Title: Class Business
1Class 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
2Greenland ice sheet
3Review 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?
5Gulf stream
6Questions from the reading
- Chapter 3 Under the glacier
- Greenland, Iceland
- Chapter 4 The butterfly and the toad
7On 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.
8Ice Cores
- Records go back 100,000 for Greenland
- And 400,000 years for Antarctica
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10Greenland 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.
12Information 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. -
13How 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,
14What 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)
16Oxygen-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.
17How 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.
18Direct 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.
19Isotopic rations
- Oxygen isotope ratios
- 1 glacial ice fossils
- 2 ocean floor
- 3 coral reefs
20Coral 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.
22Other 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.
24Biological signal
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26Interview 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