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<article language="en">
	<journal>
		<journal_title>Atmospheric Chemistry and Physics Discussions</journal_title>
		<journal_url>www.atmos-chem-phys-discuss.net</journal_url>
		<issn>1680-7367</issn>
		<eissn>1680-7375</eissn>
		<volume_number>9</volume_number>
		<issue_number>1</issue_number>
		<publication_year>2009</publication_year>
	</journal>
	<doi>10.5194/acpd-9-2559-2009</doi>
	<article_url>http://www.atmos-chem-phys-discuss.net/9/2559/2009/</article_url>
	<abstract_html>http://www.atmos-chem-phys-discuss.net/9/2559/2009/acpd-9-2559-2009.html</abstract_html>
	<fulltext_pdf>http://www.atmos-chem-phys-discuss.net/9/2559/2009/acpd-9-2559-2009.pdf</fulltext_pdf>
	<start_page>2559</start_page>
	<end_page>2608</end_page>
	<publication_date>2009-01-28</publication_date>
	<article_title content_type="html">The radiative forcing potential of different climate geoengineering options</article_title>
	<authors>
		<author numeration="1" affiliations="1,2">
			<name>T. M. Lenton</name>
			<email>t.lenton@uea.ac.uk</email>
		</author>
		<author numeration="2" affiliations="1,2">
			<name>N. E. Vaughan</name>
		</author>
	</authors>
	<affiliations>
		<affiliation numeration="1" content_type="html">School of Environmental Sciences, University of East Anglia, Norwich NR4 7TJ, UK</affiliation>
		<affiliation numeration="2" content_type="html">Tyndall Centre for Climate Change Research, UK</affiliation>
	</affiliations>
	<abstract content_type="html">Climate geoengineering proposals seek to rectify the Earth&apos;s current
radiative imbalance, either by reducing the absorption of incoming solar
(shortwave) radiation, or by removing CO&lt;sub&gt;2&lt;/sub&gt; from the atmosphere and
transferring it to long-lived reservoirs, thus increasing outgoing longwave
radiation. A fundamental criterion for evaluating geoengineering options is
their climate cooling effectiveness, which we quantify here in terms of
radiative forcing potential. We use a simple analytical approach, based on
the global energy balance and pulse response functions for the decay of
CO&lt;sub&gt;2&lt;/sub&gt; perturbations. This aids transparency compared to calculations with
complex numerical models, but is not intended to be definitive. Already it
reveals some significant errors in existing calculations, and it allows us to
compare the relative effectiveness of a range of proposals. By 2050, only
stratospheric aerosol injections or sunshades in space have the potential to
cool the climate back toward its pre-industrial state, but some land carbon
cycle geoengineering options are of comparable magnitude to mitigation
&quot;wedges&quot;. Strong mitigation, i.e. large reductions in CO&lt;sub&gt;2&lt;/sub&gt; emissions,
combined with global-scale air capture and storage, afforestation, and
bio-char production, i.e. enhanced CO&lt;sub&gt;2&lt;/sub&gt; sinks, might be able to bring
CO&lt;sub&gt;2&lt;/sub&gt; back to its pre-industrial level by 2100, thus removing the need for
other geoengineering. Alternatively, strong mitigation stabilising CO&lt;sub&gt;2&lt;/sub&gt; at
500 ppm, combined with geoengineered increases in the albedo of marine
stratiform clouds, grasslands, croplands and human settlements might achieve
a patchy cancellation of radiative forcing. Ocean fertilisation options are
only worthwhile if sustained on a millennial timescale and phosphorus
addition probably has greater long-term potential than iron or nitrogen
fertilisation. Enhancing ocean upwelling or downwelling have trivial effects
on any meaningful timescale. Our approach provides a common framework for the
evaluation of climate geoengineering proposals, and our results should help
inform the prioritisation of further research into them.</abstract>
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