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Class Business

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Greenland ice sheet. Review of Ocean Conveyor system ... Greenland Ice core. Throughout each year, layers of snow fall over the ice sheets. ... – PowerPoint PPT presentation

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Title: Class Business


1
Class Business
  • February 6th, Guest lecture Dr. Cathy Paris (I
    will post this lecture after class)
  • Feburary 8th, Chapter 3 and Chapter 4 of Kolbert
  • February 15th, First in-class exam

2
Greenland ice sheet
3
Review of Ocean Conveyor system
  • What factors control the ocean conveyor system?

4
  • Differences in salinity between the North
    Atlantic and the Pacific
  • Differences in temperature between the North
    Atlantic and Pacific
  • Why?

5
Gulf stream
6
Questions from the reading
  • Chapter 3 Under the glacier
  • Greenland, Iceland
  • Chapter 4 The butterfly and the toad

7
On 1 July 1993, after five years of drilling, the
Greenland Ice Sheet Project Two (GISP2,)
penetrated through the ice sheet and 1.55 meters
into bedrock recovering an ice core 3053.44
meters in depth, the deepest ice core thus far
recovered in the world.
8
Ice Cores
  • Records go back 100,000 for Greenland
  • And 400,000 years for Antarctica

9
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10
Greenland Ice core
11
  • Throughout each year, layers of snow fall over
    the ice sheets.
  • Each layer of snow is different in chemistry and
    texture, summer snow differing from winter snow.
  • Summer brings 24 hours of sunlight to the polar
    regions, and the top layer of the snow changes in
    texturenot melting exactly, but changing enough
    to be different from the snow it covers. The
    season turns cold and dark again, and more snow
    falls, forming the next layers of snow.

12
Information from ice cores
  • The ice cores can provide an annual record of
    temperature, precipitation, atmospheric
    composition, volcanic activity, and wind
    patterns.
  • The make-up of the snow can tell scientists about
    past temperatures.

13
How is it done?
  • Scientists employ heated drills,
  • The ice cores are then sampled, and the
    composition of the water is measured.
  • the ratio of isotopes is determined
  • the percent deviation of the isotope ratio from
    the a standard of known composition,

14
What is an isotope?
  • Atoms with the same number of protons, but
    differing numbers of neutrons. Isotopes are
    different forms of a single element.
  • Examples Carbon 12 and Carbon 14 are both
    isotopes of carbon, one with 6 neutrons and one
    with 8 neutrons (both with 6 protons).

15
The ratio of O-18 to O-16 is a proxy for
temperature change
  • Oxygen occurs in two common stable isotopes, O-16
    and O-18
  • O-16 is the most abundant
  • Ratio of O-18/O-16 is called delta (d)

16
Oxygen-Isotope composition of water
  • The isotopic concentration of sea water is the
    standard against all other waters are measured
  • THEREFORE delta0 for the sea water.
  • Measure deviations from this standard.

17
How can we use this to examine temperature?
  • When sea water evaporates, the heavier isotope is
    left behind in the remaining sea water, while the
    water vapor has more of the lighter isotope.
  • So evaporated water is higher in the lighter
    element but the sea water is higher in the
    heavier element
  • In snow, colder temperatures (less evaporation
    from the ocean) result in higher concentrations
    of light oxygen.

18
Direct temperature measurements from ice
  • Scientists can confirm these chemistry-based
    temperature measurements by observing the
    temperature of the ice sheet directly.
  • The ice sheets thickness makes its temperature
    much more resistant to change than the six inches
    of snow that might fall on your driveway during a
    winter snowstorm.
  • the ice sheet can be compared to a frozen roast
    that is put directly into the oven. The outside
    heats up quickly, but the center remains cold,
    close to the temperature of the freezer, for a
    long time.
  • Similarly, the ice sheet has warmed somewhat
    since the Ice Age, but not completely. The top
    has warmed as global temperatures have warmed,
    while the bottom has been warmed by heat flow
    from deep inside the Earth. But in the middle of
    an ice sheet, the ice remains close to the Ice
    Age temperatures at which it formed.

19
Isotopic rations
  • Oxygen isotope ratios
  • 1 glacial ice fossils
  • 2 ocean floor
  • 3 coral reefs

20
Coral reefs
  • The oxygen isotopes in coral skeletons are a
    record of water temperature

21
(red is warmer than average, blue cooler than
average) Yellow bars indicate El Nino years.
22
Other isotope ratios
Deuterium is heavier than Hydrogen
23
  • The coldest snow is the lightest because as air
    cools down, it loses moisture, in essence, the
    heavier isotopes drop out earlier so what is left
    when snow is finally formed is the lighter
    elements.

24
Biological signal
  • Examples from the book

25
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26
Interview with Chris Thomas
  •   Why do you think your paper is highly cited?
  • We showed that it is possible to tackle the
    question "what proportion of species might 
    become extinct as a result of climate change...
  • This paper attempts to quantify a major
    environmental crisisthat climate change may
    drive a substantial percentage of species to
    extinction. While this has been mentioned by
    previous papers, this is the first paper to
    tackle the issue head on. Our preliminary
    conclusions have surprised a lot of people.
  •   Does it describe a new discovery or a new
    methodology that's useful to others?
  • The approach we developed is probably the key
    advance. We showed that it is possible to tackle
    the question "what proportion of species might
    become extinct as a result of climate change"
    through a series of logical steps involving a set
    of analyses and simulations, each of which can be
    improved in the future or even replaced by a
    better method. We hope that our paper will spur
    others on to achieve these improvements.
  •   Could you summarize the significance of your
    paper in layman's terms?
  • Climate change may drive approximately 10 to 40
    of species to extinction because they either will
    not have anywhere climatically suitable to live
    in future, or because they will not be able to
    cross human-dominated landscapes to reach areas
    that will be suitable.
  •   How did you become involved in this research?
  • It came about initially, by my realizing that a
    substantial proportion of the British butterfly
    species on which I had been workingthe Orange
    Tip butterfly (Anthocharis cardamines)were
    shifting their distributions northwards.
  • Chris D. Thomas
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