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The RCP greenhouse gas concentrations and their extensions from 1765 to 2300

Dados Bibliográficos

ID23375231
AutoresMalte Meinshausen (0000-0003-4048-3521, The University of Melbourne, autor correspondente), Steven J Smith (0000-0003-3248-5607, Joint Global Change Research Institute), Katherine Calvin (0000-0003-2191-4189, Joint Global Change Research Institute), J S Daniel (0000-0001-9903-1007, National Oceanic and Atmospheric Administration), M Kainuma (National Institute for Environmental Studies), M L T Kainuma, Jean‐François Lamarque (0000-0002-4225-5074, NSF National Center for Atmospheric Research), J-F Lamarque, Katsumi Matsumoto (0000-0002-5832-9592), Ken’ichi Matsumoto (0000-0002-9349-9765, University of Shiga Prefecture), K Matsumoto, Stephen A Montzka (0000-0002-9396-0400, National Oceanic and Atmospheric Administration), S C B Raper (Manchester Metropolitan University), Keywan Riahi (0000-0001-7193-3498, International Institute for Applied Systems Analysis), A Thomson (0000-0003-4391-6839), Allison M Thomson (0000-0001-5326-1755, Joint Global Change Research Institute), Guus J M Velders (0000-0002-6597-7088, National Institute for Public Health and the Environment), Detlef P Van Vuuren (0000-0003-0398-2831, Netherlands Environmental Assessment Agency), D P P van Vuuren
Ano2011
Volume109
Fascículo1-2
Páginas213-241
Data de publicação2011-11-01
Peer ReviewedSim
Open AccessSim
TipoARTICLE
PeriódicoClimatic Change (JOURNAL)
Identificadores do periódicoISSN: 0165-0009 • E-ISSN: 1573-1480
EditoraSpringer Science and Business Media LLC (PUBLISHER)
DOI10.1007/s10584-011-0156-z
OpenAlexW2171984413
IdiomaEN
Citações recebidas205
Referências citadas66

We present the greenhouse gas concentrations for the Representative Concentration Pathways (RCPs) and their extensions beyond 2100, the Extended Concentration Pathways (ECPs). These projections include all major anthropogenic greenhouse gases and are a result of a multi-year effort to produce new scenarios for climate change research. We combine a suite of atmospheric concentration observations and emissions estimates for greenhouse gases (GHGs) through the historical period (1750–2005) with harmonized emissions projected by four different Integrated Assessment Models for 2005–2100. As concentrations are somewhat dependent on the future climate itself (due to climate feedbacks in the carbon and other gas cycles), we emulate median response characteristics of models assessed in the IPCC Fourth Assessment Report using the reduced-complexity carbon cycle climate model MAGICC6. Projected ‘best-estimate’ global-mean surface temperature increases (using inter alia a climate sensitivity of 3°C) range from 1.5°C by 2100 for the lowest of the four RCPs, called both RCP3-PD and RCP2.6, to 4.5°C for the highest one, RCP8.5, relative to pre-industrial levels. Beyond 2100, we present the ECPs that are simple extensions of the RCPs, based on the assumption of either smoothly stabilizing concentrations or constant emissions: For example, the lower RCP2.6 pathway represents a strong mitigation scenario and is extended by assuming constant emissions after 2100 (including net negative CO 2 emissions), leading to CO 2 concentrations returning to 360 ppm by 2300. We also present the GHG concentrations for one supplementary extension, which illustrates the stringent emissions implications of attempting to go back to ECP4.5 concentration levels by 2250 after emissions during the 21 st century followed the higher RCP6 scenario. Corresponding radiative forcing values are presented for the RCP and ECPs.

Atmospheric sciences · Carbon cycle · Climate change · Climate model · Climatology · Ecosystem · Greenhouse gas · Representative Concentration Pathways · Atmospheric and Environmental Gas Dynamics · Atmospheric chemistry and aerosols · Atmospheric Ozone and Climate · Ecology · Environmental Science

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Intervalo de citações2011 - 2026 (16)
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