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  • Kansas Legislator Proposes Bill to Outlaw Sustainability Education
    A bill has been introduced in the Kansas legislature this week that would prohibit the promotion of ...Read more

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    Kansas Legislator Proposes Bill to Outlaw Sustainability Education

    A bill has been introduced in the Kansas legislature this week that would prohibit the promotion of sustainability. Here is a link to the one-page bill: http://www.kslegislature.org/li/b2013_14/measures/documents/hb2366_00_0000.pdf. See report on Bloomberg News.
  • Earth's Center Is 1,000 Degrees Hotter Than Previously Thought, Synchrotron X-Ray Experiment Shows
    Scientists have determined the temperature near the Earth’s center to be 6000 degrees Celsius, 1000 ...Read more

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    Earth's Center Is 1,000 Degrees Hotter Than Previously Thought, Synchrotron X-Ray Experiment Shows

    Scientists have determined the temperature near the Earth’s center to be 6000 degrees Celsius, 1000 degrees hotter than in a previous experiment run 20 years ago. These measurements confirm geophysical models that the temperature difference between the solid core and the mantle above, must be at least 1500 degrees to explain why the Earth has a magnetic field. For more information about this study, see the press release from the European Synchrotron Radiation Facility.
  • Ocean Volcanic Rocks Contain Samples of Recycled Crust
    Scientists have long believed that lava erupted from certain oceanic volcanoes contains materials fr...Read more

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    Ocean Volcanic Rocks Contain Samples of Recycled Crust

    Scientists have long believed that lava erupted from certain oceanic volcanoes contains materials from the early Earth’s crust. But decisive evidence for this phenomenon has proven elusive. New research from a team including Carnegie’s Erik Hauri demonstrates that oceanic volcanic rocks contain samples of recycled crust dating back to the Archean era 2.5 billion years ago. Their work is published in Nature. Oceanic crust sinks into the Earth’s mantle at so-called subduction zones, where two plates come together. Much of what happens to the crust during this journey is unknown. Model-dependent studies for how long subducted material can exist in the mantle are uncertain and evidence of very old crust returning to Earth’s surface via upwellings of magma has not been found until now. For more information about these results, see the press release from the Carnegie Institution.

"Build a Tree" Dendrochronology Activity

The interactive diagram below demonstrates a very simple model of tree ring growth.

Select a temperature range (Normal, Cool, or Warm) and a precipitation amount (Normal, Dry, or Wet) for the coming year. Click the "Add Yearly Growth" button. The tree (which you are viewing a cross-section of the trunk of) grows one year's worth, adding a new ring.

Add some rings while varying the temperature and precipitation. Which of these factors has a stronger influence on the growth of the type of tree being modeled here?

Use the "Reset" button to start over.

The "Show Specimen Tree" button displays a section of an "actual" tree specimen. Can you model the annual climate during each year of the specimen tree's life, matching your diagram with the specimen, to determine the climate history "written" in the rings of the specimen tree? (The "answer" is listed below, lower down on this page).

Some Limitations of this Tree Ring Model

Tree ring cross-section

Real tree rings are much messier than the ones in this simulation, but the same principles apply.
Credit: UCAR

"All models are wrong... some models are useful." - George E.P. Box

  • Real tree ring cross-sections are not so nice and perfectly circular (and centered), or even symmetric, like the ones in this model.
  • Different types of trees have different responses in their growth rates to temperature and precipitation. Some really like warm conditions, while others are happiest when it is especially wet.
  • Other variables (besides temperature and precipitation) influence growth rates of trees.
  • Real trees have a central section called the "pith"; our model starts right in with the first annual ring instead.

The annual climate sequence for the "specimen" tree in the interactive model, starting with the tree's first year of its 15-year long life, is:

  1. normal & normal (temperature & precipitation)
  2. warm & normal
  3. normal & normal
  4. warm & normal
  5. warm & dry
  6. warm & dry
  7. normal & dry
  8. normal & normal
  9. warm & normal
  10. normal & normal
  11. cool & wet
  12. normal & normal
  13. warm & normal
  14. warm & wet
  15. warm & wet

Please refer to our Changing Planet: Survival of Trees Classroom Activity and Video for more on tree rings.

Last modified October 15, 2011 by Jennifer Bergman.

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