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©2009 Dowlatabadi
2
Overview
• What is the challenge?
• What are our options?
• What is geoengineering?
• What’s next?
©2009 Dowlatabadi
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Have you Noticed Climate Change Related to Global Warming?
Globe & Mail 27/01/2007
©2009 Dowlatabadi
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Is Global Warming Occurring Due to Human Activity?
Globe & Mail 27/01/2007
©2009 Dowlatabadi
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Are Consumers or Industry to Blame for Most Carbon Emissions?
Globe & Mail 27/01/2007
©2009 Dowlatabadi
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Are Greenhouse Gases the Same Issue as Smog?
Globe & Mail 27/01/2007
©2009 Dowlatabadi
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Can Global Warming Be Solved?
Globe & Mail 27/01/2007
©2009 Dowlatabadi
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Outcomes
Intervention
CC Completely Solved12%
CC Partially Solved70%
Not Solved at all
15%
Don’t Know & no answer
3%
Mitigation Emissions & other forcing factors > 2 GtCeq/yr
e.g., Kyoto: ~ 5% reduction in CC by 2050
Adaptation to reduce impacts from remaining ~95% CC
residual CC impacts not solvable by adaptation
Geoengineering
Iff some adverse effects of CC are less tolerable ...
©2009 Dowlatabadi
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Human Activities & Geoengineering
Outcome
Extraction of Services
Modify the Earth System
Acts
Agriculture intentional unintentional
Fossil energy intentional unintentional
Hydro dams intentional unintentional
Wind power intentional unintentional
Geogengineering intentional
©2009 Dowlatabadi
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Impacting the Earth System
• Unintended impacts have been large enough to change climate. – Those who hold fast that climate change is “mostly”
natural believe human activity is on too small a scale (compared to nature) to have brought about global change.
• The potential to impact is determined by the rate of extraction cf. rate of renewal– fresh water ...– wind power ...
©2009 Dowlatabadi
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A Short History of Intentional GeoEngineering
1905 virtue of CO2 emissions warming the earth, extending agriculture pole-wards and increasing food production.
– Russia 1932 the Soviet Union took climate modification seriously,
experimenting with cloud seeding. 1961 USSR conducts an experiment that cleared away clouds
from a 20,000 km2 area.– They were seeking to destroy arctic ice cover.
– US 1957 worry about strategic advantage of USSR.
1960s well funded programs focus on weather modification.
1966 started extensive cloud seeding in VIetnam
– International 1972 convention against military modification of environment.
©2009 Dowlatabadi
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Intolerable?Antigua and Barbuda
Marshall Islands
Bahamas
Mauritius
Barbados
Nauru
Belize
Niue
Cape Verde
Palau
Comoros
Papua New Guinea
Cook Islands
Samoa
Cuba
Singapore
Cyprus
Seychelles
Dominica
Sao Tome and Principe
Dominican Republic
Solomon Islands
Fiji
St. Kitts and Nevis
Federated States of Micronesia
St. Lucia
Grenada
St. Vincent and the Grenadines
Guinea-Bissau
Suriname
Guyana
Tonga
Haiti
Trinidad and Tobago
Jamaica
Tuvalu
Kiribati
Vanuatu
Maldives
Palau
Kiribati
Nauru
Florida Keys
©2009 Dowlatabadi
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Florida +6m Sea Level Rise
©2009 Dowlatabadi
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Unimaginable?
• The Trinity test was conducted while there were doubts about the potential for an A-bomb to set off an atmospheric chain reaction.
Image courtesy of US Govt. Defence Threat Reduction Agency
©2009 Dowlatabadi
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Geoengineering Options
• Change balance of solar radiation– in space– in the upper atmosphere– by surface modification
• Change carbon release to the atmosphere– through sequestration of captured CO2
• Change carbon uptake (... life of other GHGs)– in oceans and land through modified ecosystems
©2009 Dowlatabadi
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Blinds in Space
At L1, the angle of scatter needs to be ~ 0.01 rad~3x103 t mass
©2009 Dowlatabadi
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Sails in Orbit
source: http://antwrp.gsfc.nasa.gov/apod/image/0303/solarsail_msfc_m.jpgext
In earth orbit, the angle of scatter needs to be ~ 1 rad~3x105 t
©2009 Dowlatabadi
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More Persistent Clouds
source: http://earthobservatory.nasa.gov/NaturalHazards/natural_hazards_v2.php3?img_id=3120
©2009 Dowlatabadi
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Modelling Results
• Gavindasamy & Caldeira (2000, GRL) modelled a 1.8% reduction in solar constant.– In 2xCO2 run 97% of surface temperatures were
significantly different to control.– In 2xCO2+Geoengineering, 15% of pixels on earth
had significantly different temperature and seasonal patterns were not different to control.
• Budyko (1950s)– ~107 tSO2 in stratosphere counters 2xCO2 forcing.– Jet travel in 2005 led to 250MtC of CO2 emissions. If
we use 2% S fuel dispersal will be free.
©2009 Dowlatabadi
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Teller et al.
• 105 t of metallic mesh-structure particles enough to increase albedo by 1%.
• If made of Aluminium they would have long shiny life in stratosphere but oxidise in troposphere.
• Thickness of wires is determined by optical depth in metal (20 nm) and mesh spacing has to be 1/2 the wavelength of scattered light we plan to scatter (300 nm).
• Not cheaper than sulphur in jet fuel, but far lower in inadvertent impacts.
http://www.filmnight.org/images/Strange2.JPG
©2009 Dowlatabadi
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Ocean Fertilisation
source: http://science.hq.nasa.gov/oceans/images/seawifs_carbon.jpg
©2009 Dowlatabadi
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Pump It Down
• Redfield studies molar ratio of elements making up living tissue. was identified by Redfield– C:N:Si:P found consistently in the ratio of
106:16:15:1
• Much of ocean N-limited, and many N-fixers are limited by availability of Fe. – C:Fe = 10,000:1
• IronEx I, II, III in the 90s led to a commercial venture that aims to increase fish production and cash in on the GHG offset market.– I can’t find any of the papers or data on these any
more!
©2009 Dowlatabadi
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Lock It Up
• Geologic weathering provides the material for normal sequestration of CO2.
• CO2 has an exothermic reaction with serpentine rocks (MgSiO3).
• In principal, power-plants can separate CO2 and react it with serpentine.
• The volume of material needed is similar to the volume of fossil fuels being consumed. – This is a very costly option both in economics and in
disturbance to the environment.
http://geography.berkeley.edu/ProgramCourses/2003_Field_Pictures/SouthCoast/0304_Serpentine.jpg
©2009 Dowlatabadi
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Geoengineering
Energy Balance Energy Transport
Short Wave Albedo
Long Wave Emissivity
OceanAtmosphere & Surface
Goals space & atmospheric scattererssurface albedo
uptake of CO2 and conversion of other GHGs.
changing ocean salinity/turnover
changing: rate of evaporationSurface roughness
Means aerosolsdeforestationbuild surfaces
afforestationGMO enhanced photosynthesisOH- for CH4, O+ for N2O
large dams (Gibraltar)OTECiceberg transport
surface treatmentswind turbines
Cost ~50 B - ~300B to offset 2xCO2
x10~100 ? ?
©2009 Dowlatabadi
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More than Climate is Changing
• We are changing:– atmospheric composition, chemistry & physics– ocean chemistry and circulation– surface albedo and roughness
• If we want to reduce impacts, we should consider efforts that look beyond reducing forcing and reduce change in composition of the atmosphere.
©2009 Dowlatabadi
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CO2 Capture: Sleipner, Norway
www.statoil.com/.../ $FILE/sleipner.jpg
www.statoil.com/.../ $FILE/sleipner.jpg
©2009 Dowlatabadi
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No Black Magic in Amine Process
⇔
⇔
©2009 Dowlatabadi
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Below The Waves
©2009 Dowlatabadi
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CO2 Injection
Enhanced oil recovery using CO2 injection has been used for 3 decades.
©2009 Dowlatabadi
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Even in Florida
http://www.princeton.edu/~hotinski/Resources/NETL_tampa_gasification_large.jpg
©2009 Dowlatabadi
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CO2 Reservoirs & Leaks!
©2009 Dowlatabadi
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Reservoir Sizes
• Geological – Depleted oil and gas reservoirs: 200-500 GtC– Deep saline aquifers: 102-104 GtC– Deep coal beds: 100-200 GtC– Chemical reaction with Silicate rocks.
• Oceanic– Capacity is large: ~ 103-104 GtC; depending on the
“acceptable” degree of acidification.– Atmosphere-ocean carbon equilibrium: ~80% in
~300 years.
©2009 Dowlatabadi
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Renewables: Biomass
• Average power use in more industrial countries:– 5kW/cap.
• Range of energy capture in terrestrial systems:– 0.2 - 2 Wm2
• Area needed to meet all needs for average person:– 0.5 hectare/capita = 1/2 of (croplands + forests)
©2009 Dowlatabadi
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¢/kWh
tCO2/Gj
Electricity: GHG vs. Cost
©2009 Dowlatabadi
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Cost to Intervene
Geoengineering
Mitigation
CSS
% Climate Change Averted
Cost
0 100500
©2009 Dowlatabadi
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Cost of MitigationOption $/tC Risk
Stratospheric SO2 <<1 Atmospheric chemistry
Solar Shields 0.05-0.5 Does not address other impacts of CO2 increase
Ocean: Iron 1-10 Is Fe really limiting?can this be a long-term solutions?
Ocean: Phosphate 3-10 Oxygen depletion, ecological shift, long term capture questionable
Intensive forestry 10-100 Biodiversity and soils.
CO2 in ground 50-150 Low
CO2 in ocean 50-150 Moderate uncertainty about fate
©2009 Dowlatabadi
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Policy
• A shot-gun marriage between:
– the available
AND
– the imperative
©2009 Dowlatabadi
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©2009 Dowlatabadi
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Earth of tomorrow?