1 uiuc atmos 397g biogeochemical cycles and global change lecture 12: carbon and climate don...
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ATMOS 397GATMOS 397GBiogeochemical Cycles and Global ChangeBiogeochemical Cycles and Global Change
Lecture 12: Carbon and ClimateLecture 12: Carbon and Climate
Don WuebblesDon Wuebbles
Department of Atmospheric SciencesDepartment of Atmospheric Sciences
University of Illinois, Urbana, ILUniversity of Illinois, Urbana, IL
February 27, 2003February 27, 2003
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Climate change is one of the biggest issues confronting humanity in the 21st century
However,Global climate change much better understood than regional changes Large uncertainties remain in interpreting climate change to the local and regional scale
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Mann et al. (1999)
1000 year reconstruction
~ 0.7 oC (~ 1.3 oF) increase in global surface temperature during last 140 years
(IPCC, 2001)
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The Evidence for Global WarmingThe Evidence for Global Warming
Warmest temperatures in 1000 years 13 of last 15 years highest in 150+ years of global surface data 1998 warmest, then 2001
Major decline in glacier extent Increase in water vapor Increase in cloud cover (than 1950s) Increase in precipitation at higher latitudes and decrease in
tropics Shortened seasons of lake ice Decrease in extent of snow cover Large decrease in Arctic sea ice extent Increase in sea level
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1000 Year Temperature Records1000 Year Temperature Records
Annual Temperatures Mann et al., GRL, 1999
Global; Proxies (tree rings, ice cores, and other data)
Crowley and Lowery, AMBIO, 2000 N.H.; Proxies (tree rings, corals, ice cores, and
other data) and temperature records Huang et al., Nature, 2000
Global; Boreholes
Warm Season Temperatures Jones et al., Holocene, 1998 Briffa, Quat. Sci. Rev., 2000
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T. Crowley, Science, July 2000T. Crowley, Science, July 2000
“the agreement between modeling results and observations for past 1000 years is sufficiently compelling to allow one to conclude that natural variability plays only a subsidiary role in the 20th century warming and that the most parsimonious explanation is that is due to the anthropogenic increase in GHGs (greenhouse gases).”
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The Evidence for Global WarmingThe Evidence for Global Warming
Major decline in glacier extent
Example: The Rhone glacier in the Bernese Oberland, Switzerland
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IPCC (1996)International assessment: Climate Change 1995, The Science of Climate Change
“Nonetheless, the balance of evidence suggests a discernible human influence on global climate”
IPCC (2000)New climate assessment (>500 scientists)
“there has been a discernible human influence on global climate”
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There have been large increases in atmospheric concentrations of greenhouse gases and in aerosols over the last century ---
Human activities predominate as the causes of these increases
The Drivers of Climate Change
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The Effect of a Gas on Climate?The Effect of a Gas on Climate?
Determined by its radiative forcing relative to other forcings on climate
What is radiative forcing? Increase in concentration of a greenhouse gas
allows more of the outgoing infrared radiation of the Earth to be absorbed by the atmosphere
This reduces the efficiency by which the Earth cools to space
Tends to warm the lower atmosphere and surfaceTends to warm the lower atmosphere and surface
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Radiative Forcing on ClimateRadiative Forcing on Climate
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The Evidence for a Human Effect on ClimateThe Evidence for a Human Effect on Climate
Both land and ocean temperatures increasing Largest changes at higher latitudes Patterns of climate change Stratosphere is cooling Diurnal cycle is decreasing Modeling studies can only explain the 20th
century climate trends if include greenhouse gas forcing effects
Cannot explain in terms of natural variability or natural forcing alone
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Constant Emissions of COConstant Emissions of CO22 Does Not Does Not Mean Constant ConcentrationMean Constant Concentration
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IPCC SRES SCENARIOSIPCC SRES SCENARIOS
A1: A world of rapid economic growth and rapid introduction of new and more efficient technologies
A2: A very heterogenous world with an emphasis on familiy values and local traditions.
B1: A world of dematerialization and introduction of clean technologies
B2: A world with an emphasis on local solutions to economic and environmental sustainability
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IPCC (2000) SRES Scenarios ---IPCC (2000) SRES Scenarios ---“Business as Usual”“Business as Usual”
SRES “MARKER” Scenarios A1, A2, B1, and B2 are based on narrative storylines, describe alternative future developments in economics, technical, environmental and social dimensions.
A1 rapid economic growth, low population growth, rapid introduction of new and more efficient technology. In this world, people pursue personal wealth rather than environmental quality.
A2 emphasis on family values and local traditions, high population growth, and less concern for rapid economic development.
B1 rapid change in economic structures, "dematerialization" and introduction of clean technologies. The emphasis is on global solutions to environmental and social sustainability.
B2 emphasizes local solutions to economic, social, and environmental sustainability, with less rapid and more diverse technological change but a strong emphasis on community initiative and social innovation to find local, rather than global solutions.
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EmissionsEmissionsfor the SRESfor the SRES
ScenariosScenarios
5
10
15
20
25
30
CO
2 (G
tC)
B2
B1
A2
A1
25
50
75
100
125
SO
2 (
MtS
O2)
2000 2020 2040 2060 2080 2100
300
400
500
600
700
800
900
CH
4 (
MtC
H4)
4
8
12
16
20
N2O
(M
tN)
IPCC SRES EMISSION SCENARIOS
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COCO22 Emissions for the SRES Scenarios Emissions for the SRES Scenarios
5
10
15
20
25
30
CO
2 (G
tC)
B2
B1
A2
A1
25
50
75
100
125
SO
2 (
MtS
O2)
2000 2020 2040 2060 2080 2100
300
400
500
600
700
800
900
CH
4 (
MtC
H4)
4
8
12
16
20
N2O
(M
tN)
IPCC SRES EMISSION SCENARIOS
5
10
15
20
25
30
CO
2 (G
tC)
25
50
75
100
125
SO
2 (
MtS
O2)
2000 2020 2040 2060 2080 2100
300
400
500
600
700
800
900
CH
4 (
MtC
H4)
4
8
12
16
20
N2O
(M
tN)
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Gas Concentrations Gas Concentrations derived for the SRES derived for the SRES
ScenariosScenarios300
400
500
600
700
800
900C
O2 (
pp
mv)
B2
B1
A2
A1
1000
1500
2000
2500
3000
CH
4 (
pp
bv)
2000 2020 2040 2060 2080 2100
300
320
340
360
380
400
N2O
(p
pb
v)
IPCC SRES SCENARIOSISAM Estimated Concentrations
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Derived CO2 Concentration – SRES ScenariosDerived CO2 Concentration – SRES Scenarios
All SRES envelop
reference case
A1B Scenario envelop including climate sensitivity uncertainty
All SRES envelop including climate sensitivity uncertainty
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Uncertainty in projecting COUncertainty in projecting CO22
Model studies of uptake of Anthropogenic CO2 show possible “saturation” effects.
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Projected temperature responseProjected temperature response
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Projected sea level responseProjected sea level response
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Sandbags in Alaska
Coastal Florida
Sea Level Rise has Societal and Ecological Implications
Toxic Algae Blooms
Coral Bleeching and Destruction
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Concerns about Impacts of Climate Change are at Concerns about Impacts of Climate Change are at the Local to Regional Levelthe Local to Regional Level
Concerns Temperature, precipitation, winds Changes in sea level Severe weather (heat waves, cold snaps, floods,
droughts) Impacts
Water quality / quantity Air quality Agriculture Forests Ecosystems Communities, cities Human health (disease and health patterns) Infrastructure (transportation, energy systems)
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Achieving a Sustainable Climate (ASC)—Positioning Achieving a Sustainable Climate (ASC)—Positioning National Resources to Resolve Climate ChangeNational Resources to Resolve Climate Change
Improving definition of the problem Diagnosis and understanding (climate, carbon cycle,
etc.) Evaluating the impacts Determine ability to adapt to some climate change
Solving the problem Technology to increase conservation / efficiency Reduced-carbon energy technology development
—Public acceptance of nuclear technology—Fuel cells, etc.
Carbon capture and sequestration
ASC would also help solve other energy issues (e.g., California 2001; Reliance on foreign oil)
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ASC---The Climate Change ChallengeASC---The Climate Change Challenge
The IPCC business-as-usual scenarios
0.00
5.00
10.00
15.00
20.00
25.00
30.00
35.00
40.00
1990 2000 2010 2020 2030 2040 2050 2060 2070 2080 2090 2100
IS92a
Range of O
ther IS92 Scenarios
Fossil Fuel Carbon Emissions, Billions of tonnes per year
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ASC---The Climate Change ChallengeASC---The Climate Change Challenge
1992 United Nations Framework Convention on Climate Change (FCCC)
GOAL—”…stabilization of greenhouse gas concentrations in the atmosphere at a level that would prevent dangerous anthropogenic interference with the climate system.” (Article 2)
Stabilizing Concentrations Is not the Same as Stabilizing Emissions
Stabilizing Concentrations Implies Human-related Emissions Must (approximately) Go to ZERO.
Cumulative EmissionsConcentrations
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ASC---The Climate Change ChallengeASC---The Climate Change Challenge
Changes Required in Human-related CO2
Emissions to Stabilize Atmospheric Concentrations
Requires peak & then decline in emissions
Emissions Trajectories Consistent With Various Atmospheric CO2 Concentration Ceilings
-5
0
5
10
15
20
1990 2090 2190 2290
750 ppmv650 ppmv550 ppmv450 ppmv350 ppmvIS92a
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0
5,000
10,000
15,000
20,000
25,000
1990 2005 2020 2035 2050 2065 2080 2095
Mill
ion
s of
Ton
nes
of
Car
bon
per
yea
r
Reference Emissions
CO2 Emissions Cap
GAP
The Challenge: The Challenge: Achieving a Sustainable Climate Achieving a Sustainable Climate
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IS92a Business-as-Usual scenario assumes ~11 TW Carbon Free Energy by 2050
Hoffert et al. (Nature, 1998)
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Without New Technology: Without New Technology: Carbon Emissions & Concentrations Will RiseCarbon Emissions & Concentrations Will Rise
Emissions Concentrations
0.0
5.0
10.0
15.0
20.0
25.0
30.0
35.0
40.0
45.0
50.0
1990 2010 2030 2050 2070 2090
Pg
C/y
r
IS92a(1990 technology)
IS92a
550 Ceiling
0
100
200
300
400
500
600
700
800
900
1000
1100
1990 2010 2030 2050 2070 2090
ppm
v
IS92a(1990 technology)IS92a550 CeilingPreindustrial
Preindustrial CO2
Current EnergyS&T can reducecarbon emission.
But stabilization
requires additional
Carbon S&
T!
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Resolving scientific uncertainty Emissions mitigation, Technology development, Climate adaptation
Climate policy requires a portfolio of responses, Climate policy requires a portfolio of responses, including …including …
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1990 2005 2020 20352050
20652080
2095
0
5,000
10,000
15,000
20,000
25,000
Mill
ion
s of
Ton
nes
of
Car
bon
per
yea
r
soil carbon sequestrationsequestration from fossil power generationsequestration from synfuels productionsequestration from H2 productionend-use technology improvementsnuclearsolarbiomass550 ppmv emissions
19902005
20202035
2050 2065 2080 2095
0
5,000
10,000
15,000
20,000
25,000
Mill
ion
s of
Ton
nes
of
Car
bon
per
yea
r
soil carbon sequestrationsequestration from fossil power generationsequestration from synfuels productionsequestration from H2 productionsynfuelsfinal energynuclearsolarbiomass550 ppmv emissions
CBF 550 AOG 550
Uncertain Technology …
Need flexibility while developing technology
Analyses from Jae Edmonds, 2001
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When take a cost effective technology out of the portfolio, the costs of stabilizing CO2
are raised—The Value of Carbon Capture & Sequestration
CBF
NOTES
CP=Carbon capture & sequestration from fossil fuels used to generate electric power.
H2 Seq.=Fossil fuels used as feedstocks for hydrogen production with carbon capture and sequestration.
Results from Jae Edmonds, 2001
No Sequestration
Soil Seq. Only
Central Power Seq.
CP + H2 Seq.
CP + H2 + Soil Seq.
750 ppmv
650 ppmv
550 ppmv450 ppmv
$6,845
$4,738$4,928
$3,326
$2,180$1,453$1,034
$940 $520 $389$529$377 $299
$149 $123$266 $193 $137 $62 $52$0
$1,000
$2,000
$3,000
$4,000
$5,000
$6,000
$7,000
$ bi
llion
s
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ASC---The Climate Change ChallengeASC---The Climate Change Challenge
Stabilization requires fundamental change in the energy system
Technology advances are key to stabilizing CO2 concentrations and
controlling costs
Diversified technology portfolios are essential to manage risk Technologies that fill the “gap” are not part of the current energy system. Carbon capture and sequestration technologies expand dramatically. The technology portfolio changes over time. Some technologies are more important when others are also available. Some technologies expand their relative importance without expanding their
absolute deployment.
Need to revisit the technology strategy frequently
Energy R&D funding needs to be extensively increased as part of ASC Solution will also require public-private partnerships
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(percentages indicates real growth from 1985-1995)
$0$500
$1,000$1,500$2,000$2,500$3,000$3,500$4,000$4,500$5,000
Mil
lions o
f C
onsta
nt 1995 U
S D
oll
ars
1985 1995-9%
8%
-74%-75%
-88%-6%-49%-33% 32%
$0
$1,000
$2,000
$3,000
$4,000
$5,000
$6,000
United
Stat
esJa
pan
Canad
a
Europ
ean U
nion
German
y
United
King
dom
The N
etherl
ands
Italy
mill
ions
of
1995
US
$
.
Other Energy PrivateOther Energy PublicEnergy Conservation PrivateEnergy Conservation PublicFossil PrivateFossil PublicFusion PrivateFusion PublicNuclear Fission PrivateNuclear Fission PublicRenewable PrivateRenewable Public
Energy Research Declining,
Not Climate
Focused.
Uncoordinated, &
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Wood
Coal
OilOil (feedstock)
Gas
Hydro Nuclear
0%
20%
40%
60%
80%
100%
1850
1860
1870
1880
1890
1900
1910
1920
1930
1940
1950
1960
1970
1980
1990
It traditionally has taken 50 years or more for a technology to grow from 1 to 50% of the market.
Energy R&D
What is done in the next 10 years will strongly influence what is possible in the next 50 years