Young people's burden: requirement of negative CO 2 emissions

International audience Global temperature is a fundamental climate metric highly correlated with sea level, which implies that keeping shorelines near their present location requires keeping global temperature within or close to its preindustrial Holocene range. However, global temperature excluding...

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Published in:Earth System Dynamics
Main Authors: Hansen, James, Sato, Makiko, Kharecha, Pushker, Von Schuckmann, Karina, Beerling, David J., Cao, Junji, Marcott, Shaun, Masson-Delmotte, Valerie, prather, Michael J., Rohling, Eelco J., Shakun, Jeremy, Smith, Pete, Lacis, Andrew, Russell, Gary, Ruedy, Reto
Other Authors: Climate Science, Awareness and Solutions, Columbia University New York, Mercator Océan, Société Civile CNRS Ifremer IRD Météo-France SHOM, Department of Animal and Plant Sciences, University of Sheffield Sheffield, Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE), Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ), Glaces et Continents, Climats et Isotopes Stables (GLACCIOS), Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ), University of California Irvine (UCI), University of California, National Oceanography Centre Southampton (NOC), University of Southampton, Institute of Biological and Environmental Sciences Aberdeen, University of Aberdeen, NASA Goddard Institute for Space Studies (GISS), NASA Goddard Space Flight Center (GSFC), Department of Earth and Environmental Sciences New York
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2017
Subjects:
Online Access:https://hal.archives-ouvertes.fr/hal-01584144
https://hal.archives-ouvertes.fr/hal-01584144/document
https://hal.archives-ouvertes.fr/hal-01584144/file/esd-8-577-2017.pdf
https://doi.org/10.5194/esd-8-577-2017
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op_collection_id ftccsdartic
language English
topic [SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces
environment
spellingShingle [SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces
environment
Hansen, James
Sato, Makiko
Kharecha, Pushker
Von Schuckmann, Karina
Beerling, David J.
Cao, Junji
Marcott, Shaun
Masson-Delmotte, Valerie
prather, Michael J.
Rohling, Eelco J.
Shakun, Jeremy
Smith, Pete
Lacis, Andrew
Russell, Gary
Ruedy, Reto
Young people's burden: requirement of negative CO 2 emissions
topic_facet [SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces
environment
description International audience Global temperature is a fundamental climate metric highly correlated with sea level, which implies that keeping shorelines near their present location requires keeping global temperature within or close to its preindustrial Holocene range. However, global temperature excluding short-term variability now exceeds +1 °C relative to the 1880–1920 mean and annual 2016 global temperature was almost +1.3 °C. We show that global temperature has risen well out of the Holocene range and Earth is now as warm as it was during the prior (Eemian) interglacial period, when sea level reached 6–9 m higher than today. Further, Earth is out of energy balance with present atmospheric composition, implying that more warming is in the pipeline, and we show that the growth rate of greenhouse gas climate forcing has accelerated markedly in the past decade. The rapidity of ice sheet and sea level response to global temperature is difficult to predict, but is dependent on the magnitude of warming. Targets for limiting global warming thus, at minimum, should aim to avoid leaving global temperature at Eemian or higher levels for centuries. Such targets now require "negative emissions", i.e., extraction of CO 2 from the air. If phasedown of fossil fuel emissions begins soon, improved agricultural and forestry practices, including reforestation and steps to improve soil fertility and increase its carbon content, may provide much of the necessary CO 2 extraction. In that case, the magnitude and duration of global temperature excursion above the natural range of the current interglacial (Holocene) could be limited and irreversible climate impacts could be minimized. In contrast, continued high fossil fuel emissions today place a burden on young people to undertake massive technological CO 2 extraction if they are to limit climate change and its consequences. Proposed methods of extraction such as bioenergy with carbon capture and storage (BECCS) or air capture of CO 2 have minimal estimated costs of USD 89–535 trillion ...
author2 Climate Science, Awareness and Solutions
Columbia University New York
Mercator Océan
Société Civile CNRS Ifremer IRD Météo-France SHOM
Department of Animal and Plant Sciences
University of Sheffield Sheffield
Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE)
Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)
Glaces et Continents, Climats et Isotopes Stables (GLACCIOS)
Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)
University of California Irvine (UCI)
University of California
National Oceanography Centre Southampton (NOC)
University of Southampton
Institute of Biological and Environmental Sciences Aberdeen
University of Aberdeen
NASA Goddard Institute for Space Studies (GISS)
NASA Goddard Space Flight Center (GSFC)
Department of Earth and Environmental Sciences New York
format Article in Journal/Newspaper
author Hansen, James
Sato, Makiko
Kharecha, Pushker
Von Schuckmann, Karina
Beerling, David J.
Cao, Junji
Marcott, Shaun
Masson-Delmotte, Valerie
prather, Michael J.
Rohling, Eelco J.
Shakun, Jeremy
Smith, Pete
Lacis, Andrew
Russell, Gary
Ruedy, Reto
author_facet Hansen, James
Sato, Makiko
Kharecha, Pushker
Von Schuckmann, Karina
Beerling, David J.
Cao, Junji
Marcott, Shaun
Masson-Delmotte, Valerie
prather, Michael J.
Rohling, Eelco J.
Shakun, Jeremy
Smith, Pete
Lacis, Andrew
Russell, Gary
Ruedy, Reto
author_sort Hansen, James
title Young people's burden: requirement of negative CO 2 emissions
title_short Young people's burden: requirement of negative CO 2 emissions
title_full Young people's burden: requirement of negative CO 2 emissions
title_fullStr Young people's burden: requirement of negative CO 2 emissions
title_full_unstemmed Young people's burden: requirement of negative CO 2 emissions
title_sort young people's burden: requirement of negative co 2 emissions
publisher HAL CCSD
publishDate 2017
url https://hal.archives-ouvertes.fr/hal-01584144
https://hal.archives-ouvertes.fr/hal-01584144/document
https://hal.archives-ouvertes.fr/hal-01584144/file/esd-8-577-2017.pdf
https://doi.org/10.5194/esd-8-577-2017
genre Ice Sheet
genre_facet Ice Sheet
op_source ISSN: 2190-4979
EISSN: 2190-4987
Earth System Dynamics
https://hal.archives-ouvertes.fr/hal-01584144
Earth System Dynamics, European Geosciences Union, 2017, 8 (3), pp.577 - 616. ⟨10.5194/esd-8-577-2017⟩
https://www.earth-syst-dynam.net/8/577/2017/
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spelling ftccsdartic:oai:HAL:hal-01584144v1 2023-05-15T16:41:35+02:00 Young people's burden: requirement of negative CO 2 emissions Hansen, James Sato, Makiko Kharecha, Pushker Von Schuckmann, Karina Beerling, David J. Cao, Junji Marcott, Shaun Masson-Delmotte, Valerie prather, Michael J. Rohling, Eelco J. Shakun, Jeremy Smith, Pete Lacis, Andrew Russell, Gary Ruedy, Reto Climate Science, Awareness and Solutions Columbia University New York Mercator Océan Société Civile CNRS Ifremer IRD Météo-France SHOM Department of Animal and Plant Sciences University of Sheffield Sheffield Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE) Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ) Glaces et Continents, Climats et Isotopes Stables (GLACCIOS) Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ) University of California Irvine (UCI) University of California National Oceanography Centre Southampton (NOC) University of Southampton Institute of Biological and Environmental Sciences Aberdeen University of Aberdeen NASA Goddard Institute for Space Studies (GISS) NASA Goddard Space Flight Center (GSFC) Department of Earth and Environmental Sciences New York 2017 https://hal.archives-ouvertes.fr/hal-01584144 https://hal.archives-ouvertes.fr/hal-01584144/document https://hal.archives-ouvertes.fr/hal-01584144/file/esd-8-577-2017.pdf https://doi.org/10.5194/esd-8-577-2017 en eng HAL CCSD European Geosciences Union info:eu-repo/semantics/altIdentifier/doi/10.5194/esd-8-577-2017 hal-01584144 https://hal.archives-ouvertes.fr/hal-01584144 https://hal.archives-ouvertes.fr/hal-01584144/document https://hal.archives-ouvertes.fr/hal-01584144/file/esd-8-577-2017.pdf doi:10.5194/esd-8-577-2017 info:eu-repo/semantics/OpenAccess ISSN: 2190-4979 EISSN: 2190-4987 Earth System Dynamics https://hal.archives-ouvertes.fr/hal-01584144 Earth System Dynamics, European Geosciences Union, 2017, 8 (3), pp.577 - 616. ⟨10.5194/esd-8-577-2017⟩ https://www.earth-syst-dynam.net/8/577/2017/ [SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment info:eu-repo/semantics/article Journal articles 2017 ftccsdartic https://doi.org/10.5194/esd-8-577-2017 2021-12-19T00:50:20Z International audience Global temperature is a fundamental climate metric highly correlated with sea level, which implies that keeping shorelines near their present location requires keeping global temperature within or close to its preindustrial Holocene range. However, global temperature excluding short-term variability now exceeds +1 °C relative to the 1880–1920 mean and annual 2016 global temperature was almost +1.3 °C. We show that global temperature has risen well out of the Holocene range and Earth is now as warm as it was during the prior (Eemian) interglacial period, when sea level reached 6–9 m higher than today. Further, Earth is out of energy balance with present atmospheric composition, implying that more warming is in the pipeline, and we show that the growth rate of greenhouse gas climate forcing has accelerated markedly in the past decade. The rapidity of ice sheet and sea level response to global temperature is difficult to predict, but is dependent on the magnitude of warming. Targets for limiting global warming thus, at minimum, should aim to avoid leaving global temperature at Eemian or higher levels for centuries. Such targets now require "negative emissions", i.e., extraction of CO 2 from the air. If phasedown of fossil fuel emissions begins soon, improved agricultural and forestry practices, including reforestation and steps to improve soil fertility and increase its carbon content, may provide much of the necessary CO 2 extraction. In that case, the magnitude and duration of global temperature excursion above the natural range of the current interglacial (Holocene) could be limited and irreversible climate impacts could be minimized. In contrast, continued high fossil fuel emissions today place a burden on young people to undertake massive technological CO 2 extraction if they are to limit climate change and its consequences. Proposed methods of extraction such as bioenergy with carbon capture and storage (BECCS) or air capture of CO 2 have minimal estimated costs of USD 89–535 trillion ... Article in Journal/Newspaper Ice Sheet Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe) Earth System Dynamics 8 3 577 616