Triggers for the Late Ordovician Ice Age: Volcanic Aerosols vs. CO2 - PowerPoint PPT Presentation

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Triggers for the Late Ordovician Ice Age: Volcanic Aerosols vs. CO2

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Title: Triggers for the Late Ordovician Ice Age: Volcanic Aerosols vs. CO2


1
Triggers for the Late Ordovician Ice Age
Volcanic Aerosols vs. CO2
  • Konrad Cunningham UG
  • Eric Santiago HSS
  • Linda Sohl PI
  • Mark Chandler PI

2
Ordovician Period
  • Started about 500 million years ago.
  • Hardly any plants or animals lived on the land
    most were in the sea.
  • Compared to todays Sun, the Sun of the
    Ordovician was 4 dim.
  • Most land masses were in the Southern Hemisphere.

3
The Ice Age of the Ordovician
  • Lasted 0.5 to 1.5 million years.
  • Some researchers think that there was a high
    level of atmospheric CO2
  • Our hypothesis the sharp decrease in
    temperature could have been caused by a
    combination of low CO2 and high SO2 related to
    volcanic activity in the atmosphere.

4
Paleogeography
5
Volcano locations in the late Ordovician
  • The volcanoes were part of an island arc between
    Laurentia and Baltica.
  • These volcanoes were active and created 5,000
    times the volume of ash than Mt. St. Helens
    eruption in 1980.
  • The eruptions were 3 of the 20 largest events in
    the last 600 million years.

6
Anomaly Plots for SurfAirTemp
CO21000 ppm, Solar96
CO23000 ppm, Solar96
CO2500 ppm, Solar96
CO21000ppm Solar94
7
Conclusion
  • Ord_testrun3 shows that a ice age is highly
    improbable with high atmospheric CO2, no matter
    what the level of solar luminosity.
  • Ord_testrun8 gives us the most probable
    conditions on Earth that would help create an ice
    age.
  • Future simulations will explore the effects of
    both high SO2 and low CO2 on Ordovician climate.

8
References
  • Alaska Volcano Observatory
  • http//www.avo.alaska.edu/activity/avoreport.php?v
    iewkaminfoid199typekaminfomonthOctoberyear
    2006
  • ATMOSPHERIC TRANSMISSION OF DIRECT SOLAR
    RADIATION AT MAUNA LOA, HAWAII
  • http//climate.envsci.rutgers.edu/pdf/emissions_02
    07.pdf
  • Global Volcanism Program
  • http//www.volcano.si.edu/
  • Volcanic SO2 Archive Service
  • http//www.oma.be/BIRA-IASB/Molecules/SO2archive/v
    s/orbit.php
  • Mount Pinatubo Eruption
  • http//geography.about.com/library/weekly/aa030901
    a.htm
  • Ordovician
  • http//en.wikipedie.org.wiki.Ordovian
  • Impacts of Volcanic Gases
  • http//pubs.usgs.gov/of/1997/of97-262/of/97-262.ht
    ml
  • Ancient Oceans Separate the Continents
  • http/www.scotese.com/newpage1.html
  • The Geology of OhioThe Ordovician
  • http//www.dnr.state.oh.us/geosurvey/oh_geol/97_Fa
    ll/ordovici.htm
  • The size and frequency of the largest explosive
    eruptions on Earth
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