Rob Gutro
      Goddard Space Flight Center, Greenbelt, Md.
      (Phone: 301/286-4044; at AGU: 415/905-1007)

      NOTE TO EDITORS: N03-138

      SCIENTISTS "RECONSTRUCT" EARTH'S CLIMATE OVER PAST MILLENNIA

      Using the perspective of the last few centuries and millennia,
      speakers in a press conference at the Fall Meeting of the American
      Geophysical Union in San Francisco will discuss the latest research
      involving climate reconstructions and different climate models.

      The press conference features Caspar Ammann of the National Center for
      Atmospheric Research (NCAR), Boulder, Colo.; Drew Shindell of NASA's
      Goddard Institute for Space Studies, New York; and Tom Crowley of Duke
      University, Durham, N.C. The press conference is at 5 p.m. EST,
      Thursday, December 11 in the Moscone Convention Center West, Room 2012.

      Changes in the sun's activity have been considered responsible for
      some part of past climatic variations. Although useful measurements of
      solar energy are limited to the last 25 years of satellite data, this
      record is not long enough to confirm potential trends in solar energy
      changes over time. Tentative connections between the measured solar
      activity, with sunspots or the production of specific particles in the
      Earth's atmosphere (such as carbon-14 and beryllium-10), have been
      used to estimate past solar energy.

      Ammann will discuss how he used a set of irradiance estimates with the
      NCAR coupled Ocean-Atmosphere General Circulation computer model to
      show the climate system contains a clearly detectable signal from the
      sun. Ammann's work with the model also demonstrates that smaller,
      rather than larger, background trends in the sun's emitted energy are
      in better agreement with the long-term climate record, as obtained
      from proxy climate records, such as tree-ring data.

      Shindell will discuss how he used a climate model that included solar
      radiation changes, volcanic eruptions, and natural internal
      variability to arrive at a more accurate look at Earth's changing
      climate today. Shindell said that while solar radiation changes and
      volcanoes exert a similar influence on global or hemispheric
      average-temperature changes, the solar component has the biggest
      regional effect over time scales of decades to centuries, while
      volcanoes cause the largest year-to-year changes.

      Crowley will discuss one of the goals of climate modeling, to test
      whether moderately reliable predictions of regional climate change can
      be made under global warming scenarios. Using paleoclimate data,
      scientists can in some cases test computer climate-model performance.
      This testing would occur for a time period in which models accurately
      predict the larger (hemispheric-scale) response to changes in the
      Earth's radiation balance.

      NASA's Earth Science Enterprise is dedicated to understanding the
      Earth as an integrated system and applying Earth System Science to
      improve prediction of climate, weather and natural hazards using the
      unique vantage point of space.

      NCAR is a research laboratory operated by the University Corporation
      for Atmospheric Research, a consortium of 67 universities offering
      doctoral programs in the atmospheric and related sciences. NCAR's
      primary sponsor is the National Science Foundation.

      For more information and images related to the press conference on the
      Internet, visit:

      http://www.gsfc.nasa.gov/topstory/2003/1211millenium.html
    Your message has been successfully submitted and would be delivered to recipients shortly.