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Ice Time

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Karl Shimper. Stages of scientific discovery: ... The surface gets hot enough that it radiates just right to maintain. the balance. ... – PowerPoint PPT presentation

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Title: Ice Time


1
Ice Time

2
Erratics and moraines
3
Erratics
such obvious mechanical absurdities William
Hopkins
4
Scratches in rocks
Could scratches and polish just be due to ice?
Robert Murchison
5
Fjords
6
Glacier in Switzerland
7
Glacier moraine
8
Stages of scientific discovery first, people
deny that it is true then they deny that it is
important finally they credit the wrong person.
Alexander von Humboldt
Karl Shimper
Jean de Charpentier
9
History of Climate on Earth
  • The photograph taken in 1928, above, shows how
    the Upsala Glacier, part of the South American
    Andes in Argentina, used to look. The ice on the
    Upsala Glacier today, shown in 2004 below, is
    retreating at least 180 ft. per year

10
Climate over past 600 million years
Coal Deposits Desert Deposits Tropical
Soils Glacial Material Plant and animal fossils
11
Ice Core Data (past 400,000 yrs)
Bottom line Climate can be stable and regular
for long periods of time, But sometimes it can
also go crazy (in a big way) as the result of
modest causes.
12
Depiction of recent ice age
13
Current location of continents and glaciers
14
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15
Causes of Climate Change
  • Amount of energy given off by sun
  • Orbital variations (Croll)
  • Spin variations (Milancovich)
  • Plate tectonics (continents rearranging)
  • Snow White
  • Greenhouse gases

16
Solar energy output
  • Solar output increasing over Suns lifetime
  • Sun currently gives off 30 more energy than 4.5
    billion years ago
  • Liquid water not stable on Earth 2 billion years
    from now!
  • Solar cycle and changes in solar activity
  • Maunder Minimum low sunspot activity may have
    influenced Little Ice Age (17th century)

17
Sun is more active when it has sunspots
18
Does the sun give off more or less energy when
it has fewer sunspots?
19
Orbital and spin variations
  • Croll-Milankovitch cycles
  • Why werent these guys taken seriously?
  • Why did mainstream scientists resist these ideas?
  • Eccentricity (Croll)
  • Shape of orbit changes (100,000 yrs)
  • Tilt (Milankovitch)
  • Tilt changes, not always 23.5 degrees (41,000
    yrs)
  • Precession
  • Direction of the tilt changes (20,000 yrs)

20
Orbit changes affect the tilt of the Earths spin
axis. The tilt (called the obliquity) is the
reason for seasons.
21
Where is the Sun throughout the year?
zenith
and Sept 21 (Autumnal Equinox)
east
west
south
22
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23
Add all 3 cycles together, whats that spell?
Croll-Milankovitch Cycle
24
Continental Drift
  • Plate tectonics causes continents to drift
  • Location of continents and oceans affects climate
  • Himalayas Isthmus of Panama
  • http//www.scotese.com/paleocli.htm

25
The Snow White Effect
  • If part of the Earth is covered with snow, it
    reflects away sunlight, so Earth gets cooler
  • A possible runaway effect

Ice ages change very quickly 1) Biggest factor
for ice ages how cool the summers are, not how
brutal the winters are 2) If ice doesnt melt
over summer, less sunlight absorbed and it gets
colder Feedback loops (positive and negative)
can enhance or dampen climate changes
26
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27
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28
Snowball Earth Hypothesis Frozen up to 2.2
billion years ago, million year thaw, then bigger
ice age (super ice age) Temperatures may have
dropped up to 80 degrees Fahrenheit Ocean froze
over completely? What kept some life going? Some
open water over hotspot? Translucent ice? How
did we get out of snowball earth? Volcanoes?
Pushed through ice and released greenhouse
gases? Correlates with 650 million years ago and
Cambrian explosion, more on this later
29
Causes of Climate Change
  • Amount of energy given off by sun
  • Maunder Minimum
  • Orbital and spin variations
  • Croll-Milankovitch cycles
  • Precession, obliquity, eccentrity
  • Plate tectonics
  • Location of continents
  • Himalayas Isthmus of Panama
  • Snow White effect
  • Greenhouse gases
  • Greenhouse gases affect flow of energy through
    atmosphere

30
To understand how a greenhouse works, you need to
know Wiens law The hotter something is,
the shorter the wavelength that it glows
(or radiates) at. Some things (like white)
reflect light better than others (like
black). Some things scatter light (depending on
the wavelength). Pay attention to
the blackboard!
31
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32
Energy Budget Every planet heats up just
enough so that it can radiate energy out (IR)
to balance the solar energy coming in (IR
visible light) If there is an atmosphere, that
is where the planets radiation exits into space.
So the atmospheres temperature matters for
balancing the budget. The surface gets much
warmer because it gets energy from the Sun
plus some of the IR from the atmosphere
(greenhouse effect). Is the greenhouse effect
good or bad for us? As discussed later The
warmed surface radiates back up to the
atmosphere. The surface gets hot enough that it
radiates just right to maintain the
balance. Bottom line the surface is warmer
than it would be without the atmosphere acting
like a greenhouse
33
Which of the following appear to have a
greenhouse effect?
34
Wiens Law
  • Terrestrial spectrum peaks in IR around 10
    microns (.01mm)
  • Sun radiates mostly visible and IR
  • Earth radiates mostly IR

SUNLIGHT
EARTHLIGHT
35
Wavelength Dependent Absorption
  • Greenhouse gases (H20, CO2, CH4, other)
  • Absorb different wavelengths of light
  • Transmit visible light
  • Absorb and re-emit IR

http//www.ucar.edu/learn/1_3_1.htm
36
Atmosphere Absorption Spectrum
  • Very little absorption at visible wavelengths
  • Absorption of UV by ozone in upper atmosphere
  • Absorption of IR by greenhouse gases in lower
    atmosphere

37
Greenhouse gases keep IR from transmitting
directly out to space
  • The Greenhouse Effect

38
Greenhouse Effect Animation
  • http//www.colorado.edu/physics/phet/
  • http//dev.cadre.com.au/Astro_V/Project/Contact_Li
    st/

39
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40
Understanding the Greenhouse Effect (GHE)
  • Effective Temperature
  • Surface of Earth would be much colder w/out GHE
  • Spectra for sun and earth
  • Sun peaks in visible Earth peaks in IR
  • Greenhouse gases absorb at different wavelengths
  • H20, CO2, CH4
  • Transparent at visible wavelengths
  • Absorb and re-emit IR
  • Surface temperature of planet raised above
    effective temperature
  • Surface of planet is heated by energy radiated
    from the Sun AND energy re-radiated from the
    atmosphere

41
Common Greenhouse Effect (GHE) Misconceptions
  • GHE is related to ozone depletion.
  • GHE involves reflected sunlight.
  • GHE is new phenomenon on Earth.
  • GHE is harmful to life.
  • GHE on Earth is intermediate between that on Mars
    and Venus due to distance from sun.
  • GHE is caused by smog and air pollution.
  • GHE is same as global warming.

42
Human-induced Greenhouse Effect
  • Caused by humans
  • Increased levels of CO2 from burning of fossil
    fuels during industrial revolution to present
  • 1.5F (0.8 C) temperature increase over past 150
    years

43
Population is dramatically increasing
44
CO2 levels rising from emissions related to
transportation, energy, industry, and
deforestation
45
Global temperatures are rising
46
Time before present (thousands of years)
47
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48
The Earths atmosphere is very unstable. Small
things can have big effects. For the past few
thousand years, the climate has been relatively
steady, not too hot, not too cold, explaining in
part why civilization has been so successful. We
are changing the amount of an important
greenhouse gas, by putting CO2 back into the
air. Is this a good idea? Its not nice to fool
with Mother Nature
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