Optimal Sunshade Configurations for Space-Based Geoengineering near the Sun-Earth L1 Point
Within the context of anthropogenic climate change, but also considering the Earth's natural climate variability, this paper explores the speculative possibility of large-scale active control of the Earth's radiative forcing. In particular, the paper revisits the concept of deploying a lar...
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description | Within the context of anthropogenic climate change, but also considering the Earth's natural climate variability, this paper explores the speculative possibility of large-scale active control of the Earth's radiative forcing. In particular, the paper revisits the concept of deploying a large sunshade or occulting disk at a static position near the Sun-Earth L1 Lagrange equilibrium point. Among the solar radiation management methods that have been proposed thus far, space-based concepts are generally seen as the least timely, albeit also as one of the most efficient. Large occulting structures could potentially offset all of the global mean temperature increase due to greenhouse gas emissions. This paper investigates optimal configurations of orbiting occulting disks that not only offset a global temperature increase, but also mitigate regional differences such as latitudinal and seasonal difference of monthly mean temperature. A globally resolved energy balance model is used to provide insights into the coupling between the motion of the occulting disks and the Earth's climate. This allows us to revise previous studies, but also, for the first time, to search for families of orbits that improve the efficiency of occulting disks at offsetting climate change on both global and regional scales. Although natural orbits exist near the L1 equilibrium point, their period does not match that required for geoengineering purposes, thus forced orbits were designed that require small changes to the disk attitude in order to control its motion. Finally, configurations of two occulting disks are presented which provide the same shading area as previously published studies, but achieve reductions of residual latitudinal and seasonal temperature changes. |
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In particular, the paper revisits the concept of deploying a large sunshade or occulting disk at a static position near the Sun-Earth L1 Lagrange equilibrium point. Among the solar radiation management methods that have been proposed thus far, space-based concepts are generally seen as the least timely, albeit also as one of the most efficient. Large occulting structures could potentially offset all of the global mean temperature increase due to greenhouse gas emissions. This paper investigates optimal configurations of orbiting occulting disks that not only offset a global temperature increase, but also mitigate regional differences such as latitudinal and seasonal difference of monthly mean temperature. A globally resolved energy balance model is used to provide insights into the coupling between the motion of the occulting disks and the Earth's climate. This allows us to revise previous studies, but also, for the first time, to search for families of orbits that improve the efficiency of occulting disks at offsetting climate change on both global and regional scales. Although natural orbits exist near the L1 equilibrium point, their period does not match that required for geoengineering purposes, thus forced orbits were designed that require small changes to the disk attitude in order to control its motion. Finally, configurations of two occulting disks are presented which provide the same shading area as previously published studies, but achieve reductions of residual latitudinal and seasonal temperature changes.</description><identifier>ISSN: 1932-6203</identifier><identifier>EISSN: 1932-6203</identifier><identifier>DOI: 10.1371/journal.pone.0136648</identifier><identifier>PMID: 26309047</identifier><language>eng</language><publisher>United States: Public Library of Science</publisher><subject>Active control ; Anthropogenic climate changes ; Anthropogenic factors ; Astronauts ; Carbon dioxide ; Carbon dioxide removal ; Civil engineering ; Climate change ; Climate variability ; Climatic variability ; Collection Review ; Configurations ; Disks ; Earth ; Earth (Planet) ; Emissions ; Energy balance ; Engineering - methods ; Equilibrium ; General circulation models ; Geoengineering ; Geology ; Global temperatures ; Greenhouse Effect ; Greenhouse gases ; Management methods ; Mean temperatures ; Orbits ; Radiative forcing ; Shading ; Solar Activity ; Solar radiation ; Sun ; Sunlight ; Temperature ; Temperature changes ; Temperature effects ; Temperature rise</subject><ispartof>PloS one, 2015-08, Vol.10 (8), p.e0136648-e0136648</ispartof><rights>2015 Sánchez, McInnes. This is an open access article distributed under the terms of the Creative Commons Attribution License: http://creativecommons.org/licenses/by/4.0/ (the “License”), which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited Notwithstanding the ProQuest Terms and Conditions, you may use this content in accordance with the terms of the License.</rights><rights>2015 Sánchez, McInnes 2015 Sánchez, McInnes</rights><lds50>peer_reviewed</lds50><oa>free_for_read</oa><woscitedreferencessubscribed>false</woscitedreferencessubscribed><citedby>FETCH-LOGICAL-c4418-2889f27a8ac1bbcee078f2640e6775db8b17629464b40d2bd87ebb5f4beed1713</citedby><cites>FETCH-LOGICAL-c4418-2889f27a8ac1bbcee078f2640e6775db8b17629464b40d2bd87ebb5f4beed1713</cites></display><links><openurl>$$Topenurl_article</openurl><openurlfulltext>$$Topenurlfull_article</openurlfulltext><thumbnail>$$Tsyndetics_thumb_exl</thumbnail><linktopdf>$$Uhttps://www.ncbi.nlm.nih.gov/pmc/articles/PMC4550401/pdf/$$EPDF$$P50$$Gpubmedcentral$$Hfree_for_read</linktopdf><linktohtml>$$Uhttps://www.ncbi.nlm.nih.gov/pmc/articles/PMC4550401/$$EHTML$$P50$$Gpubmedcentral$$Hfree_for_read</linktohtml><link.rule.ids>230,314,723,776,780,860,881,2096,2915,23845,27901,27902,53766,53768,79569,79570</link.rule.ids><backlink>$$Uhttps://www.ncbi.nlm.nih.gov/pubmed/26309047$$D View this record in MEDLINE/PubMed$$Hfree_for_read</backlink></links><search><creatorcontrib>Sánchez, Joan-Pau</creatorcontrib><creatorcontrib>McInnes, Colin R</creatorcontrib><title>Optimal Sunshade Configurations for Space-Based Geoengineering near the Sun-Earth L1 Point</title><title>PloS one</title><addtitle>PLoS One</addtitle><description>Within the context of anthropogenic climate change, but also considering the Earth's natural climate variability, this paper explores the speculative possibility of large-scale active control of the Earth's radiative forcing. In particular, the paper revisits the concept of deploying a large sunshade or occulting disk at a static position near the Sun-Earth L1 Lagrange equilibrium point. Among the solar radiation management methods that have been proposed thus far, space-based concepts are generally seen as the least timely, albeit also as one of the most efficient. Large occulting structures could potentially offset all of the global mean temperature increase due to greenhouse gas emissions. This paper investigates optimal configurations of orbiting occulting disks that not only offset a global temperature increase, but also mitigate regional differences such as latitudinal and seasonal difference of monthly mean temperature. A globally resolved energy balance model is used to provide insights into the coupling between the motion of the occulting disks and the Earth's climate. This allows us to revise previous studies, but also, for the first time, to search for families of orbits that improve the efficiency of occulting disks at offsetting climate change on both global and regional scales. Although natural orbits exist near the L1 equilibrium point, their period does not match that required for geoengineering purposes, thus forced orbits were designed that require small changes to the disk attitude in order to control its motion. Finally, configurations of two occulting disks are presented which provide the same shading area as previously published studies, but achieve reductions of residual latitudinal and seasonal temperature changes.</description><subject>Active control</subject><subject>Anthropogenic climate changes</subject><subject>Anthropogenic factors</subject><subject>Astronauts</subject><subject>Carbon dioxide</subject><subject>Carbon dioxide removal</subject><subject>Civil engineering</subject><subject>Climate change</subject><subject>Climate variability</subject><subject>Climatic variability</subject><subject>Collection Review</subject><subject>Configurations</subject><subject>Disks</subject><subject>Earth</subject><subject>Earth (Planet)</subject><subject>Emissions</subject><subject>Energy balance</subject><subject>Engineering - methods</subject><subject>Equilibrium</subject><subject>General circulation models</subject><subject>Geoengineering</subject><subject>Geology</subject><subject>Global temperatures</subject><subject>Greenhouse Effect</subject><subject>Greenhouse gases</subject><subject>Management methods</subject><subject>Mean temperatures</subject><subject>Orbits</subject><subject>Radiative forcing</subject><subject>Shading</subject><subject>Solar Activity</subject><subject>Solar radiation</subject><subject>Sun</subject><subject>Sunlight</subject><subject>Temperature</subject><subject>Temperature changes</subject><subject>Temperature effects</subject><subject>Temperature 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Sunshade Configurations for Space-Based Geoengineering near the Sun-Earth L1 Point</atitle><jtitle>PloS one</jtitle><addtitle>PLoS One</addtitle><date>2015-08-26</date><risdate>2015</risdate><volume>10</volume><issue>8</issue><spage>e0136648</spage><epage>e0136648</epage><pages>e0136648-e0136648</pages><issn>1932-6203</issn><eissn>1932-6203</eissn><abstract>Within the context of anthropogenic climate change, but also considering the Earth's natural climate variability, this paper explores the speculative possibility of large-scale active control of the Earth's radiative forcing. In particular, the paper revisits the concept of deploying a large sunshade or occulting disk at a static position near the Sun-Earth L1 Lagrange equilibrium point. Among the solar radiation management methods that have been proposed thus far, space-based concepts are generally seen as the least timely, albeit also as one of the most efficient. Large occulting structures could potentially offset all of the global mean temperature increase due to greenhouse gas emissions. This paper investigates optimal configurations of orbiting occulting disks that not only offset a global temperature increase, but also mitigate regional differences such as latitudinal and seasonal difference of monthly mean temperature. A globally resolved energy balance model is used to provide insights into the coupling between the motion of the occulting disks and the Earth's climate. This allows us to revise previous studies, but also, for the first time, to search for families of orbits that improve the efficiency of occulting disks at offsetting climate change on both global and regional scales. Although natural orbits exist near the L1 equilibrium point, their period does not match that required for geoengineering purposes, thus forced orbits were designed that require small changes to the disk attitude in order to control its motion. Finally, configurations of two occulting disks are presented which provide the same shading area as previously published studies, but achieve reductions of residual latitudinal and seasonal temperature changes.</abstract><cop>United States</cop><pub>Public Library of Science</pub><pmid>26309047</pmid><doi>10.1371/journal.pone.0136648</doi><oa>free_for_read</oa></addata></record> |
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subjects | Active control Anthropogenic climate changes Anthropogenic factors Astronauts Carbon dioxide Carbon dioxide removal Civil engineering Climate change Climate variability Climatic variability Collection Review Configurations Disks Earth Earth (Planet) Emissions Energy balance Engineering - methods Equilibrium General circulation models Geoengineering Geology Global temperatures Greenhouse Effect Greenhouse gases Management methods Mean temperatures Orbits Radiative forcing Shading Solar Activity Solar radiation Sun Sunlight Temperature Temperature changes Temperature effects Temperature rise |
title | Optimal Sunshade Configurations for Space-Based Geoengineering near the Sun-Earth L1 Point |
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