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Answers
Interpreting Ice Core Data
- Does there seem to be a correlation between each of the
variables and temperature? Are they proportional or inversely
proportional?
- Yes, there is a correlation between each component and the
graph of temperature. Each graph has peaks and valleys that
correspond at approximately the same time as the others, although
it may be in the opposite direction. Insolation and methane are
proportional and the calcium dust is inversely proportional to
changes in temperature.
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- Is the timing between a change in any variable and a
corresponding change in temperature immediate or is there a delay?
Why do you think a delay might exist?
- If you were to touch a hot stove you would probably feel pain,
but it often takes a second or two for your brain to register
pain. This delay is called a lag time. If an increase in the
concentration of dust in the atmosphere corresponds to a lowering
of temperature, there would be a lag time between the time of the
highest concentrations of dust and the time that the atmosphere
actually registers cooler temperatures. When there is a cause and
effect relationship between the variables and temperature there
would be some lag time no matter how small. The data plotted on
these graphs are 50 year averages; if no lag time is apparent,
that may mean that the lag time is less than 50 years.
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- Describe how any part of the graph, for any of the
variables, could be used to determine past or future climatic
conditions.
- A common method for interpreting graphs is called
extrapolating, which refers to going beyond the information given.
For example, extrapolating the graph of insolation into the past
you might suspect that the cyclic changes would continue at the
same frequency and magnitude; using this information you can
estimate the amount of insolation at any time in the past. The
same can be done for the graphs of dust and gas. During the
glacial period dust concentrations seemed to peak every 1,000
years. Extrapolating into the past, this trend may have continued
into the last interglacial warm period. Extrapolating into the
future you might conclude that the concentration of dust will
continue to rise.
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