The effects of rerouting aircraft around the arctic circle on arctic and global climate

Climate data suggest greater warming over the Arctic than lower latitudes, and the most abundant direct source of black carbon and other climate-relevant pollutants over the Arctic is cross-polar flights by international aviation. A relevant question is whether rerouting cross-polar flights to circu...

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Main Authors: Mark Jacobson, Jordan Wilkerson, Sathya Balasubramanian, Wayne Cooper, Nina Mohleji
Format: Article in Journal/Newspaper
Language:unknown
Subjects:
Online Access:http://hdl.handle.net/10.1007/s10584-012-0462-0
id ftrepec:oai:RePEc:spr:climat:v:115:y:2012:i:3:p:709-724
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spelling ftrepec:oai:RePEc:spr:climat:v:115:y:2012:i:3:p:709-724 2023-05-15T14:32:22+02:00 The effects of rerouting aircraft around the arctic circle on arctic and global climate Mark Jacobson Jordan Wilkerson Sathya Balasubramanian Wayne Cooper Nina Mohleji http://hdl.handle.net/10.1007/s10584-012-0462-0 unknown http://hdl.handle.net/10.1007/s10584-012-0462-0 article ftrepec 2020-12-04T13:33:09Z Climate data suggest greater warming over the Arctic than lower latitudes, and the most abundant direct source of black carbon and other climate-relevant pollutants over the Arctic is cross-polar flights by international aviation. A relevant question is whether rerouting cross-polar flights to circumnavigate the Arctic Circle reduces or enhances such warming. To study this issue, a model accounting for subgrid exhaust plumes from each individual commercial flight worldwide was used with 2006 global aircraft emission inventories that treated cross-polar flights and flights rerouted around the Arctic Circle (66.56083 °N), respectively. Rerouting increased fuel use by 0.056 % in the global average, mostly right outside the Arctic Circle, but most of the associated black carbon and other emissions were removed faster because they were now over latitudes of greater precipitation and lesser stability. Rerouting also reduced fuel use and emissions within the Arctic Circle by 83 % and delayed pollutant transport to the Arctic. The Arctic reduction in pollutants, particularly of black carbon, decreased Arctic and global temperature and increased Arctic sea ice over 22 years. Although the slight increase in total CO 2 emissions due to rerouting may dampen the benefit of rerouting over more decades, rerouting or even partial rerouting (allowing cross-polar flights during polar night only) may delay the elimination of Arctic sea ice, which will otherwise likely occur within the next 2–3 decades due to global warming in general. Rerouting may increase worldwide fuel plus operational costs by only ~$99 million/yr, 47–55 times less than an estimated 2025 U.S.-alone cost savings due to the global warming reduction from rerouting. Copyright Springer Science+Business Media B.V. 2012 Article in Journal/Newspaper Arctic black carbon Global warming polar night Sea ice RePEc (Research Papers in Economics) Arctic
institution Open Polar
collection RePEc (Research Papers in Economics)
op_collection_id ftrepec
language unknown
description Climate data suggest greater warming over the Arctic than lower latitudes, and the most abundant direct source of black carbon and other climate-relevant pollutants over the Arctic is cross-polar flights by international aviation. A relevant question is whether rerouting cross-polar flights to circumnavigate the Arctic Circle reduces or enhances such warming. To study this issue, a model accounting for subgrid exhaust plumes from each individual commercial flight worldwide was used with 2006 global aircraft emission inventories that treated cross-polar flights and flights rerouted around the Arctic Circle (66.56083 °N), respectively. Rerouting increased fuel use by 0.056 % in the global average, mostly right outside the Arctic Circle, but most of the associated black carbon and other emissions were removed faster because they were now over latitudes of greater precipitation and lesser stability. Rerouting also reduced fuel use and emissions within the Arctic Circle by 83 % and delayed pollutant transport to the Arctic. The Arctic reduction in pollutants, particularly of black carbon, decreased Arctic and global temperature and increased Arctic sea ice over 22 years. Although the slight increase in total CO 2 emissions due to rerouting may dampen the benefit of rerouting over more decades, rerouting or even partial rerouting (allowing cross-polar flights during polar night only) may delay the elimination of Arctic sea ice, which will otherwise likely occur within the next 2–3 decades due to global warming in general. Rerouting may increase worldwide fuel plus operational costs by only ~$99 million/yr, 47–55 times less than an estimated 2025 U.S.-alone cost savings due to the global warming reduction from rerouting. Copyright Springer Science+Business Media B.V. 2012
format Article in Journal/Newspaper
author Mark Jacobson
Jordan Wilkerson
Sathya Balasubramanian
Wayne Cooper
Nina Mohleji
spellingShingle Mark Jacobson
Jordan Wilkerson
Sathya Balasubramanian
Wayne Cooper
Nina Mohleji
The effects of rerouting aircraft around the arctic circle on arctic and global climate
author_facet Mark Jacobson
Jordan Wilkerson
Sathya Balasubramanian
Wayne Cooper
Nina Mohleji
author_sort Mark Jacobson
title The effects of rerouting aircraft around the arctic circle on arctic and global climate
title_short The effects of rerouting aircraft around the arctic circle on arctic and global climate
title_full The effects of rerouting aircraft around the arctic circle on arctic and global climate
title_fullStr The effects of rerouting aircraft around the arctic circle on arctic and global climate
title_full_unstemmed The effects of rerouting aircraft around the arctic circle on arctic and global climate
title_sort effects of rerouting aircraft around the arctic circle on arctic and global climate
url http://hdl.handle.net/10.1007/s10584-012-0462-0
geographic Arctic
geographic_facet Arctic
genre Arctic
black carbon
Global warming
polar night
Sea ice
genre_facet Arctic
black carbon
Global warming
polar night
Sea ice
op_relation http://hdl.handle.net/10.1007/s10584-012-0462-0
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