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School of Economics and Finance

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Title: School of Economics and Finance


1
Policy Discussion Meetings
Paul Frijters and Joseph Jeisman
  • Recap on series for the newcomers (1 minute)
  • Global Warming Stan Hurn (15 minutes)
  • Its not real and its not a problem by Chris
    Coleman-Fenn (15 Minutes)
  • Its real and its a problem, by Joseph Jeisman
    (15 min)
  • Group Discussion

2
Introduction to series
House notices
  • Once every 2 weeks on a Thursday.
  • Attendance roll for honours students.
  • Interruptions and arguments from students warmly
    invited. Non-presenting staff are asked to keep
    quiet until the last 20 minutes.
  • Website http//www.bus.qut.edu.au/paulfrijters/di
    scussion-meetings.jsp.

3
Background
  • This is a revamp of an earlier discussion group
    by the school, On steroids.
  • Part of a QUT wide drive towards research
    excellence. These meetings represent a major
    commitment from the school, are part of the new
    econometrics centre, and if things work out,
    youll get a better research training at this
    school than anywhere in Oz.
  • Preliminary Team Paul Frijters and Joseph
    Jeisman (main organisers), Stan Hurn, Michael
    Drew, Adrian Pagan.
  • Comes from the recognition that research at
    postgrad level in Economics and Finance is a big
    step up from an undergraduate degree and requires
    major time investments.
  • These meetings are an attempt to instil an
    academic attitude and acquaint those interested
    with a sense of the breadth and depth of policy
    relevant issues in economics and finance as well
    as a glimpse of the research frontier.

4
Timing
At the end of 2006 Functioning reading groups
and workshops
5
Global Warming
  • Statistical Fact or Fiction?
  • Stan Hurn

6
Introduction
  • To maintain a certain, constant temperature, the
    rate that Earth emits energy into space must
    equal the rate it absorbs the sun's energy.
  • Greenhouse gases, or gases conducive to the
    greenhouse effect, act like a blanket or the
    panes of glass in a greenhouse's walls they
    reflect the heat the earth would radiate into
    space back down towards the earth, holding it in.
    This keeps Earth's average surface temperature at
    about 60F (15C).
  • If there were no greenhouse gases in the
    atmosphere, most of the heat radiated by the
    Earth's surface would be lost directly to outer
    space, and the planet's temperature would be 0F
    (-18C), too cold for most forms of life.

7
The question
  • Global warming is an observed increase in the
    average temperature of the Earth's atmosphere and
    oceans.
  • Part of this increase may be due to natural
    processes, and would have occurred independently
    of human activity.
  • The remainder is due to a human-induced
    intensification of the greenhouse effect.
  • The G8 nations believe the average global
    temperature has risen 0.6 0.2 C since the late
    19th century, and that it is likely that "most of
    the warming observed over the last 50 years is
    attributable to human activities. Furthermore,
    temperatures may increase by 1.4 to 5.8 C
    between 1990 and 2100.
  • A hotly contested political and public debate
    exists over what should be done to reduce or
    reverse future warming, and how to cope with the
    consequences.

8
Anthropogenic Global Warming
  • Human caused emissions of greenhouse gases
  • CO2 (human respiration, burning of fossil fuel,
    deforestation)
  • Methane (livestock flatulence, oil and gas
    production, coal mining, solid waste, and wet
    rice agriculture)
  • Nitrous oxide (laughing gas!)
  • Chlorofluorocarbons (gases used as refrigerants
    and in aerosol spray dispensers)
  • Hydrochlorofluorocarbons and hydrofluorocarbons
    (CFC substitutes)

9
The argument
  • Before the Industrial Revolution (when greenhouse
    gases were arguably at a stable level) Earth's
    climate tended to fluctuate widely. 
  • A period from 5,000 to 3,000 BC is called the
    Climatic Optimum and another period from 900 -
    1200 AD is called the Little Climatic Optimum or
    the Medieval Climatic Optimum, both so named for
    their unusually warm temperatures. 
  • Likewise, a period from 1550 to 1850 is known as
    the Little Ice Age for its unusually cold
    temperatures.  At this time, glaciers in southern
    Norway reached their greatest extent in 9000
    years. 
  • With such large variations possible, it is
    difficult to know where the next natural
    fluctuation could take us.  Perhaps those who
    find that global climate is warming are simply
    measuring a natural fluctuation.  Or perhaps a
    natural fluctuation is masking the real effect of
    GHGs on the globe.

10
The battleground
  • Global circulation models (GCMs)
  • GCMs aim to simulate changes in climate as a
    result of slow changes greenhouse gas
    concentration.
  • GCMs model surface and deep ocean circulations
    and atmospheric condtions
  • Parameters are calibrated (not estimated) with
    resultant problem that a small error in the sea
    surface temperature a small bias in cloudiness
    can cause significant errors in long-term climate
    change prediction.

11
The battleground
  • Time series data
  • Air temperature, sea temperature, deep ocean
    temperature, the ice-core records, ice volume in
    the Antarctic
  • Particularly rich time-series data are available
  • Vostok ice-core data span more than 164,000 years
  • A number of cycles are found in this data (the
    longest is claimed to have a period of 41,000
    years!)
  • Problems
  • Sensitive to choice of sample
  • Use of simple models can be misleading. Letting
    Yt a bt et, where Yt represents the
    temperature at time t and et represents error
    from the trend line, a test of the hypothesis
    that b 0 may yield evidence of global warming.
    However, naïve models of this kind detect a
    deterministic trend in a relatively high
    percentage of realizations from a wide range of
    models where there is known to be no trend present

12
Global Warming
  • Statistical Fact or Fiction?
  • Chris Coleman-Fenn

13
Overview
  • Does global warming really exist?
  • Suppose it exists, what are its effects and do we
    thus really care?
  • How can we resolve it?

14
Does it really exist?
  • Antarctic Data
  • Whereas climate models suggest that temperatures
    in Antarctica should have been warming in recent
    decades in response to increases in greenhouse
    gases, measurements show otherwise. The majority
    of the continent shows no significant trend or an
    actual decrease.

15
Antarctic temperatures
16
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17
Does it really exist?
  • Majority of the last 2.5 million years, earth has
    been in an ice age interrupted by interglacial
    thaws. Thaws used to occur every 41000 years but
    1,000,000 years ago this changed to every 100,000
    years.
  • Mini ice-age between the 14th and 19th century.

18
Does it really exist?
  • Majority of temperature measurements are taken in
    or near cities whose populations have grown
    markedly and as cities retain more heat than
    rural areas, these measurements are biased.
  • Not all methods agree Kaser says that weather
    balloon readings show slight cooling over the
    tropics between 1979 and 1997.
  • There are other influences on temperature that
    may be more important, such as dimming (direct
    reflection of sunlight through additional
    particles in the air).

19
Suppose it does, so what?
  • Ocean conveyer belt shuts down
  • Thermohaline circulation of oceans shut down
    which would stop heat being evenly distributed
    causing increase of 2 to 2.5 degrees Celsius
    increase. Has occurred before and is reversible.
  • Greenlands ice cap melts
  • Would raise global sea levels by 7 metres and
    will occur if temperatures rise by 2.7 degrees
    and would take 1000 to 3000 years to happen.
  • Methane burps
  • If permafrost melts and penetration of ocean
    warming into sediments may cause release of
    pockets of methane trapped since formation of
    earth. May cause a 3 degrees Celsius increase in
    temperature and accelerate global warming. Has
    occurred many times before, probably after every
    ice age.
  • Other problems more pressing?
  • Nitrogen!!!!
  • Benefits from more CO2? See next slide

20
Does it really exist?
Tree rings in the US are now bigger, showing
faster biomass growth!
21
How can we resolve it if we wanted to?
  • Reducing greenhouse emissions does not seem to
    get you much fast, nor does it seem like thats
    politically feasible

22
How can we resolve it?
23
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24
How can we resolve it (II)
  • We could increase Dimming ourselves
  • aerosols reflect radiation and heat back into
    space. Increase such particles and reduce global
    warming?
  • Let nature do it (I) Increased warming will
    increase evaporation from the oceans which will
    increase the cloud cover, reflecting more heat
    and radiation back into space.
  • Let nature do it (II) Richard Lindzen of MIT
    says that global warming may dry out the upper
    levels of the troposphere. Less water in this
    level will reduce the greenhouse effect.

25
Global warming is our fault!Joseph Jeisman
26
CO2 Concentration
  • Over the last 150 years CO2 concentrations in the
    atmosphere have risen from approximately 280
    parts per million (ppm) to nearly 380 ppm.

27
How much of this rise can be attributed to human
activities?
  • Most of it (perhaps nearly all of it).
  • Best evidence Fossil fuel burning and land
    clearing reduces the ratio of 13C to 12C in the
    atmosphere natural processes do not. The ratio -
    13C/12C has become about 2 lower (e.g. examining
    tree rings, corals etc), starting its decline at
    the same time the concentration of CO2 in the
    atmosphere started to increase around 1850.

28
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29
Source http//en.wikipedia.org/wiki/Image1000_Ye
ar_Temperature_Comparison.png
30
Antarctic cooling
  • It is important to recognize that the
    widely-cited Antarctic cooling appears, from
    the limited data available, to be restricted only
    to the last two decades, and that averaged over
    the last 40 years, there has been a slight
    warming (e.g. Bertler et al. 2004).
  • It has been recognized for some time that model
    simulations result in much greater warming in the
    high latitudes of the Northern Hemisphere than in
    the South, due to ocean heat uptake by the
    Southern Ocean. This appears to be driven by
    changes in wind current that affect the
    distribution of heat in the world, not the extent
    of the increase.

Source http//www.realclimate.org
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