Target atmospheric CO2: where should humanity aim?

Paleoclimate data show that climate sensitivity is ~3°C for doubled CO 2 , including only fast feedback processes. Equilibrium sensitivity, including slower surface albedo feedbacks, is ~6°C for doubled CO 2 for the range of climate states between glacial conditions and icefree Antarctica. Decreasin...

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Main Authors: James Hansen, Makiko Sato, Pushker Kharecha, David Beerling, Valerie Masson-Delmotte, Mark Pagani, Maureen Raymo, Dana L Royer, James C Zachos
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Published: 2008
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Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1070.1458
http://climateknowledge.org/figures/Rood_Climate_Change_AOSS480_Documents/Hansen_targetCO2.pdf
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spelling ftciteseerx:oai:CiteSeerX.psu:10.1.1.1070.1458 2023-05-15T13:57:44+02:00 Target atmospheric CO2: where should humanity aim? James Hansen Makiko Sato Pushker Kharecha David Beerling Valerie Masson-Delmotte Mark Pagani Maureen Raymo Dana L Royer James C Zachos The Pennsylvania State University CiteSeerX Archives 2008 application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1070.1458 http://climateknowledge.org/figures/Rood_Climate_Change_AOSS480_Documents/Hansen_targetCO2.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1070.1458 http://climateknowledge.org/figures/Rood_Climate_Change_AOSS480_Documents/Hansen_targetCO2.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://climateknowledge.org/figures/Rood_Climate_Change_AOSS480_Documents/Hansen_targetCO2.pdf text 2008 ftciteseerx 2020-04-26T00:19:58Z Paleoclimate data show that climate sensitivity is ~3°C for doubled CO 2 , including only fast feedback processes. Equilibrium sensitivity, including slower surface albedo feedbacks, is ~6°C for doubled CO 2 for the range of climate states between glacial conditions and icefree Antarctica. Decreasing CO 2 was the main cause of a cooling trend that began 50 million years ago, large scale glaciation occurring when CO 2 fell to 425±75 ppm, a level that will be exceeded within decades, barring prompt policy changes. If humanity wishes to preserve a planet similar to that on which civilization developed and to which life on Earth is adapted, paleoclimate evidence and ongoing climate change suggest that CO 2 will need to be reduced from its current 385 ppm to at most 350 ppm. The largest uncertainty in the target arises from possible changes of non-CO 2 forcings. An initial 350 ppm CO 2 target may be achievable by phasing out coal use except where CO 2 is captured and adopting agricultural and forestry practices that sequester carbon. If the present overshoot of this target CO 2 is not brief, there is a possibility of seeding irreversible catastrophic effects. Human activities are altering Earth's atmospheric composition. Concern about global warming due to long-lived human-made greenhouse gases (GHGs) led to the United Nations Framework Convention on Climate Change (1) with the objective of stabilizing GHGs in the atmosphere at a level preventing "dangerous anthropogenic interference with the climate system." The Intergovernmental Panel on Climate Change (IPCC, 2) and others (3) used several "reasons for concern" to estimate that global warming of more than 2-3°C may be dangerous. The European Union adopted 2°C above pre-industrial global temperature as a goal to limit human-made warming (4). Hansen et al. (5) argued for a limit of 1°C global warming (relative to 2000, 1.7°C relative to pre-industrial time), aiming to avoid practically irreversible ice sheet and species loss. This 1°C limit, with nominal climate ... Text Antarc* Antarctica Ice Sheet Unknown
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description Paleoclimate data show that climate sensitivity is ~3°C for doubled CO 2 , including only fast feedback processes. Equilibrium sensitivity, including slower surface albedo feedbacks, is ~6°C for doubled CO 2 for the range of climate states between glacial conditions and icefree Antarctica. Decreasing CO 2 was the main cause of a cooling trend that began 50 million years ago, large scale glaciation occurring when CO 2 fell to 425±75 ppm, a level that will be exceeded within decades, barring prompt policy changes. If humanity wishes to preserve a planet similar to that on which civilization developed and to which life on Earth is adapted, paleoclimate evidence and ongoing climate change suggest that CO 2 will need to be reduced from its current 385 ppm to at most 350 ppm. The largest uncertainty in the target arises from possible changes of non-CO 2 forcings. An initial 350 ppm CO 2 target may be achievable by phasing out coal use except where CO 2 is captured and adopting agricultural and forestry practices that sequester carbon. If the present overshoot of this target CO 2 is not brief, there is a possibility of seeding irreversible catastrophic effects. Human activities are altering Earth's atmospheric composition. Concern about global warming due to long-lived human-made greenhouse gases (GHGs) led to the United Nations Framework Convention on Climate Change (1) with the objective of stabilizing GHGs in the atmosphere at a level preventing "dangerous anthropogenic interference with the climate system." The Intergovernmental Panel on Climate Change (IPCC, 2) and others (3) used several "reasons for concern" to estimate that global warming of more than 2-3°C may be dangerous. The European Union adopted 2°C above pre-industrial global temperature as a goal to limit human-made warming (4). Hansen et al. (5) argued for a limit of 1°C global warming (relative to 2000, 1.7°C relative to pre-industrial time), aiming to avoid practically irreversible ice sheet and species loss. This 1°C limit, with nominal climate ...
author2 The Pennsylvania State University CiteSeerX Archives
format Text
author James Hansen
Makiko Sato
Pushker Kharecha
David Beerling
Valerie Masson-Delmotte
Mark Pagani
Maureen Raymo
Dana L Royer
James C Zachos
spellingShingle James Hansen
Makiko Sato
Pushker Kharecha
David Beerling
Valerie Masson-Delmotte
Mark Pagani
Maureen Raymo
Dana L Royer
James C Zachos
Target atmospheric CO2: where should humanity aim?
author_facet James Hansen
Makiko Sato
Pushker Kharecha
David Beerling
Valerie Masson-Delmotte
Mark Pagani
Maureen Raymo
Dana L Royer
James C Zachos
author_sort James Hansen
title Target atmospheric CO2: where should humanity aim?
title_short Target atmospheric CO2: where should humanity aim?
title_full Target atmospheric CO2: where should humanity aim?
title_fullStr Target atmospheric CO2: where should humanity aim?
title_full_unstemmed Target atmospheric CO2: where should humanity aim?
title_sort target atmospheric co2: where should humanity aim?
publishDate 2008
url http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.1070.1458
http://climateknowledge.org/figures/Rood_Climate_Change_AOSS480_Documents/Hansen_targetCO2.pdf
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http://climateknowledge.org/figures/Rood_Climate_Change_AOSS480_Documents/Hansen_targetCO2.pdf
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