Science 7 May
2010:
Vol. 328. no. 5979, pp. 690 - 691
DOI: 10.1126/science.328.5979.690-a
Letters
Shifting the Debate on
Geoengineering
As discussed in the recent Policy
Forum "The politics of geoengineering" (J. J. Blackstock and
J. C. S. Long, 29 January, p. 527),
there is growing recognition that avoiding dangerous climate change
during the 21st century may require society to adopt geoengineering
technologies to supplement CO2 emission reduction efforts.
Unfortunately, despite the essential role that CO2 removal (CDR) and
solar radiation management (SRM) technologies may play in reducing the
risks of dangerous climate change, discussions of the necessary
research and development [including the Policy Forum and others
(1, 2)] frequently turn into debates about the
environmental costs and benefits of SRM. A more productive approach
would shift the debate to comparing the relative costs and benefits of
CDR and SRM.
CDR approaches are frequently
discounted because, as Blackstock and Long explain, "technical
challenges and large uncertainties [surround] large-scale CDR
deployment." Although this may be true for human-built systems
that capture CO2 from air at ambient concentrations, there are other
technologies based on biological carbon fixation that could be
fast-tracked for rapid deployment during the next few decades (3). Most major international energy corporations
are investing in algal-based biofuel technologies because of the
tremendous production potential of algae relative to terrestrial
energy crops (4). Commercial-scale production of algal
biofuels will begin during the next 5 years, and rapid scaling up can
be expected afterward if the economic incentives are favorable.
However, becoming carbon negative will require society to develop
plans for retrofitting existing coal-fired power plants and building
future ones so that they can burn algal biomass and capture the
emitted CO2 for subsequent sequestration. The basic technologies
described here are not novel; rather, I am proposing a conceptual
rearrangement that may enable society to transition more gracefully
from fossil to modern carbon fuel sources while simultaneously
reducing CO2 levels in the atmosphere and ocean.
Charles H.
Greene
Department of Earth and
Atmospheric Sciences, Cornell University, Ithaca, NY 14853,
USA.
References
- 1. A. Robock et al.,
Science 327, 530 (2010).[Abstract/Free Full Text]
- 2. D. W. Keith, E. Parson, M. G.
Morgan, Nature 463, 426 (2010).[CrossRef][Web of Science][Medline]
- 3. D. W. Keith, M. Ha-Duong, J. K.
Stollaroff, Climat. Change 74, 17 (2006).[CrossRef]
- 4. M. E. Huntley, D. G. Redalje,
Mitigation Adapt. Strategies Global Change 12, 573
(2007).[CrossRef]