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The lectures in the Mini-School will meet from 11 a.m. to 12:15 p.m. on Wednesdays from September 6 through October 4, 2006
in Building 1 at 12420 Warwick Boulevard in Newport News (click
here for map).
Lectures are scheduled for 45 minutes and will be followed by a question and answer period. A guided tour of VIMS on Friday, October 6th will round out the program.
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Global Change:
From Plankton to Planet
(September 6, 2006)
Join us as Dr. Deb Bronk
explores how tiny marine organisms can influence planetary processes by
interacting with elements such as nitrogen, iron, and carbon. Dr. Bronk will also introduce the global
climate system, the greenhouse effect, and the
DOMINO program, a 5-year,
multi-institution project to study the role that plankton play in the consumption and production of
dissolved organic matter in the ocean. Bronk is the Principal Investigator on the DOMINO project,
which is funded by a grant from the National Science Foundation.
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Ocean Alchemy: Can Iron Make an Ice Age?
(September 13, 2006)
Sprinkling iron onto the ocean surface has been touted as one way to help curb global
warming—based on the idea that this iron "fetilizer" can boost the rate at which
marine plants remove carbon dioxide from the atmosphere. Join
Dr. Walker Smith's graduate student
Amy Shields as she examines whether this idea would work, and how the marine
food web might respond. Smith was a key member of the Southern Ocean Iron Experiment (SOFeX),
one of the largest oceanographic experiments ever mounted. This two-year collaborative effort
brought 3 ships, 45 tons of equipment and supplies, and 17 leading U.S. oceanographic
institutions to study the effects of iron enrichment in the waters around Antarctica. |
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Sink or Swim: Animal Drifters and the Carbon Cycle
(September 20, 2006) Join us as
Dr. Deborah Steinberg
investigates how
organic matter gets from the ocean's surface to its depths.
The fate of this material is important because it represents a potentially huge sink for
carbon dioxide—the main greenhouse gas implicated in global warming. Atmospheric carbon dioxide dissolves into seawater,
where tiny marine plants take up the carbon during photosynthesis. When these phytoplankton
die or are eaten by zooplankton, their carbon-rich tissues begin to
sink to the depths. Carbon that reaches the deep sea contributes nothing to global warming and
can remain there for thousands of years. But marine organisms and chemical reactions
continually transform this "marine snow" as it sinks. If these transformations are rapid and
sinking is slow, the materials may never reach the deep sea, instead being recycled back into
the surface ocean and atmosphere.
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Virtual Reality: Computers Models, Global Change, and You
(September 27, 2006) Policy makers rely on predictions from computer models to inform climate treaties such as the Kyoto Protocol. Global climate models generally agree that Earth's
climate is warming, although they differ in their predictions of the warming's magnitude and regional
variations. In this lecture VIMS graduate student Paul Bradley will explore how climate models work, review predicted
changes in surface temperature and sea level, and address the political debate surrounding the issue of
"global warming."
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VIMS LABORATORY TOUR
(October 6, 2006) Join
Dr.
Walker Smith
at 11 am for a 1-hour guided tour of the Virginia Institute of
Marine Science in Gloucester Point, including a tour of a research laboratory.
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