Ch 4. The three modern global change problems. - PowerPoint PPT Presentation

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Ch 4. The three modern global change problems.

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Title: Intro-1 EOSC 112 Course Overview [text KKC, pp.] Author: William Hsieh Last modified by: ytang Created Date: 6/28/2003 6:10:43 AM Document presentation format – PowerPoint PPT presentation

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Title: Ch 4. The three modern global change problems.


1
Ch 4. The three modern global change
problems.
2
  • Earth has been changing and will continue to do
    so. It is changing faster today than it ever has.
    The major reason is human activity.
  • Ozone depletion Ozone hole in South Pole
  • deforestation
  • Greenhouse gases and global warming

3
  • Ozone
  • source O and O2 makes it through chemical
    process.
  • Location in middle-layer atmosphere
    (stratosphere).
  • roles absorb ultraviolet radiation from
    Sun.

4
Vertical Structure of the Atmosphere
4 distinct layers determined by the change
of temperature with height
5
  • Ozone depletion describes two distinct, but
    related observations
  • (1) a slow, steady decline of about 4 per
    decade in the total volume of ozone in Earth's
    stratosphere (ozone layer) since the late 1970s,
  • (2) a much larger, but seasonal, decrease in
    stratospheric ozone over Earth's polar regions
    during the same period.

6
  • Ozone ( ) is a form of oxygen, and protects
    the earths surface from Suns harmful
    ultraviolet radiation. Ozone depletion is the
    result of a complex set of circumstances and
    chemistry .
  • Antarctic Ozone Levels in Fall 2003
  • The ozone hole is represented by the purple, red,
    burgundy, and gray areas that appeared over
    Antarctica in the fall of 2003. The ozone hole is
    defined as the area having less than 220 Dobson
    units (DU) of ozone in the overhead column (i.e.,
    between the ground and space).

7
Image of the largest Antarctic ozone hole ever
recorded (September 2006).
8
Ozone over Antarctic during Oct.
9
  • Mean total ozone over Antarctica during the month
    of October

10
  • It shows a sharp drop beginning in the early
    1970s. The graph to the left shows long-term
    ozone levels over Arosa, Switzerland. Although
    ozone levels rise and fall in natural cycles, the
    average level remained constant from 1926 until
    1973. Beginning in 1973, however, and continuing
    through 2001, ozone levels have dropped at a rate
    of 2.3 percent / decade.

11
  • Too much ultra-violet light can result in
  • Skin cancer
  • Eye damage such as cataracts
  • Immune system damage
  • Reduction in phytoplankton in the oceans that
    forms the basis of all marine food chains
    including those in Antarctica.
  • Damage to the DNA in various life-forms. So far
    this has been as observed in Antarctic ice-fish
    that lack pigments to shield them from the
    ultra-violet light (they've never needed them
    before)
  • Probably other things too that we don't know
    about at the moment.

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  • Global warming is the serious problem because
  • It affects the greatest number of people
  • Migration of marine animals could result
  • Rising sea level could result
  • Cold climate species might die
  • Ozone depletion and deforestation are both
    confined to particular areas whereas global
    warming is truly global

14
  • Global warming is the serious problem because
  • It affects the greatest number of people
  • Migration of marine animals could result
  • Rising sea level could result
  • Cold climate species might die
  • Ozone depletion and deforestation are both
    confined to particular areas whereas global
    warming is truly global

15
  • Why does a ozone hole form over Antarctica?
  • The ozone hole is caused by the effect of
    pollutants in the atmosphere destroying
    stratospheric ozone. During the Antarctic winter
    something special happens to the Antarctic
    weather.
  • Firstly, strong winds blowing around the
    continent form,
  • this is known as the "polar vortex" -  this
    isolates the air
  • over Antarctica from the rest of the world.
  • Secondly, clouds form called Polar
    Stratospheric
  • Clouds. Clouds turn out to have the effect
    of
  • concentrating the pollutants that break down
    the ozone,
  • so speeding the process up.

16
Deforestation
17
Deforestation affects Carbon balance Hydrological
cycle Radiative energy balance Biodiversity
18
Statistics
It has been estimated that about half of the
earth's mature tropical forests between 7.5
million and 8 million km2 of the original 15
million to 16 million km2 , have now been
cleared since 1947.
  • North America and Europe already done
  • 85 of old growth forests in US destroyed by
    settlers most replanted
  • Parts of Pacific NW and Alaska deforesting now
    as fast as Brazil

Canada One case of deforestation in Canada is
happening in Ontario's boreal forests, near
Thunder Bay, where 28.9 of a 19,000 km² of
forest area had been lost in the last 5 years
and is threatening woodland caribou. This is
happening mostly to supply pulp for the facial
tissue industry. In Canada, less than 8 of the
boreal forest is protected from development and
more than 50 has been allocated to logging
companies for cutting.
19
Tropical Rainforest
Earth's most complex biome in terms of both
structure and species diversity abundant
precipitation and year round warmth. Climate
Mean monthly temperatures are above 64F
precipitation is often in excess of 100 inches a
year. Vegetation 100 to 120 feet tall
canopy. Soil infertile, deeply weathered and
severely leached. Red color because of high iron
and aluminum oxides. Fauna Animal life is highly
diverse Distribution of biome 10N and 10S
latitude. Neotropical (Amazonia into Central
America), African (Zaire Basin with an outlier in
West Africa also eastern Madagascar),
Indo-Malaysian (west coast of India, southeast
Asia)
20
  • Tropics
  • Rainforests 50 years ago covered 14 of the
    world's land surface and have been reduced to 6,
    and that all tropical forests will be gone by the
    year 2090
  • Brazil slash and burn Amazon 200 increase
    in deforested area from 1979 - 1988

Some scientists have predicted that unless
significant measures (such as seeking out and
protecting old growth forests that have not been
disturbed) are taken on a worldwide basis, by
2030 there will only be ten percent remaining.
21
The problem
  • Disappearing at a rate of tens of thousands of
    square miles per year
  • Land clearing in developing countries for
    farming and ranching (e.g., Brazil)
  • Wood as a fuel (e.g., 90 of Africans use wood
    as primary fuel)
  • Ballooning populations in developing countries
  • Loss of fauna associated with the forests
  • Current extinction rate of 50,000 species per
    year
  • Rate reflects fact that most fauna and flora in
    tropics are disappearing
  • Loss of soil value for farming (formation of
    laterites)

22
Effects
  • Lowered oxygen production levels
  • Increased CO2
  • Changed climate (radiation, temperature) and
    hydrologic cycle
  • Loss of flora and fauna
  • Increased soil erosion (i.e., global erosion
    rate of 25.4 billion tons of top soil per year)
  • Increased effects of floods, especially coastal
    (e.g., 10x increase
  • in catastrophic floods in Bangladesh)
  • Landslides
  • Cycle (vicious circle)
  • deforestation ? soil erosion and loss of wood
    materials ? lowered productivity of soil and
    loss of wood source ? increased human needs ?
    enhanced deforestation
  • e.g., 40-50 million trees removed in Haiti each
    year
  • correlates with 7x increase in food aid over
    last 20 years

23
  • Global warming

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The balance of evidence suggests that there is a
discernible human influence on global climate '
Intergovernmental Panel on Climate Change (United
Nations), Second Assessment Report, 1996
27
There is new and stronger evidence that most of
the warming observed overthe last 50 years is
attributable to human activity'
Intergovernmental Panel on Climate Change (United
Nations), Third Assessment Report, 2001
28
Most of the observed increase in globally
averaged temperatures since the mid-20th century
is verylikely due to the observed increase in
anthropogenic greenhouse gas concentrations
Intergovernmental Panel on Climate Change (United
Nations), Fourth Assessment Report, 2007
29
Discovery of the Greenhouse Effect
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34
GREENHOUSE EFFECT?
Glass allows visible radiation to pass through
the glass which absorbs thermal radiation and
re-emits some of it back into the greenhouse ---
like a radiation blanket.
35
Heat Transfer --- Convection
  • Less dense warm air moves upward and more dense
    cold air moves downward.
  • Convection is the dominant process for
    transferring heat in the troposphere.

36
The distribution of temperature in a convective
atmos.(red line). The green line shows how the
temperature increases when the amount of CO2
present in atmos. is increased (in the diagram
the difference between the lines is exaggerated).
Also shown for the two cases are the average
levels from which thermal radiation leaving the
atmosphere originates (about 6km for the
unperturbed atmosphere).
37
Radiation is emitted out to space by these gases
from level somewhere near the top of the atmos.
typically from between 5 and 10km high. Here,
temperature is much colder -30 50C or so colder
than at the surface. gt emitting less radiation
to space. So absorb radiation emitted from the
earth surface but then to emit much less
radiation out to space.
38
Component of the radiation (in watts per square
meter) which on average enter and leave the
earths atmos. and make up the radiation budget
for the atmosphere.
39
The enhanced greenhouse effect
F ?T4 ? 5.67 x 10-8 W/m2/K4
average levels from which thermal radiation
leaving the atmosphere originates
40
Blackbody rad. curves for Sun Earth
?max const./T Temp. T in K const. 2898 ?m
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46
Planetary energy balance
  • Earth is at steady state
  • Energy emitted by Earth
  • Energy
    absorbed ..(1)
  • E emitted (area of Earth) ? ? Te4
  • 4? Re2 ? ? Te4
  • (Te Earths effective rad. temp., Re Earths
    radius)
  • E absorbed E intercepted - E reflected
  • Solar E intercepted S ?Re2 (solar flux S)
  • Solar E reflected AS ?Re2 (albedo A)
  • E absorbed (1-A) S ?Re2
  • (1) gt 4? Re2 ? ? Te4 (1-A) S ?Re2

47
Magnitude of greenhouse effect
  • ? Te4 (1-A) S/4
  • Te (1-A) S/(4 ? )1/4 (i.e. fourth root)
  • Te 255K -18C, very cold!
  • Observ. mean surf. temp. Ts 288K 15C
  • Earths atm. acts as greenhouse, trapping
    outgoing rad.
  • Ts - Te ?Tg, the greenhouse effect
  • ?Tg 33C

48
Greenhouse effect of a 1-layer atm.
  • Energy balance at Earths surface
  • ?Ts4 (1-A)S/4 ?Te4 ..(1)
  • Energy balance for atm.
  • ?Ts4 2 ?Te4 .. (2)

49
  • Subst. (2) into (1)
  • ?Te4 (1-A)S/4 ..(3) (same eq. as in last
    lec.)
  • Divide (2) by ? take 4th root
  • Ts 21/4 Te 1.19 Te
  • For Te 255K, Ts 303K. (Observ. Ts 288K)
  • ?Tg Ts - Te 48K,
  • 15K higher than actual value.
  • Overestimation atm. is not perfectly absorbing
    all IR rad. from Earths surface.

50
  • Weather forecasting also uses atm. GCMs.
    Assimilate observ. data into model. Advance model
    into future gt forecasts.
  • Simpler 1-D (vertical direction)
    radiative-convective model (RCM)
  • Doubling atm. CO2 gt 1.2C in ave.sfc.T
  • Need to incorporate climate feedbacks
  • water vapour feedback
  • snow ice albedo feedback
  • IR flux/Temp. feedback
  • cloud feedback

51
Water vapour feedback
  • If Ts incr., more evap. gt more water vapour gt
    more greenhouse gas gt Ts incr.
  • If Ts decr., water vap. condenses out gt less
    greenhouse gas gt Ts decr.
  • Feedback factor f 2.
  • From RCM ?T0 1.2C (without feedback)
  • gt ?Teq f ?T0 2.4C.

()
52
Snow ice albedo feedback
  • If Ts incr. gt less snow ice gt decr. planetary
    albedo gt Ts incr.

()
53
IR flux/Temp. feedback
  • So far only ve feedbacks gt unstable.
  • Neg. feedback If Ts incr. gt more IR rad. from
    Earths sfc. gt decr. Ts

(-)
  • But this feedback loop can be overwhelmed if Ts
    is high lots of water vap. around
  • gt water vap. blocks outgoing IR
  • gt runaway greenhouse (e.g. Venus)

54
Climatic effects of clouds
  • Without clouds, Earths albedo drops from 0.3 to
    0.1.
  • By reflecting solar rad., clouds cool Earth.
  • But clouds absorb IR radiation from Earths
    surface (greenhouse effect) gt warms Earth.
  • Cirrus clouds ice crystals let solar rad. thru,
    but absorbs IR rad. from Earths sfc.
  • gt warm Earth
  • Low level clouds (e.g. stratus) reflects solar
    rad. absorbs IR gt net cooling of Earth

55
  • IR rad. from clouds at ?T4
  • High clouds has much lower T than low clouds
  • gt high clouds radiate much less to space than
    low clouds.
  • gt high clouds much stronger greenhouse effect.

56
Uncertainties in cloud feedback
  • Incr. Ts gt more evap. gt more clouds
  • But clouds occur when air is ascending, not when
    air is descending. If area of ascending/descending
    air stays const.
  • gt area of cloud cover const.
  • High clouds or low clouds? High clouds warm
    while low clouds cool the Earth.
  • GCMs resolution too coarse to resolve clouds gt
    need to parameterize (ie. approx.) clouds.
  • GCM gt incr. Ts gt more cirrus clouds gt warming
    gt positive feedback.
  • gt ?Teq 2 -5C for CO2 doubling

57
Greenhouse Gases
Water Vapor Carbon Dioxide (CO2) CH4 methane,
N2O nitrous oxide...
58
NATURAL GREENHOUSE EFFECT
59
ENHANCED GREENHOUSE EFFECT
60
  • Water Vapor
  • source evaporation from Earths surface
  • location the lowest 5 km of the
    atmosphere
  • residence time 10 days
  • variation range 0.1 - 4
  • roles in atmosphere source of moisture
    for
  • cloud absorber of energy
    emitted by
  • Earths surface greenhouse
    gas.

61
Water Vapor
  • Naturally occurring greenhouse gas, generally
    unaffected by humans.

Importance The Clausius-Clapeyron relationship
(shown below) suggests that warmer air can hold
more water vapor. As the planet warms due to the
greenhouse effect, more water vapor will change
global climate conditions.
By solving for water vapor (e), we can see that
temperature (T) increases the amount of water
vapor.
62
  • Carbon Dioxide (CO2)
  • source plant and animal respiration, the decay
    of organic materials, and natural and
    anthropogenic (human-produced).
  • Current concentration 380ppm (parts per
    million, i.e., 0.04) a global increase in
    recent decades.
  • The increase in carbon dioxide (CO2) has
    contributed about 72 of the enhanced greenhouse
    effect to date, methane (CH4) about 21 and
    nitrous oxide (N2O) about 7.

63
The Carbon Cycle
  • There is a natural process by which carbon
    dioxide is cycled through the Earth's ecosystems
    and atmosphere.
  • The blue arrows represent the natural processes
    by which living organisms emit and absorb carbon
    throughout their life and death (e.g.
    Respiration, photosynthesis, decomposition)?

The red arrows represent the anthropogenic flux
which is a scientific term for the human effect
on the carbon cycle, including industrialization
and fossil fuel burning.
64
  • carbon is exchanged between the biosphere,
    geosphere, hydrosphere, and atmosphere of the
    Earth.
  • Four reservoirs of CO2 atmosphere, ocean,
    biosphere and sediments.
  • Carbon cycle modeling. Models of the carbon
    cycle can be incorporated into global climate
    models, so that the interactive response of the
    oceans and biosphere on future CO2 levels can be
    modeled. Such models typically show that there
    is a positive feedback between temperature and
    CO2.

65
  • The land and ocean are large reservoirs to stock
    carbon than atmos. For example, the release of
    just 2 of the carbon stored in the oceans would
    double the amount of atmos. CO2.
  • At the time scales which we concern, CO2 is not
    destroyed but redistributed among the various
    carbon reservoirs. E.g., about 50 of an increase
    in atmos. CO2 will be removed within 30 years, a
    further 30 within a few centuries, and the
    remaining 20 may remain in the atmos. for many
    thousands of years.

66
The Human Footprint
  • 5 of the world's population resides in the
    United States, creating ¼ of the total greenhouse
    gas emissions.
  • For most people, their car is the main source of
    emissions. 22Lbs of CO2 is produced from every
    gallon of gas. Do the math
  • Number of miles traveled by car each year __ ,
    divide by average miles per gallon __ gallons
    of gas, multiplied by 22 lbs CO2/gallon of gas
    __ pounds of CO2
  • The 1997 Kyoto protocol called for all people to
    limit their carbon emissions to 5.4 tons, or
    about 11,000 lbs, per year.
  • Some scientists believe that in order to reverse
    the damage caused by greenhouse gas emissions, we
    would need to reduce our individual emissions
    down to 5,000 lbs per year.

67
Solving the Carbon Dilemma
  • What are some things that you can do to reduce
    your carbon emissions?
  • It's the act of consuming less that will
    ultimately make a difference.
  • Energy-efficient, energy-conserving electronics,
    lightbulbs, hardware and other devices are
    available for almost anything. You can expect
    that energy-efficient products are meant to last
    longer and will save you money.
  • Reduce your dependency on cars!

68
Greenhouse gases
  • Greenhouse gases (CH4 methane, N2O nitrous
    oxide)
  • trap outgoing radiation from Earths surface
  • Coal burning ? Sulfur dioxide (SO2) ? acid rain.
  • SO2 ? Sulfate aerosol, reflects sunlight gt
    cooling.
  • 1940-1970 cooling may be due to coal burning.
  • Coal burning incr. CO2 (long-term warming) and
    incr. sulfate aerosol (short-term cooling)
    aerosol washed out by precip.

69
Atmospheric CO2 concentrations--recent.
  • Seasonal cycle of atmospheric CO2
  • (Mauna Loa record)

70
  • Short-term variability

71
Global mean surface temperatures have increased
0.5-1.0 F since the late 19th century The 20th
century's 10 warmest years all occurred in the
last 15 years of the century. Of these, 1998 was
the warmest year on record. The snow cover in the
Northern Hemisphere and floating ice in the
Arctic Ocean have decreased, sea level has risen
4-8 inches over the past century.
  • Some facts of global changes
  • (1) Global warming

72
Atmospheric CO2 concentrations--past 1000 years.
73
Short term climate change
74
Holland in 1565 (Little Ice Age)
(Pieter Bruegel)
75
  • Cooling in 1940s-1960s gt fear of coming ice age!
  • Volcanic eruptions gt drop in temp. for 3 years
    (e.g., Agung 1963)
  • Viking colony on Greenland lost by early 1400s.
  • Little Ice Age in late 1500s.

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Emitted millions of tons of sulfur dioxide and
ash particles.
El Chicon Mexico, 1982
Agung, Indonesia, 1963
Mount Pinatubo, Philippines, 1991
78
London smog in 1952

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Red cross simulated global mean Tem. (62
simulations)black line mean of all
simulationsblue round observed global mean
Tem.
81
Anthropogenic greenhouse warming
  • Atm. CO2
  • Keeling started measuring atm.CO2 in 1958 on
    Mauna Loa, Hawaii
  • Seasonal cycle (forests absorb CO2 in summer
    release CO2 in winter) rising trend

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local temp. trends
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An increasing body of observations gives
a collective picture of a warming world and
other changes in the climate system
  • Global mean surface temperature increase
  • (NH, SH, land, ocean)
  • Melting of glaciers, sea ice retreat and
    thinning
  • Rise of sea levels
  • Decrease in snow cover
  • Decrease in duration of lake and river ice
  • Increased water vapor, precipitation and
  • intensity of precipitation over the NH
  • Less extreme low temperatures, more
  • extreme high temperatures

89
Recent Range Shifts due to Warming
Species Affected Location Observed Changes

Arctic shrubs Alaska Expansion into shrub-free areas
39 butterfly spp. NA, Europe Northward shift up to 200 km in 27 yrs.
Lowland birds Costa Rica Advancing to higher elevations
12 bird species Britain 19 km northward average range extension
Red Arctic Fox Canada Red fox replacing Arctic fox
Treeline Europe, NZ Advancing to higher altitude
Plants invertebrates Antarctica Distribution changes
Zooplankton, fish invertebrates California, N. Atlantic Increasing abundance of warm water spp.
Walther et al., Ecological responses to recent
climate change, Nature 416389 (2002)
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Red Arctic Fox
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Modes of Climate Variation
Periodic variation
Periodic variation
Abrupt shift in climate state
Warming or cooling to new climate state
Changes in amplitude or frequency of climate
oscillations
93
  • The three serious problems
  • The three modern global change problems
    discussed in this chapter-- global warming, ozone
    depletion, or loss of biodiversity

94
  • The ozone depletion is the serious problem
    because
  • It causes the most immediate damage to our planet
    and its inhabitants
  • It can cause skin cancer
  • It occurs faster than global warming, because
    global temperatures only rise 1 degree in 100
    years so this is an insignificant amount compared
    to the decline in the total amount of ozone

95
  • The loss of biodiversity is the serious problem
    because
  • There is potential for recovery for the other
    problems the ozone layer could recover within a
    few generations and greenhouse gas concentrations
    should return to normal within a few million
    years.
  • The recovery rate for species following
    extinction is tens of millions of years.
  • Once a species is gone, it is gone for good.
  • It could cause an imbalance in the Earths
    ecosystem and economy.
  • Deforestation also contributes to global warming.

96
  • Global warming is the serious problem because
  • It affects the greatest number of people
  • Migration of marine animals could result
  • Rising sea level could result
  • Cold climate species might die
  • Ozone depletion and deforestation are both
    confined to particular areas whereas global
    warming is truly global
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