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How Humans First Altered the Global Climate (William Ruddiman)

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Title: How Humans First Altered the Global Climate (William Ruddiman)


1
How Humans First Altered the Global Climate
(William Ruddiman)
  • Presenter Chris Simmons
  • November 13, 2006

2
The Main Idea
  • CO2 (Carbon Dioxide) and CH4 (Methane) have
    varied according to regular cycles for the past
    several hundred years, according to ice core
    evidence
  • About 10,000 years ago, this 400,000 year-long
    cycle ended and both gases gradually began
    increasing when they should have been decreasing
  • This cycle breakdown also corresponds to the time
    period of the advent of horticulture/pastoralism/a
    griculture as a human subsistence strategy
  • Ruddiman argues that the changes in GHG cycles is
    directly correlated to the change in human
    cultural development

3
Natural Methane and CO2 cycles
  • As we have seen in class, the Earths major
    orbital/axial changes (and related solar forcing
    changes) occur on 22,000, 41,000, and 100,000
    year cycles (precession, obliquity, and
    eccentricity respectively)
  • 3 Km long ice cores in Vostok (with air bubbles
    bubbles preserved in each ice layer) record
    atmospheric composition and show cyclical GHG
    changes

4
The Methane Cycle
  • Methane follows the precession cycle
  • Most atmospheric methane is formed from the decay
    of wetland vegetation (Methane is also known as
    swamp gas because of this)
  • Most of the worlds continental landmass and
    wetlands are in the Northern Hemisphere, so
    methane levels are closely connected to solar
    radiation variation in the Northern Hemisphere

5
The Methane Cycle
  • Strong sunshine in NH results in high methane
    output
  • More meltwater in high latitude continental
    regions
  • Greater monsoon activity in Asia (greater heating
    of land/ water, more evaporation and
    precipitation possible)
  • As the NH summer becomes aligned with the
    aphelion, wetland activity decreases and methane
    levels drop
  • Thus, methane levels generally bottom out around
    now (NH summer is furthest away from the sun, SH
    summer closest to sun)

6
An Illustration of the Methane Cycle
7
The Recent Breakdown in the Methane Cycle
8
Some Values for the Natural Methane Cycle
  • Maximum MethaneInterglacial period, NH summers
    at the perihelion700 ppb
  • Minimum Methane450 ppb when NH summer reaches
    the aphelion
  • RECENT REVERSAL We are now in the aphelion, and
    over the past 5,000 years methane has been 250
    ppb above the expected value

9
Carbon Dioxide Cycle
  • Similar type of predictable pattern as Methane
    through most of the Vostok Core
  • The sum effects of precession, eccentricity, and
    obliquity produces predictable CO2 variations
  • peak at 275-300 ppm at very beginning of each
    warm period, decline steadily
  • minimum245 ppm
  • RECENT REVERSAL 8,000 years ago, began
    increasing when it should have been decreasing,
    as much as 40 ppm above cyclical average by start
    of the industrial era.

10
An Illustration of the Carbon Dioxide Cycle
11
The Recent Breakdown in the Carbon Dioxide Cycle
12
Properties of Greenhouse Gases (Particularly
Methane)
  • CH4 is a very important greenhouse gas a
    relatively small increase in Methane can have a
    large impact on the longwave absorptivity of the
    atmosphere
  • Demonstration using MODTRAN3, a moderate
    resolution radiation transfer model, available
    at
  • http//geosci.uchicago.edu/archer/cgimodels/radia
    tion.html

13
An Atmosphere of No CO2 or Methane (At 70 km,
looking down)
Ground T, K 272.20 (fixed for average
Midlatitude Winter) Iout, W/m2 250.352
14
An Atmosphere of No CO2 and 10000ppm Methane (At
70 km, looking down)
Ground T, K 272.20 (fixed for average
Midlatitude Winter) Iout, W/m2 234.37
15
An Atmosphere of No CO2 or Methane (At 70 km,
looking down)
Ground T, K 272.20 (fixed for average
Midlatitude Winter) Iout, W/m2 250.352
16
An Atmosphere of 10000ppm CO2 and No Methane (At
70 km, looking down)
Ground T, K 272.20 (fixed for average
Midlatitude Winter) Iout, W / m2 218.23
17
Model Output Conclusions
  • Carbon Dioxide absorbs near the wavelength of
    maximum emission of the Earth (mid to thermal
    IR), Methane absorbs at significantly shorter,
    higher energy wavelengths (near IR)
  • Extreme values of Carbon Dioxide (without any
    Methane present) lead to greater warming than the
    same extreme values of Methane (without any
    Carbon Dioxide present)Methane saturates
    sooner due to less radiation emitted at higher
    near-IR wavelengths
  • However, lets look at a more realistic scenario
    with less extreme variation..

18
Todays Atmosphere of 330ppm CO2 and 1.75ppm
Methane (At 70 km, looking down)
Ground T, K 272.20 (fixed for average
Midlatitude Winter) Iout, W/m2 228.247
19
An increase of 0.25ppm of Methane (CO2 kept
constant)
Ground T, K 272.20 (fixed for average
Midlatitude Winter) Iout, W/m2 228.184
So we have an increase of 0.063 W/m2 flux at the
surface
20
An increase of 0.25ppm CO2 (Methane kept constant)
Ground T, K 272.20 (fixed for average
Midlatitude Winter) Iout, W / m2 228.247
So we have an increase of lt0.0005 W/m2 at the
surface (several orders or magnitude less than
with the same increase in Methane)
21
Things to Learn from this Demonstration The
Properties of Methane
  • Given reasonable initial GHG levels, a small
    increase in CH4 has a much larger impact on
    global temperature than the same small increase
    in CO2
  • Methane absorbs at shorter, higher energy
    wavelengths than CO2 and absorbs across a longer
    spectrum of wavelengths than CO2
  • So, smaller impacts (pre-industrial human
    activities) on methane levels can drive
    significant climate change, hence the authors
    and others focus on human-related methane
    increases
  • Post-industrial Methane has increased over 1ppm
    since 1750.

22
Changes in Human Cultural Development
  • Before 10,000 years ago, humans lived primarily
    in foraging cultures
  • Also called hunting and gathering
  • After the end of the last ice age, humans began
    cultivating crops and keeping livestock
  • this required deforestation, fire burns, etc,
    which allowed for increasing CO2 and CH4
  • Horticulture, Pastoralism, and Agriculture
    widespread across much of the world by 5,000
    years ago
  • Allowed for increased population density (more
    food than before with foraging cultures)

23
Pre-industrial Humans Influence on Methane Levels
  • Rice Paddies Humans create their own wetlands
    by trapping rainwater and runoff
  • particularly in SE Asia
  • increases methane Levels (author stresses this is
    the reason for reversal 5,000 years ago)
  • Livestock Cows and other animals release
    methane in feces and belches, and human waste as
    well adds to methane(yes, and it does make a
    difference!).
  • Greater population associated with agricultural
    subsistence means more waste and livestock.

24
Pre-industrial Humans Influence on Methane Levels
  • Agricultural and Deforestation Fires perhaps
    the primary source of methane increases
  • NIWA Study http//www.niwascience.co.nz/pubs/mr/
    archive/2005-09-09-1

25
Agricultural Burns
  • The NIWA group analyzed isotopic signatures of
    Carbon in methane found in the Vostok ice core
  • Can track how methane was produced by its carbon
    isotope ratio (rice paddies vs. vegetative
    fires).
  • fires produce more Carbon-12, which becomes the
    carbon element of methane molecules
  • Low Carbon-13/Carbon-12 ratios in ice cores
    reveal that much of the atmospheric methane of
    the past few thousand years has been connected to
    burns.
  • thus, more grassfires/wildfires than one would
    expect producing higher methane levels
    (anthropogenic)
  • Native Americans and other groups used burning as
    a primary means or replenishing the land,
    agricultural burns still practiced today around
    the world.

26
Increase in Carbon Dioxide
  • Deforestation for agriculture removes trees that
    provide important carbon dioxide sinks
  • we know from tools used to cut down trees that
    this process began 8,000 years ago in China,
    Europe
  • silts and clays eroding from previously-forested
    hillsides can also provide clues to deforestation
    rates
  • Much of the deforestation in N Europe took place
    during Charlemagnes time, Domesday book from
    1100s indicates 90 of England deforested at
    that time.
  • Cautionary Note most important deforestation
    effects will be in tropical regions that hold the
    most extensive forests (lack of data in this
    region)

27
An Ice Age Prevented?
  • 250 ppb Methane, 40 ppm Carbon Dioxide from
    expected levels. What are the consequences of
    these increases?
  • average warming of 0.8C (with all models
    sensitivities)
  • Authors individual climate model run 1.5-2C
    cooling, last ice age was only 5-6C cooler than
    today
  • put 1.5C cooler temps in model, significant
    glaciers start forming in Canada
  • ice age might have been only a few thousand years
    away without this anthropogenic,
    agriculture-related warming, so weve essentially
    delayed the next ice age

28
Pandemics and GHG Levels
  • Pandemics reduce agricultural activity and aerial
    coverage
  • allow trees/vegetation to grow back (in 50 yrs)
  • leads to decreasing CO2
  • Major Pandemics Justinians Plague, Bubonic
    Plague Outbreaks, the Native American pandemics
    after discovery

29
Pandemics and GHG Levels A Critical View
  • Pandemics do not always cause significant changes
    in agricultural activities
  • Immediately after the Black Death, some villages
    were abandoned, but most land was recultivated
    within a few years, and the population rebounded
    within 100 years
  • Urban areas most affected by the Black Death
  • Europe has a very small land area and its
    forests CO2 sink is small on a global scale

30
Pandemics and GHG Levels A Critical View
  • The North American Pandemic might have had a
    greater impact on global methane increases than
    CO2 decreases
  • Native Americans burnt vast areas (Great Plains),
    which produced C-12 rich methane
  • Pandemic wiped out 90 of native population,
    European immigration halted cultural
    farming/burning practices in many parts of the
    Americas
  • Lead to methane decreases (NIWA)
  • Possible CO2 decrease associated with less
    horticultural slash-burning agriculture in the
    rainforests of Central America

31
Other Thoughts?
  • Foraging humans likely set fires as well, so why
    is this trend only seen in recent data from the
    past 10,000 years? Why not from before the last
    ice age as well? Were fires really increased
    because of agriculture?
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