Solar radiation management

Solar radiation management[1] (SRM) projects are a type of geoengineering which seek to reflect sunlight and thus reduce global warming.[2] Examples include the creation of stratospheric sulfur aerosols. They do not reduce greenhouse gas concentrations in the atmosphere, and thus do not address problems such as ocean acidification caused by these gases. Their principal advantages as an approach to geoengineering is the speed with which they can be deployed and become fully active, as well as their low financial cost. By comparison, other geoengineering techniques based on greenhouse gas remediation, such as ocean iron fertilization, need to sequester the anthropogenic carbon excess before they can arrest global warming. Solar radiation management projects can therefore be used as a geoengineering 'quick fix' while levels of greenhouse gases can be brought under control by greenhouse gas remediation techniques.

A study by Lenton and Vaughan suggest that marine cloud brightening and stratospheric sulfur aerosols are each capable of reversing the warming effect of a doubling of the level of CO2 in the atmosphere (when compared to pre-industrial levels).[3]

Contents

Background

The phenomenon of global dimming is widely known, and is not necessarily a geoengineering technique. It occurs in normal conditions, due to aerosols caused by pollution, or caused naturally as a result of volcanoes and major forest fires. However, its deliberate manipulation is a tool of the geoengineer. The majority of recent global dimming has been in the troposphere, except that resulting from volcanos, which affect mainly the stratosphere.

By intentionally changing the Earth's albedo, or reflectivity, scientists propose that we could reflect more heat back out into space, or intercept sunlight before it reaches the Earth through a literal shade built in space. A 0.5% albedo increase would roughly halve the effect of CO2 doubling.[4]

These geoengineering projects have been proposed in order to reduce global warming. The effect of rising greenhouse gas concentrations in the atmosphere on global climate is a warming effect on the planet. By modifying the albedo (whiteness) of the Earth's surface, or by preventing sunlight reaching the Earth by using a solar shade, this warming effect can be cancelled out - although it should be noted that the cancellation is imperfect, with regional discrepancies remaining.[5]

The applicability of many techniques listed here has not been comprehensively tested. Even if the effects in computer simulation models or of small-scale interventions are known, there may be cumulative problems such as ozone depletion, which only become apparent from large scale experiments.[6]

Various small-scale experiments have been carried out on techniques such as cloud seeding, increasing the volume of stratospheric sulfur aerosols and implementing cool roof technology.

As early as 1974, Russian expert Mikhail Budyko suggested that if global warming became a problem, we could cool down the planet by burning sulfur in the stratosphere, which would create a haze. Paul Crutzen suggests that this would cost 25 to 50 billion dollars per year. It would, however, increase the environmental problem of acid rain.[7][8][9] However, this is now believed to be a minor side effect.[10]

A preliminary study by Edward Teller and others in 1997 presented the pros and cons of various relatively "low-tech" proposals to mitigate global warming through scattering/reflecting sunlight away from the Earth via insertion of various materials in the upper stratosphere, low earth orbit, and L1 locations.[11]

Limitations

As well as the imperfect cancellation of the effect of greenhouse gases on global warming, there are other significant problems with solar radiation management as a from of geoengineering not least of these are effects on the global hydrological cycle[12] and the inability of such techniques to reduce ocean acidification.

Particular to solar radiation management, a risk of abrupt cessation exists. If SRM were to abruptly stop, the climate would rapidly warm.[13] This would cause a sudden rise in global temperatures towards levels which would have existed without the use of the geoengineering technique. The rapid rise in temperature may lead to more severe consequences than a gradual rise of the same magnitude.[13]

Atmospheric projects

These projects seek to modify the atmosphere, either by enhancing natural processes such as the sulfur cycle, or by using artificial techniques such as reflective balloons.

Stratospheric sulfur aerosols

Stratospheric sulfur aerosols: proposed by Paul Crutzen,[8] with the purpose to modify the Earth's albedo with reflective or absorptive materials spread over portions of its surface. This would typically be achieved using hydrogen sulfide or sulfur dioxide, delivered using artillery, aircraft (such as the high-flying F15-C) or balloons.[8][14][15] [16] Ozone depletion is a risk of such techniques,[17] but only if high enough quantities of aerosols drift to, or are deposited in, polar stratospheric clouds before the levels of CFCs and other ozone destroying gases fall naturally to safe levels because CFCs can settle on larger sulfate particles, increasing their ozone destroying potential.[18] This proposal, not unlike the others, carries with it considerable risks, including increased drought[19] or acid rain.[20] Broadly speaking, this technique is seen as a credible geoengineering scheme, although not one without major risks, and challenges for its implementation. This technique can give >3.7W/m2 of globally averaged negative forcing,[3] which is sufficient to entirely offset the warming caused by a doubling of CO2.

Reflective aerosols or dust

Methods based on increasing the aerosol content in the lower stratosphere for climate modification were proposed by a Russian scientist, Budyko.[21]

United States Patent 5003186 suggested that tiny metal flakes could be "added to the fuel of jet airliners, so that the particles would be emitted from the jet engine exhaust while the airliner was at its cruising altitude." Alternative proposals, not known to have been published in peer-reviewed journals, include the addition of silicon compounds to jet fuel to make silicon dioxide particles in the exhaust.[22]

A more sophisticated approach, using multi-layered nanoparticles (consisting of aluminum and barium titanate), was published by David Keith in 2010. He suggests utilizing the effects of photophoresis to increase the amount of time the aerosols stay airborne.[23]

Alleged secret experiments with aircraft exhaust modification are one version of the Chemtrail conspiracy theory.[24]

In 1992, a report by the US National Academy of Sciences (NAS)[25] on geoengineering noted that dust is a better choice compared to sulphur, because dust is from natural soil and so should have no noticeable effect on the ground as it gradually falls into the troposphere and rains out. It estimated that about 1010 kg dust would be required to mitigate the warming from a doubling of atmospheric CO2 or about 1 kg dust per 100 t of carbon emissions.

[26]

An example of the effects of the imposition of aerosol particles in the atmosphere can be found in history. Comets have been blamed for the dramatic but brief cooling period which commenced in 1159 BCE, and resulted in widespread disruption to civilisations at the time.[27] However, this mechanism, and even the involvement of a comet, is not universally accepted. If a comet was indeed to blame, the action of its aerosols could also have been by the mechanism of cloud condensation nuclei. Other examples of climate change events linked to comets include the famines around 536 CE.[28]

Cloud whitening / marine cloud brightening / cloud reflectivity enhancement

Various schemes have been suggested,[29][30] [31] such as that proposed by John Latham and Stephen Salter,[32][33] which works by spraying seawater in the atmosphere to increase the reflectiveness of clouds.[14] The extra condensation nuclei created by the spray will change the size distribution of the drops in existing clouds to make them whiter.[34] The sprayers would use fleets of unmanned Rotor ships known as Flettner vessels to spray mist created from seawater into the air to thicken clouds and thus reflect more radiation from the Earth.[29][35] The whitening effect is created by using very small cloud condensation nuclei, which whiten the clouds due to the Twomey effect.

This technique can give >3.7W/m2 of globally averaged negative forcing,[3][35] which is sufficient to reverse the warming effect of a doubling of CO2.

Ocean sulfur cycle enhancement

Enhancing the natural sulfur cycle in the Southern Ocean[36] ocean by fertilizing a small portion with iron in order to enhance dimethyl sulfide production and cloud reflectivity. The goal is to slow Antarctic ice from melting and raising sea level.[37][38] Such techniques also tend to sequester carbon, but in this specific project the enhancement of cloud albedo was both the desired outcome and measured result.[16] An alternative technique proposes the vertical mixing of ocean water, to bring deep-water nutrients to surface plankton.[39][40] This technique can give only 0.016W/m2 of globally averaged negative forcing, which is essentially insignificant for geoengineering purposes.[3]

Reflective balloons

Placing billions of aluminized, hydrogen-filled balloons in the stratosphere has been suggested to provide a reflective screen.[11][34][41][42]

These reflectors would be placed at a high enough altitude so that they do not interfere with air traffic. The cost estimate is about 20 times as much as the distribution of dust in the stratosphere,[25] making these schemes economically nonviable. The large number of reflectors and the trash problem posed by their fall make the system unattractive.

Cloud seeding

Cloud seeding has been proposed using various methods to to distribute the cloud-seeding materials, including airliners[43] and ships or power plants.[44] Reck (1978) studied the effect of increases in cloud cover and, using a radiative-convective atmospheric model, found that a 4 to 5 percent increase in low-level cloud cover would be sufficient to offset the warming predicted from a doubling of preindustrial CO2. This value is in reasonable agreement with Randall et al. (1984), who estimated that a 4 percent increase was required in the amount of marine stratocumulus, which comprises the bulk of the low clouds on a global basis."[34]

Terrestrial albedo modification

Cool roof

Painting pavements and roof materials in white or pale colours to reflect solar radiation, known as 'cool roof' technology, and encouraged by legislation in some areas (notably California).[45] This is a benign technique,[46] although limited in its ultimate effectiveness by the costrained surface area available for treatment. This technique can give between 0.01-0.19W/m2 of globally averaged negative forcing, depending on whether cities or all settlements are so treated.[3] This is generally insignificant when compared to the 3.7W/m2 of positive forcing from a doubling of CO2. However, in many cases it can be achieved at little or no cost by simply selecting different materials. Further, it can reduce the need for air conditioning, which causes CO2 emissions which worsen global warming. For this reason alone it is still demonstrably worth pursuing.

Reflective sheeting

Reflective plastic sheets covering 67,000 square miles (170,000 km2) of desert, to reflect the Sun’s energy.[47][48] This technique can give globally averaged 1.74W/m2 of negative forcing,[3] which is insufficient to offset the 3.7W/m2 of positive forcing from a doubling of CO2, but is still a very significant contribution and is sufficient to offset the current level of warming (approx. 1.7W/m2). However, the effect would be strongly regional, and would not be ideal for controlling Arctic shrinkage, which is one of the most significant problems resulting from global warming.

Ocean changes

An early geoengineering idea was to use pale coloured floating litter within certain stable oceanic gyres.[49] This litter would tend to group into large and stable areas, such as the Great Pacific Garbage Patch.[50]

Oceanic foams have also been suggested,[51] using microscopic bubbles suspended in the upper layers of the photic zone.

Farming, forestry, and land management

Forestry

Reforestation in tropical areas has a cooling effect. Deforestation of high-latitude and high-altitude forests exposes snow and this increases albedo.[52]

Grassland management

Changes to grassland have been proposed to increase albedo.[53] This technique can give 0.64W/m2 of globally averaged negative forcing,[3] which is insufficient to offset the 3.7W/m2 of positive forcing from a doubling of CO2, but could make a minor contribution towards it.

High-albedo crop varieties

Selecting or genetically modifying commercial crops with high albedo has been suggested.[54] This has the advantage of being relatively simple to implement, with farmers simply switching from one variety to another. Temperate areas may experience a 1°C cooling as a result of this technique.[55] This technique is an example of bio-geoengineering. This technique can give 0.44W/m2 of globally averaged negative forcing,[3] which is insufficient to offset the 3.7W/m2 of positive forcing from a doubling of CO2, but could make a minor contribution towards it.

Space projects

Space-based geoengineering projects are seen by many commentators and scientists as being far-fetched at present.[49]

Space mirrors

Mirrors in space: proposed by Roger Angel with the purpose to deflect a percentage of solar sunlight into space, using mirrors orbiting around the Earth.[14][56]

Moon dust

Mining moon dust to create a shielding cloud was proposed by Curtis Struck at Iowa State University in Ames [57][58][59]

Dispersive solutions

Several authors have proposed dispersing light before it reaches the Earth by putting a very large diffraction grating (thin wire mesh) or lens in space, perhaps at the L1 point between the Earth and the Sun. Using a Fresnel lens in this manner was proposed in 1989 by J. T. Early.[60] Using a diffraction grating was proposed in 1997 by Edward Teller, Lowell Wood, and Roderick Hyde.[11] In 2004, physicist and science fiction author Gregory Benford calculated that a concave rotating Fresnel lens 1000 kilometres across, yet only a few millimeters thick, floating in space at the L1 point, would reduce the solar energy reaching the Earth by approximately 0.5% to 1%. He estimated that this would cost around US$10 billion up front, and another $10 billion in supportive cost during its lifespan.[61] These ideas conflict with reality poorly in that a 1000 kilometre diameter fresnell is a 1000 kilometre diameter solar sail and it would cost a stupendous amount of energy to hold such a mirror at Lagrange-1 with the solar wind blowing at gale force way out there. Side-effects include that, if this lens were built and global warming were avoided, there would be less incentive to reduce greenhouse gases, and humans might continue to produce too much carbon dioxide until it caused some other environmental catastrophe, such as a chemical change in ocean water that could be disastrous to ocean life.[62]

See also

Global warming portal
Ecology portal
Environment portal

References

  1. ^ http://thehardlook.typepad.com/thehardlook/files/schnare_supplemental_testimony_a_framework_for_geoengineering.pdf
  2. ^ http://journals.royalsociety.org/content/84j11614488142u8/
  3. ^ a b c d e f g h Lenton, T. M., Vaughan, N. E. (2009). "The radiative forcing potential of different climate geoengineering options". Atmos. Chem. Phys. Discuss. 9 (1): 2559–2608. doi:10.5194/acpd-9-2559-2009. http://www.atmos-chem-phys-discuss.net/9/2559/2009/acpd-9-2559-2009.pdf. 
  4. ^ Committee on Science, Engineering, and Public Policy (1992). Policy Implications of Greenhouse Warming: Mitigation, Adaptation, and the Science Base. National Academy Press. p. 447. ISBN 0-309-04386-7. http://fermat.nap.edu/openbook/0309043867/html/447.html. 
  5. ^ Geoengineering the Climate: Science, Governance, and Uncertainty. London: The Royal Society. September 2009. http://royalsociety.org/Geoengineering-the-climate/. 
  6. ^ Mark, Jason (2009). "Hacking the Sky: Geo-Engineering Could Save the Planet.. And in the Process Sacrifice the World". Earth Island Journal (San Francisco, CA: Earth Island Institute) 24 (3): 40–46. ISSN 1041-0406. 472240324. 
  7. ^ Spencer Weart (July 2006). "Aerosols: Effects of Haze and Cloud". http://www.aip.org/history/climate/aerosol.htm. 
  8. ^ a b c Crutzen, P. J. (2006). "Albedo Enhancement by Stratospheric Sulfur Injections: A Contribution to Resolve a Policy Dilemma?". Climatic Change 77 (3–4): 211–220. doi:10.1007/s10584-006-9101-y. http://www.springerlink.com/content/t1vn75m458373h63/fulltext.pdf.  edit
  9. ^ Harshvardhan (June 1978). "Albedo enhancement and perturbation of radiation balance due to stratospheric aerosols". Unknown. Bibcode 1978aepr.rept.....H. 1978aepr.rept.....H. 
  10. ^ http://climate.envsci.rutgers.edu/pdf/aciddeposition7.pdf
  11. ^ a b c Edward Teller; Roderick Hyde, and Lowell Wood (1997) (PDF). Global Warming and Ice Ages: Prospects for Physics-Based Modulation of Global Change. Lawrence Livermore National Laboratory. https://e-reports-ext.llnl.gov/pdf/231636.pdf. Retrieved 2018-10-30. See pages 10-14 in particular. 
  12. ^ http://www.sciencedaily.com/releases/2008/05/080527155519.htm
  13. ^ a b Ross, A.; Damon Matthews, H. (2009). "Climate engineering and the risk of rapid climate change". Environmental Research Letters 4 (4): 045103. Bibcode 2009ERL.....4d5103R. doi:10.1088/1748-9326/4/4/045103.  edit
  14. ^ a b c Five ways to save the world-overview
  15. ^ http://www.wired.com/science/planetearth/magazine/16-07/ff_geoengineering
  16. ^ a b http://www.pmel.noaa.gov/pubs/outstand/bate1229/estimate.shtml
  17. ^ http://www.cosis.net/abstracts/EGU2008/10823/EGU2008-A-10823.pdf
  18. ^ Hargreves, Ben (2010). "Protecting the Planet". Professional Engineering (Professional Engineering Publishing) 23 (19): 18–22. ISSN 09536639. 
  19. ^ Catherine Brahic (2007-08-02). "'Sunshade' for global warming could cause drought". http://www.newscientist.com/article/dn12397. Retrieved 2009-04-29. 
  20. ^ David Over. "Sulphur screens - 21st Century Challenges". Royal Geographic Society with IBG. http://www.21stcenturychallenges.org/60-seconds/sulphur-screens/. Retrieved 2009-04-29. 
  21. ^ Budyko, M. I., Climate Changes, American Geophysical Union, Washington, DC, English translation of 1974 Russian volume, 1977, p. 244
  22. ^ http://groups.google.com/group/geoengineering/web/jet-fuel-additive
  23. ^ Keith, David W.: Photophoretic levitation of engineered aerosols for geoengineering, PNAS, September 07. 2010
  24. ^ Thomas, William Stolen Skies: The Chemtrail Mystery, Earth Island Journal, 2002
  25. ^ a b National Academy of Sciences, Policy implications of greenhouse warming: Mitigation, adaptation and the science base. National Academy Press, Washington DC, 1992, pp. 433–464.
  26. ^ G. Bala (10 January 2009). "Problems with geoengineering schemes to combat climate change". Current Science 96 (1). 
  27. ^ http://abob.libs.uga.edu/bobk/ccc/cc070799.html
  28. ^ http://www.topnews.in/comet-smashes-triggered-dry-fog-caused-famine-1500-years-ago-2106421
  29. ^ a b Latham, J. (1990). "Control of global warming" (PDF). Nature 347 (6291): 339–340. Bibcode 1990Natur.347..339L. doi:10.1038/347339b0. http://www.mmm.ucar.edu/people/latham/files/Latham_Nature_1990.pdf. 
  30. ^ Latham, J.; Salter, S. (PDF). Preventing global warming by increasing cloud albedo. http://www.mmm.ucar.edu/people/latham/files/cloud_albedo_onepage_handout.pdf. Retrieved 2008-04-20.  (A brief handout, with artist's renderings.)
  31. ^ Keith Bower, et al. (2006). "Assessment of a Proposed Technique for Global Warming Mitigation via Albedo-Enhancement of Marine Stratocumulus Clouds". Atmospheric Research 82 (1–2): 328–336. Bibcode 2006AtmRe..82..328B. doi:10.1016/j.atmosres.2005.11.013. 
  32. ^ Latham, J. (2002). "Amelioration of global warming by controlled enhancement of the albedo and longevity of low-level maritime clouds" (PDF). Atmos. Sci. Lett. 3 (2–4): 52–58. Bibcode 2002AtScL...3...52L. doi:10.1006/asle.2002.0099. http://www.mmm.ucar.edu/people/latham/files/cloud_albedo_atmos_sci_lett_2002.pdf. 
  33. ^ Salter, S, G. Sortino & J. Latham (2008). "Sea-going hardware for the cloud albedo method of reversing global warming". Phil. Trans. R. Soc. A 366 (1882): 3989–4006. Bibcode 2008RSPTA.366.3989S. doi:10.1098/rsta.2008.0136. PMID 18757273. http://rsta.royalsocietypublishing.org/content/366/1882/3989.full. 
  34. ^ a b c Panel on Policy Implications of Greenhouse Warming, National Academy of Sciences, National Academy of Engineering, Institute of Medicine (1992). Policy Implications of Greenhouse Warming: Mitigation, Adaptation, and the Science Base. The National Academies Press. ISBN 0585030952. http://books.nap.edu/openbook.php?record_id=1605&page=828. 
  35. ^ a b Latham, J., P.J. Rasch, C.C.Chen, L. Kettles, A. Gadian, A. Gettelman, H. Morrison, K. Bower, T.W.Choularton (2008). "Global Temperature Stabilization via Controlled Albedo Enhancement of Low-level Maritime Clouds". Phil. Trans. Roy. Soc. A 366 (1882): 3969–87. doi:10.1098/rsta.2008.0137. PMID 18757272. 
  36. ^ Wingenter, Oliver W.; Elliot, Scott M.; Blake, Donald R. (November 2007). "New Directions: Enhancing the natural sulfur cycle to slow global warming". Atmospheric Environment 41 (34): 7373–5. doi:10.1016/j.atmosenv.2007.07.021. 
  37. ^ http://www.climos.com/news/articles/slowingglobal.htm Oliver W. Wingenter
  38. ^ Coale, K. H.; Johnson, K. S.; Buesseler, K.; Sofex Group; Johnson; Buesseler; Sofex Group (12/2002). "SOFeX: Southern Ocean Iron Experiments. Overview and Experimental Design". American Geophysical Union. Fall Meeting 2002: 01. Bibcode 2002AGUFMOS22D..01C. 2002AGUFMOS22D..01C. 
  39. ^ http://www.johnduke.com/JDukeETCC09052007.pdf
  40. ^ http://www.cosis.net/abstracts/EGU2008/10885/EGU2008-A-10885.pdf
  41. ^ Edward Teller; Roderick Hyde, and Lowell Wood (2002) (PDF). Active Climate Stabilization: Practical Physics-Based Approaches to Prevention of Climate Change. Lawrence Livermore National Laboratory. https://e-reports-ext.llnl.gov/pdf/244671.pdf. Retrieved 2018-10-30. 
  42. ^ http://www.grida.no/publications/other/ipcc_tar/?src=/CLIMATE/IPCC_TAR/wg3/176.htm
  43. ^ Mitchell, D. L.; Finnegan, W. (2009). "Modification of cirrus clouds to reduce global warming". Environmental Research Letters 4 (4): 045102. Bibcode 2009ERL.....4d5102M. doi:10.1088/1748-9326/4/4/045102.  edit
  44. ^ http://www.reason.com/news/show/30433.html
  45. ^ Hashem Akbari, et al. (2008). "Global Cooling: Increasing World-wide Urban Albedos to Offset CO2". http://www.energy.ca.gov/2008publications/CEC-999-2008-020/CEC-999-2008-020.PDF. 
  46. ^ http://climatesafety.org/downloads/climatesafety.pdf
  47. ^ Alvia Gaskill. "Desert Area Coverage". Global Albedo Enhancement Project. http://www.global-warming-geo-engineering.org/Albedo-Enhancement/Surface-Albedo-Enhancement/Calculation-of-Coverage-Areas-to-Achieve-Desired-Level-of-ForcingOffsets/Desert-Area-Coverage/ag28.html. 
  48. ^ http://www.global-warming-geo-engineering.org/Albedo-Enhancement/Surface-Albedo-Enhancement/ag21.html
  49. ^ a b "Solar Radiation Management (GeoEngineering)". http://www.climatechangesask.com/html/learn_more/Solutions/GeoEngineering/Solar_Radiation_Management_/index.cfm. Retrieved 23 April 2011. 
  50. ^ "What is the Great Pacific Garbage Patch?". 21st Century Challenges. http://www.21stcenturychallenges.org/60-seconds/what-is-the-great-pacific-garbage-patch/. Retrieved 23 April 2011. ,
  51. ^ Evans, J.; Stride, E.; Edirisinghe, M.; Andrews, D.; Simons, R. (2010). "Can oceanic foams limit global warming?". Climate Research 42 (2): 155–160. doi:10.3354/cr00885.  edit
  52. ^ http://www.carbonplanet.com/downloads/Climate_Effects_of_Forests_Full.pdf
  53. ^ Hamwey, Robert M. (2005). "Active Amplification of the Terrestrial Albedo to Mitigate Climate Change: An Exploratory Study". Mitigation and Adaptation Strategies for Global Change 12 (4): 419. arXiv:physics/0512170. doi:10.1007/s11027-005-9024-3. 
  54. ^ http://www.newscientist.com/article/dn16428-a-highalbedo-diet-will-chill-the-planet.html
  55. ^ Ridgwell, A; Singarayer, J; Hetherington, A; Valdes, P (2009). "Tackling Regional Climate Change By Leaf Albedo Bio-geoengineering". Current Biology 19 (2): 146–50. doi:10.1016/j.cub.2008.12.025. PMID 19147356. 
  56. ^ David W. Keith (2000). "Geoengineering the climate: History and Prospect". Annual Review of Energy and the Environment 25 (1): 245–284. doi:10.1146/annurev.energy.25.1.245. 
  57. ^ Journal of the British Interplanetary Society, vol 60, p 1
  58. ^ Roger Angel, S. Pete Worden (Summer 2006). "Making Sun-Shades from Moon Dust". National Space Society, Ad Astra 18 (1). http://www.nss.org/adastra/volume18/angel.html. 
  59. ^ LiveScience, Space Ring Could Shade Earth and Stop Global Warming
  60. ^ J. T. Early (1989). "Space-Based Solar Shield To Offset Greenhouse Effect". Journal of the British Interplanetary Society 42: pp. 567–569.  This proposal is also discussed in footnote 23 of Edward Teller; Roderick Hyde, and Lowell Wood (1997) (PDF). Global Warming and Ice Ages: Prospects for Physics-Based Modulation of Global Change. Lawrence Livermore National Laboratory. https://e-reports-ext.llnl.gov/pdf/231636.pdf. Retrieved 2018-10-30. 
  61. ^ See Russell Dovey, "Supervillainy: Astroengineering Global Warming and Bill Christensen, "Reduce Global Warming by Blocking Sunlight".
  62. ^ Gregory Benford (Comments at the 64th World Science Fiction Convention, August 2006.)

Further reading