Climate Change

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Climate Change

• The 4-point consensus view of global warming
• Some objections impartially considered
• (Evaluating Impacts)

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The 4-point consensus on global warming!

• Its happening (certain)
• We're causing it (almost certain)
• It will continue (yes but how much)
• This will be a Bad Thing (weaker)

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(1) Global Warming is happening...
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(2) We're causing it
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(2) We're causing it (cont...)
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(2) ...we're causing it (...cont 2)
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(3) It will get worse
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(4) This will be a Bad Thing

• Sea level rise is bad, but slow
• Temperature rise regionally varying winners and
  losers, political tradeoffs
• Ecological impacts important, but I don't know

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Antarctica and Greenland are melting!
Greenland www.realclimate.org/index.php?p267
Antarctica scienceblogs.com/stoat/2006/03/grace_p
uzzle.php
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Common myths, impartially considered

• Satellite temperatures - show warming too
• The urban heat island - negligible effect
• The hockey stick controversy
• The Day After Tomorrow - will not happen
• Little relation between the Ozone hole and GW
• CO2 increase is anthropogenic (more than...)

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Satellite temperature measurements

• Mears et al 0.193 C/decade
• Spencer and Christy version 5.2, 0.123 C/decade
• Fu et al, 0.2 C/decade (May 04)
• Vinnikov and Grody, with 0.22C to 0.26C per
  decade (Oct. 03)
• Surface record 0.06 C/decade over the past
  century and 0.15 C/decade since 1979.

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Urban Heat Island (1)

• Cities tend to be hotter than the surrounding
  countryside. But (for the purposes of the
  temperature record) we care about trends ie are
  cities getting even warmer?
• Hansen et al. (JGR, 2001) adjusted trends in
  urban stations around the world to match rural
  stations in their regions, in an effort to
  homogenise the temperature record. Of these
  adjustments, 42 warmed the urban trends which
  is to say that in 42 of cases, the cities were
  getting cooler relative to their surroundings
  rather than warmer. One reason is that urban
  areas are heterogeneous, and weather stations are
  often sited in "cool islands" - parks, for
  example - within urban areas.
• IPCC UHI does not exceed about 0.05C over the
  period 1900 to 1990, because
• land, sea, and borehole records are in agreement
• the trends in urban stations for 1951 to 1989
  (0.10C/decade) are not greatly more than those
  for all land stations (0.09C/decade).
• the differences in trend between rural and all
  stations are also virtually unaffected by
  elimination of areas of largest temperature
  change, like Siberia, because such areas are well
  represented in both sets of stations.

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Urban Heat Island (2)

• Peterson, J Clim, 2003 "Assessment of urban
  versus rural in situ surface temperatures in the
  contiguous United States No difference found"
  indicates that the effects of the UHI may have
  been overstated, finding that Contrary to
  generally accepted wisdom, no statistically
  significant impact of urbanization could be found
  in annual temperatures. This was done by using
  satellite-based night-light detection of urban
  areas, and more thorough homogenisation of the
  time series (with corrections, for example, for
  the tendency of surrounding rural stations to be
  slightly higher, and thus cooler, than urban
  areas).
• Parker, Nature 2004 attempts to test the urban
  heat island theory, by comparing tempature
  readings taken on calm nights with those taken on
  windy nights. If the urban heat island theory is
  correct then instruments should have recorded a
  bigger temperature rise for calm nights than for
  windy ones, because wind blows excess heat away
  from cities and away from the measuring
  instruments. There was no difference between the
  calm and windy nights, and the author says we
  show that, globally, temperatures over land have
  risen as much on windy nights as on calm nights,
  indicating that the observed overall warming is
  not a consequence of urban development.
• Publication bias Peterson notes that essentially
  all large-scale studies showed some urban centres
  cooling. But no individual city studies did.
  People were reporting what they expected to see.

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Hockey Stick controversy...or,The temperature
over the last 1-2 kyr
http//en.wikipedia.org/wiki/Image1000_Year_Tempe
rature_Comparison.png
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The day after tomorrow...will not happen

• Simulations using the HadCM3 climate model of the
  Atlantic thermohaline circulation from 1860-2000
  (using historical variations of greenhouse gases,
  sulphate aerosol, solar radiation and volcanic
  dust). The simulations show a freshening of the
  Labrador Sea from 1950-2000, as has been seen in
  observations, but this is associated with a
  slight strengthening of the thermohaline
  circulation over the same period, rather than a
  weakening as has sometimes been suggested. When
  the simulations are extended forward from
  2000-2080 (using a projection of future
  greenhouse gases and aerosols), both trends are
  reversed, with a salting in the Labrador Sea and
  a weakening thermohaline circulation

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Ozone hole/depletion and climate change

• Although they are often interlinked in the
  popular press, the connection between global
  warming and ozone depletion is not strong.
• Global warming from CO2 radiative forcing is
  expected (perhaps somewhat surprisingly) to cool
  the stratosphere. This, in turn, would lead to a
  relative increase in ozone depletion and the
  frequency of ozone holes.
• Conversely, ozone depletion represents a
  radiative forcing of the climate system. O3
  losses over the past two decades have tended to
  cool the surface.
• One of the strongest predictions of the GW theory
  is that the stratosphere should cool. However,
  although this is observed, it is difficult to use
  it for attribution (for example, warming induced
  by increased solar radiation would not have this
  upper cooling effect) because similar cooling is
  caused by ozone depletion.

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CO2 emissions... reductions?
http//mustelid.blogspot.com/2005/11/more-uk-co2-e
missions.html

• Of the "frontrunners" one is an order of
  magnitude bigger than the rest Extend UK
  participation in EU carbon trading scheme (4.2).
  Means don't actually produce less CO2, but buy
  permits to emit it.
• Of the "emerging" category, the two biggest are
  Introduce ways to store carbon pollution
  underground (0.5-2.5) (i.e., don't produce any
  less, just...) and Force energy suppliers to use
  more offshore wind turbines (Up to 1). Which
  would actually save CO2.
• In the "difficult" category the biggest is Change
  (read enforce) road speed limits (1.7) - a
  surprisingly large number.
• Road transport is big - telecommute!

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Evaluating Impacts

• Not really my thing just some ideas
• Of the Consensus View, the weakest point is
  ...and it will be a bad thing. Which is not to
  say its wrong, just harder to evaluate. Risk
  change from what we (and ecologies) are adapted
  to.
• Sea Level Rise is fairly obviously bad, but
  probably slow (surprises?)
• Ecological impacts I don't know but difficult
  political choices how many flights to go skiing
  are people prepared to forgo, in order to save
  polar bears (were that the choice).

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Wikipedia!

• For readers
• For writers
• A model community

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What do you find on wikipedia?

• Lots of useful articles (global warming)
• Lots of useless articles (Jordanhill railway
  station VFD)
• People working together collaboratively
• People fighting like ferrets in a sack (rules
  3RR Civility...) over predictable things (Jesus
  Cartoons controversy Palestine Gdansk anything
  to do with the Balkans...)
• A power structure of sorts (users admins
  mediaton arbcomm developers Jimbo Wales)

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The community/Power structure

• Normal users won't notice it User pages
• If you vandalise, you will be noticed (counter
  vandalism unit! Crypto Derks Vandal Fighter) and
  warned and blocked if you persist. If you're
  excessively rude, ditto
• All pages have Talk Pages
• IRC (tends to be for the experienced
  sub-community)
• 3RR slows down content disputes. After that
• RFC (requests for comments)
• Mediation
• Arbitration
• Elections for admins/arbcomm
• VFD

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