AustralieFrV1, PascalFrancis, Corpus, bibRecord, 000664

Attributing the increase in atmospheric CO2 to emitters and absorbers

Identifieur interne : 000664 ( PascalFrancis/Corpus ); précédent : 000663; suivant : 000665

Attributing the increase in atmospheric CO2 to emitters and absorbers

Auteurs : P. Ciais ; T. Gasser ; J. D. Paris ; K. Caldeira ; M. R. Raupach ; J. G. Canadell ; A. Patwardhan ; P. Friedlingstein ; S. L. Piao ; V. Gitz

Source :

Nature climate change : (Print) [ 1758-678X ] ; 2013.

RBID : Francis:14-0180070

Descripteurs français

Pascal (Inist)
- Dioxyde de carbone, Facteur anthropique, Activité humaine, Changement climatique, Equité, Tiers Monde, Pays industrialisé, Relation source puits, Gaz effet serre, Développement durable, Réchauffement climat, Changement planétaire, Mitigation, Politique du climat.

English descriptors

KwdEn :
- Anthropogenic factor, Carbon dioxide, Climate policy, Equity, Human activity, Mitigation, Source sink relationship, Third World, climate change, climate warming, global change, greenhouse gas, industrialized countries, sustainable development.

Abstract

Climate change policies need to consider the contribution of each emitting region to the increase in atmospheric carbon dioxide. We calculate regional attributions of increased atmospheric CO₂ using two different assumptions about land sinks. In the first approach, each absorber region is attributed 'domestic sinks' that occur within its boundaries. In the second, alternative approach, each emitter region is attributed 'foreign sinks' that it created indirectly through its contribution to increasing CO₂. We unambiguously attribute the largest share of the historical increase in CO₂ between pre-industrial times and the present-day period to developed countries. However, the excess CO₂ in the atmosphere since pre-industrial times attributed to developing countries is greater than their share of cumulative CO₂ emissions. This is because a greater fraction of their emissions occurred more recently. If emissions remain high over the coming decades, the share of excess CO₂ attributable to developing countries will grow, and the sink service provided by forested regions-in particular those with tropical forest-to other regions will depend critically on future tropical land-use change.

Notice en format standard (ISO 2709)

Pour connaître la documentation sur le format Inist Standard.

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Format Inist (serveur)

NO :	FRANCIS 14-0180070 INIST
ET :	Attributing the increase in atmospheric CO₂ to emitters and absorbers
AU :	CIAIS (P.); GASSER (T.); PARIS (J. D.); CALDEIRA (K.); RAUPACH (M. R.); CANADELL (J. G.); PATWARDHAN (A.); FRIEDLINGSTEIN (P.); PIAO (S. L.); GITZ (V.)
AF :	Laboratoire des Sciences du Climat et de l'Environnement, CEA-CNRS-UVSQ, CE l'Orme des Merisiers/91191 Gif sur Yvette/France (1 aut., 2 aut., 3 aut.); Department of Ecology, College of Urban and Environmental Science, Peking University/Beijing 100871/Chine (1 aut., 9 aut.); Carnegie Institution Department of Global Ecology, 260 Panama Street/Stanford, California 94305/Etats-Unis (4 aut.); Global Carbon Project, CSIRO Marine and Atmospheric Research/Canberra, Australian Capital Territory 2601/Australie (5 aut., 6 aut.); S J Mehta School of Management, Indian Institute of Technology/Powai, 400076 Mumbai/Inde (7 aut.); College of Engineering, Mathematics and Physical Sciences, University of Exeter/Exeter EX4 4QF/Royaume-Uni (8 aut.); Institute of Tibetan Plateau Research, Chinese Academy of Sciences/Beijing 100085/Chine (9 aut.); Centre International de Recherche sur l'Environnement et le Développèment, CNRS-CIRAD-ParisTech-EHESS 45 bis avenue de la Belle Gabrielle/94736 Nogent Sur Marne/France (10 aut.)
DT :	Publication en série; Niveau analytique
SO :	Nature climate change : (Print); ISSN 1758-678X; Royaume-Uni; Da. 2013; Vol. 3; No. 10; Pp. 926-930; Bibl. 28 ref.
LA :	Anglais
EA :	Climate change policies need to consider the contribution of each emitting region to the increase in atmospheric carbon dioxide. We calculate regional attributions of increased atmospheric CO₂ using two different assumptions about land sinks. In the first approach, each absorber region is attributed 'domestic sinks' that occur within its boundaries. In the second, alternative approach, each emitter region is attributed 'foreign sinks' that it created indirectly through its contribution to increasing CO₂. We unambiguously attribute the largest share of the historical increase in CO₂ between pre-industrial times and the present-day period to developed countries. However, the excess CO₂ in the atmosphere since pre-industrial times attributed to developing countries is greater than their share of cumulative CO₂ emissions. This is because a greater fraction of their emissions occurred more recently. If emissions remain high over the coming decades, the share of excess CO₂ attributable to developing countries will grow, and the sink service provided by forested regions-in particular those with tropical forest-to other regions will depend critically on future tropical land-use change.
CC :	52118; 521
FD :	Dioxyde de carbone; Facteur anthropique; Activité humaine; Changement climatique; Equité; Tiers Monde; Pays industrialisé; Relation source puits; Gaz effet serre; Développement durable; Réchauffement climat; Changement planétaire; Mitigation; Politique du climat
ED :	Carbon dioxide; Anthropogenic factor; Human activity; climate change; Equity; Third World; industrialized countries; Source sink relationship; greenhouse gas; sustainable development; climate warming; global change; Mitigation; Climate policy
SD :	Carbono dióxido; Factor antrópico; Actividad humana; Equidad; País industrializado; Relación fuente sumidero; Cambio planetario; Política del clima
LO :	INIST-28118.354000505894240200
ID :	14-0180070

Links to Exploration step

Francis:14-0180070

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<term>Mitigation</term>
<term>Source sink relationship</term>
<term>Third World</term>
<term>climate change</term>
<term>climate warming</term>
<term>global change</term>
<term>greenhouse gas</term>
<term>industrialized countries</term>
<term>sustainable development</term>
</keywords>
<keywords scheme="Pascal" xml:lang="fr"><term>Dioxyde de carbone</term>
<term>Facteur anthropique</term>
<term>Activité humaine</term>
<term>Changement climatique</term>
<term>Equité</term>
<term>Tiers Monde</term>
<term>Pays industrialisé</term>
<term>Relation source puits</term>
<term>Gaz effet serre</term>
<term>Développement durable</term>
<term>Réchauffement climat</term>
<term>Changement planétaire</term>
<term>Mitigation</term>
<term>Politique du climat</term>
</keywords>
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<front><div type="abstract" xml:lang="en">Climate change policies need to consider the contribution of each emitting region to the increase in atmospheric carbon dioxide. We calculate regional attributions of increased atmospheric CO<sub>2</sub>
 using two different assumptions about land sinks. In the first approach, each absorber region is attributed 'domestic sinks' that occur within its boundaries. In the second, alternative approach, each emitter region is attributed 'foreign sinks' that it created indirectly through its contribution to increasing CO<sub>2</sub>
. We unambiguously attribute the largest share of the historical increase in CO<sub>2</sub>
 between pre-industrial times and the present-day period to developed countries. However, the excess CO<sub>2</sub>
 in the atmosphere since pre-industrial times attributed to developing countries is greater than their share of cumulative CO<sub>2</sub>
 emissions. This is because a greater fraction of their emissions occurred more recently. If emissions remain high over the coming decades, the share of excess CO<sub>2</sub>
 attributable to developing countries will grow, and the sink service provided by forested regions-in particular those with tropical forest-to other regions will depend critically on future tropical land-use change.</div>
</front>
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<inist><standard h6="B"><pA><fA01 i1="01" i2="1"><s0>1758-678X</s0>
</fA01>
<fA03 i2="1"><s0>Nat. clim. chang. : (Print)</s0>
</fA03>
<fA05><s2>3</s2>
</fA05>
<fA06><s2>10</s2>
</fA06>
<fA08 i1="01" i2="1" l="ENG"><s1>Attributing the increase in atmospheric CO<sub>2</sub>
 to emitters and absorbers</s1>
</fA08>
<fA11 i1="01" i2="1"><s1>CIAIS (P.)</s1>
</fA11>
<fA11 i1="02" i2="1"><s1>GASSER (T.)</s1>
</fA11>
<fA11 i1="03" i2="1"><s1>PARIS (J. D.)</s1>
</fA11>
<fA11 i1="04" i2="1"><s1>CALDEIRA (K.)</s1>
</fA11>
<fA11 i1="05" i2="1"><s1>RAUPACH (M. R.)</s1>
</fA11>
<fA11 i1="06" i2="1"><s1>CANADELL (J. G.)</s1>
</fA11>
<fA11 i1="07" i2="1"><s1>PATWARDHAN (A.)</s1>
</fA11>
<fA11 i1="08" i2="1"><s1>FRIEDLINGSTEIN (P.)</s1>
</fA11>
<fA11 i1="09" i2="1"><s1>PIAO (S. L.)</s1>
</fA11>
<fA11 i1="10" i2="1"><s1>GITZ (V.)</s1>
</fA11>
<fA14 i1="01"><s1>Laboratoire des Sciences du Climat et de l'Environnement, CEA-CNRS-UVSQ, CE l'Orme des Merisiers</s1>
<s2>91191 Gif sur Yvette</s2>
<s3>FRA</s3>
<sZ>1 aut.</sZ>
<sZ>2 aut.</sZ>
<sZ>3 aut.</sZ>
</fA14>
<fA14 i1="02"><s1>Department of Ecology, College of Urban and Environmental Science, Peking University</s1>
<s2>Beijing 100871</s2>
<s3>CHN</s3>
<sZ>1 aut.</sZ>
<sZ>9 aut.</sZ>
</fA14>
<fA14 i1="03"><s1>Carnegie Institution Department of Global Ecology, 260 Panama Street</s1>
<s2>Stanford, California 94305</s2>
<s3>USA</s3>
<sZ>4 aut.</sZ>
</fA14>
<fA14 i1="04"><s1>Global Carbon Project, CSIRO Marine and Atmospheric Research</s1>
<s2>Canberra, Australian Capital Territory 2601</s2>
<s3>AUS</s3>
<sZ>5 aut.</sZ>
<sZ>6 aut.</sZ>
</fA14>
<fA14 i1="05"><s1>S J Mehta School of Management, Indian Institute of Technology</s1>
<s2>Powai, 400076 Mumbai</s2>
<s3>IND</s3>
<sZ>7 aut.</sZ>
</fA14>
<fA14 i1="06"><s1>College of Engineering, Mathematics and Physical Sciences, University of Exeter</s1>
<s2>Exeter EX4 4QF</s2>
<s3>GBR</s3>
<sZ>8 aut.</sZ>
</fA14>
<fA14 i1="07"><s1>Institute of Tibetan Plateau Research, Chinese Academy of Sciences</s1>
<s2>Beijing 100085</s2>
<s3>CHN</s3>
<sZ>9 aut.</sZ>
</fA14>
<fA14 i1="08"><s1>Centre International de Recherche sur l'Environnement et le Développèment, CNRS-CIRAD-ParisTech-EHESS 45 bis avenue de la Belle Gabrielle</s1>
<s2>94736 Nogent Sur Marne</s2>
<s3>FRA</s3>
<sZ>10 aut.</sZ>
</fA14>
<fA20><s1>926-930</s1>
</fA20>
<fA21><s1>2013</s1>
</fA21>
<fA23 i1="01"><s0>ENG</s0>
</fA23>
<fA43 i1="01"><s1>INIST</s1>
<s2>28118</s2>
<s5>354000505894240200</s5>
</fA43>
<fA44><s0>0000</s0>
<s1>© 2014 INIST-CNRS. All rights reserved.</s1>
</fA44>
<fA45><s0>28 ref.</s0>
</fA45>
<fA47 i1="01" i2="1"><s0>14-0180070</s0>
</fA47>
<fA60><s1>P</s1>
</fA60>
<fA61><s0>A</s0>
</fA61>
<fA64 i1="01" i2="1"><s0>Nature climate change : (Print)</s0>
</fA64>
<fA66 i1="01"><s0>GBR</s0>
</fA66>
<fC01 i1="01" l="ENG"><s0>Climate change policies need to consider the contribution of each emitting region to the increase in atmospheric carbon dioxide. We calculate regional attributions of increased atmospheric CO<sub>2</sub>
 using two different assumptions about land sinks. In the first approach, each absorber region is attributed 'domestic sinks' that occur within its boundaries. In the second, alternative approach, each emitter region is attributed 'foreign sinks' that it created indirectly through its contribution to increasing CO<sub>2</sub>
. We unambiguously attribute the largest share of the historical increase in CO<sub>2</sub>
 between pre-industrial times and the present-day period to developed countries. However, the excess CO<sub>2</sub>
 in the atmosphere since pre-industrial times attributed to developing countries is greater than their share of cumulative CO<sub>2</sub>
 emissions. This is because a greater fraction of their emissions occurred more recently. If emissions remain high over the coming decades, the share of excess CO<sub>2</sub>
 attributable to developing countries will grow, and the sink service provided by forested regions-in particular those with tropical forest-to other regions will depend critically on future tropical land-use change.</s0>
</fC01>
<fC02 i1="01" i2="S"><s0>52118</s0>
<s1>IV</s1>
</fC02>
<fC02 i1="02" i2="S"><s0>521</s0>
</fC02>
<fC03 i1="01" i2="X" l="FRE"><s0>Dioxyde de carbone</s0>
<s2>NK</s2>
<s2>FX</s2>
<s5>01</s5>
</fC03>
<fC03 i1="01" i2="X" l="ENG"><s0>Carbon dioxide</s0>
<s2>NK</s2>
<s2>FX</s2>
<s5>01</s5>
</fC03>
<fC03 i1="01" i2="X" l="SPA"><s0>Carbono dióxido</s0>
<s2>NK</s2>
<s2>FX</s2>
<s5>01</s5>
</fC03>
<fC03 i1="02" i2="X" l="FRE"><s0>Facteur anthropique</s0>
<s5>02</s5>
</fC03>
<fC03 i1="02" i2="X" l="ENG"><s0>Anthropogenic factor</s0>
<s5>02</s5>
</fC03>
<fC03 i1="02" i2="X" l="SPA"><s0>Factor antrópico</s0>
<s5>02</s5>
</fC03>
<fC03 i1="03" i2="X" l="FRE"><s0>Activité humaine</s0>
<s5>03</s5>
</fC03>
<fC03 i1="03" i2="X" l="ENG"><s0>Human activity</s0>
<s5>03</s5>
</fC03>
<fC03 i1="03" i2="X" l="SPA"><s0>Actividad humana</s0>
<s5>03</s5>
</fC03>
<fC03 i1="04" i2="2" l="FRE"><s0>Changement climatique</s0>
<s5>04</s5>
</fC03>
<fC03 i1="04" i2="2" l="ENG"><s0>climate change</s0>
<s5>04</s5>
</fC03>
<fC03 i1="05" i2="X" l="FRE"><s0>Equité</s0>
<s5>05</s5>
</fC03>
<fC03 i1="05" i2="X" l="ENG"><s0>Equity</s0>
<s5>05</s5>
</fC03>
<fC03 i1="05" i2="X" l="SPA"><s0>Equidad</s0>
<s5>05</s5>
</fC03>
<fC03 i1="06" i2="2" l="FRE"><s0>Tiers Monde</s0>
<s5>06</s5>
</fC03>
<fC03 i1="06" i2="2" l="ENG"><s0>Third World</s0>
<s5>06</s5>
</fC03>
<fC03 i1="07" i2="2" l="FRE"><s0>Pays industrialisé</s0>
<s5>07</s5>
</fC03>
<fC03 i1="07" i2="2" l="ENG"><s0>industrialized countries</s0>
<s5>07</s5>
</fC03>
<fC03 i1="07" i2="2" l="SPA"><s0>País industrializado</s0>
<s5>07</s5>
</fC03>
<fC03 i1="08" i2="X" l="FRE"><s0>Relation source puits</s0>
<s5>08</s5>
</fC03>
<fC03 i1="08" i2="X" l="ENG"><s0>Source sink relationship</s0>
<s5>08</s5>
</fC03>
<fC03 i1="08" i2="X" l="SPA"><s0>Relación fuente sumidero</s0>
<s5>08</s5>
</fC03>
<fC03 i1="09" i2="2" l="FRE"><s0>Gaz effet serre</s0>
<s5>41</s5>
</fC03>
<fC03 i1="09" i2="2" l="ENG"><s0>greenhouse gas</s0>
<s5>41</s5>
</fC03>
<fC03 i1="10" i2="2" l="FRE"><s0>Développement durable</s0>
<s5>43</s5>
</fC03>
<fC03 i1="10" i2="2" l="ENG"><s0>sustainable development</s0>
<s5>43</s5>
</fC03>
<fC03 i1="11" i2="2" l="FRE"><s0>Réchauffement climat</s0>
<s5>44</s5>
</fC03>
<fC03 i1="11" i2="2" l="ENG"><s0>climate warming</s0>
<s5>44</s5>
</fC03>
<fC03 i1="12" i2="2" l="FRE"><s0>Changement planétaire</s0>
<s5>45</s5>
</fC03>
<fC03 i1="12" i2="2" l="ENG"><s0>global change</s0>
<s5>45</s5>
</fC03>
<fC03 i1="12" i2="2" l="SPA"><s0>Cambio planetario</s0>
<s5>45</s5>
</fC03>
<fC03 i1="13" i2="3" l="FRE"><s0>Mitigation</s0>
<s5>46</s5>
</fC03>
<fC03 i1="13" i2="3" l="ENG"><s0>Mitigation</s0>
<s5>46</s5>
</fC03>
<fC03 i1="14" i2="2" l="FRE"><s0>Politique du climat</s0>
<s4>CD</s4>
<s5>96</s5>
</fC03>
<fC03 i1="14" i2="2" l="ENG"><s0>Climate policy</s0>
<s4>CD</s4>
<s5>96</s5>
</fC03>
<fC03 i1="14" i2="2" l="SPA"><s0>Política del clima</s0>
<s4>CD</s4>
<s5>96</s5>
</fC03>
<fN21><s1>223</s1>
</fN21>
</pA>
</standard>
<server><NO>FRANCIS 14-0180070 INIST</NO>
<ET>Attributing the increase in atmospheric CO<sub>2</sub>
 to emitters and absorbers</ET>
<AU>CIAIS (P.); GASSER (T.); PARIS (J. D.); CALDEIRA (K.); RAUPACH (M. R.); CANADELL (J. G.); PATWARDHAN (A.); FRIEDLINGSTEIN (P.); PIAO (S. L.); GITZ (V.)</AU>
<AF>Laboratoire des Sciences du Climat et de l'Environnement, CEA-CNRS-UVSQ, CE l'Orme des Merisiers/91191 Gif sur Yvette/France (1 aut., 2 aut., 3 aut.); Department of Ecology, College of Urban and Environmental Science, Peking University/Beijing 100871/Chine (1 aut., 9 aut.); Carnegie Institution Department of Global Ecology, 260 Panama Street/Stanford, California 94305/Etats-Unis (4 aut.); Global Carbon Project, CSIRO Marine and Atmospheric Research/Canberra, Australian Capital Territory 2601/Australie (5 aut., 6 aut.); S J Mehta School of Management, Indian Institute of Technology/Powai, 400076 Mumbai/Inde (7 aut.); College of Engineering, Mathematics and Physical Sciences, University of Exeter/Exeter EX4 4QF/Royaume-Uni (8 aut.); Institute of Tibetan Plateau Research, Chinese Academy of Sciences/Beijing 100085/Chine (9 aut.); Centre International de Recherche sur l'Environnement et le Développèment, CNRS-CIRAD-ParisTech-EHESS 45 bis avenue de la Belle Gabrielle/94736 Nogent Sur Marne/France (10 aut.)</AF>
<DT>Publication en série; Niveau analytique</DT>
<SO>Nature climate change : (Print); ISSN 1758-678X; Royaume-Uni; Da. 2013; Vol. 3; No. 10; Pp. 926-930; Bibl. 28 ref.</SO>
<LA>Anglais</LA>
<EA>Climate change policies need to consider the contribution of each emitting region to the increase in atmospheric carbon dioxide. We calculate regional attributions of increased atmospheric CO<sub>2</sub>
 using two different assumptions about land sinks. In the first approach, each absorber region is attributed 'domestic sinks' that occur within its boundaries. In the second, alternative approach, each emitter region is attributed 'foreign sinks' that it created indirectly through its contribution to increasing CO<sub>2</sub>
. We unambiguously attribute the largest share of the historical increase in CO<sub>2</sub>
 between pre-industrial times and the present-day period to developed countries. However, the excess CO<sub>2</sub>
 in the atmosphere since pre-industrial times attributed to developing countries is greater than their share of cumulative CO<sub>2</sub>
 emissions. This is because a greater fraction of their emissions occurred more recently. If emissions remain high over the coming decades, the share of excess CO<sub>2</sub>
 attributable to developing countries will grow, and the sink service provided by forested regions-in particular those with tropical forest-to other regions will depend critically on future tropical land-use change.</EA>
<CC>52118; 521</CC>
<FD>Dioxyde de carbone; Facteur anthropique; Activité humaine; Changement climatique; Equité; Tiers Monde; Pays industrialisé; Relation source puits; Gaz effet serre; Développement durable; Réchauffement climat; Changement planétaire; Mitigation; Politique du climat</FD>
<ED>Carbon dioxide; Anthropogenic factor; Human activity; climate change; Equity; Third World; industrialized countries; Source sink relationship; greenhouse gas; sustainable development; climate warming; global change; Mitigation; Climate policy</ED>
<SD>Carbono dióxido; Factor antrópico; Actividad humana; Equidad; País industrializado; Relación fuente sumidero; Cambio planetario; Política del clima</SD>
<LO>INIST-28118.354000505894240200</LO>
<ID>14-0180070</ID>
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Attributing the increase in atmospheric CO2 to emitters and absorbers

Attributing the increase in atmospheric CO2 to emitters and absorbers

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