Is there warming in the pipeline? A multi-model analysis of the Zero Emissions Commitment from CO2

被引:108
作者
MacDougall, Andrew H. [1 ]
Frolicher, Thomas L. [2 ,3 ]
Jones, Chris D. [4 ]
Rogelj, Joeri [5 ,6 ]
Matthews, H. Damon [7 ]
Zickfeld, Kirsten [8 ]
Arora, Vivek K. [9 ]
Barrett, Noah J. [1 ]
Brovkin, Victor [10 ,11 ]
Burger, Friedrich A. [2 ,3 ]
Eby, Michel [12 ]
Eliseev, Alexey, V [13 ,14 ]
Hajima, Tomohiro [15 ]
Holden, Philip B. [16 ]
Jeltsch-Thommes, Aurich [2 ,3 ]
Koven, Charles [17 ]
Mengis, Nadine [18 ]
Menviel, Laurie [19 ]
Michou, Martine [20 ]
Mokhov, Igor I. [13 ,14 ]
Oka, Akira [21 ]
Schwinger, Jorg [22 ]
Seferian, Roland [20 ]
Shaffer, Gary [23 ,24 ]
Sokolov, Andrei [25 ]
Tachiiri, Kaoru [15 ]
Tjiputra, Jerry [22 ]
Wiltshire, Andrew [4 ]
Ziehn, Tilo [26 ]
机构
[1] St Francis Xavier Univ, Climate & Environm, Antigonish, NS B2G 2W5, Canada
[2] Univ Bern, Phys Inst, Climate & Environm Phys, Bern, Switzerland
[3] Univ Bern, Oeschger Ctr Climate Change Res, Bern, Switzerland
[4] Met Off Hadley Ctr, Exeter EX1 3PB, Devon, England
[5] Imperial Coll London, Grantham Inst Climate Change & Environm, London SW7 2BU, England
[6] Int Inst Appl Syst Anal IIASA, Laxenburg, Austria
[7] Concordia Univ, Dept Geog, Montreal, PQ H3G 1M8, Canada
[8] Simon Fraser Univ, Dept Geog, Burnaby, BC V5A 1S6, Canada
[9] Environm & Climate Change Canada, Canadian Ctr Climate Modelling & Anal, Victoria, BC V8W 2Y2, Canada
[10] Max Planck Inst Meteorol, Hamburg, Germany
[11] Univ Hamburg, CEN, Hamburg, Germany
[12] Univ Victoria, Sch Earth & Ocean Sci, Victoria, BC V8W 2Y2, Canada
[13] Lomonosov Moscow State Univ, Fac Phys, Moscow, Russia
[14] Russian Acad Sci, AM Obukhov Inst Atmospher Phys, Moscow, Russia
[15] Japan Agcy Marine Earth Sci & Technol, Res Ctr Environm Modeling & Applicat, Yokohama, Kanagawa, Japan
[16] Open Univ, Sch Environm Earth & Ecosyst Sci, Milton Keynes MK7 6AA, Bucks, England
[17] Lawrence Berkeley Natl Lab, Climate & Ecosyst Sci Div, Berkeley, CA USA
[18] GEOMAR Helmholtz Ctr Ocean Res, Biogeochem Modelling Dept, Kiel, Germany
[19] Univ New South Wales, Climate Change Res Ctr, PANGEA, Sydney, NSW, Australia
[20] Univ Toulouse, CNRS, CNRM, Meteo France, Toulouse, France
[21] Univ Tokyo, Atmosphere & Ocean Res Inst, Tokyo, Japan
[22] Bjerknes Ctr Climate Res, NORCE Norwegian Res Ctr, Bergen, Norway
[23] Univ Magallanes, Res Ctr GAIA Antarctica, Punta Arenas, Chile
[24] Univ Copenhagen, Niels Bohr Inst, Copenhagen, Denmark
[25] MIT, Ctr Global Change Sci, Cambridge, MA 02139 USA
[26] Commonwealth Sci & Ind Res Org Oceans & Atmospher, Aspendale, Vic, Australia
基金
加拿大自然科学与工程研究理事会; 澳大利亚研究理事会; 俄罗斯基础研究基金会; 瑞士国家科学基金会; 俄罗斯科学基金会;
关键词
EARTH SYSTEM MODEL; ENVIRONMENT SIMULATOR JULES; CARBON-CYCLE; CLIMATE-CHANGE; INTERMEDIATE COMPLEXITY; OCEAN BIOGEOCHEMISTRY; ATMOSPHERIC LIFETIME; PART II; DIOXIDE; ENERGY;
D O I
10.5194/bg-17-2987-2020
中图分类号
Q14 [生态学(生物生态学)];
学科分类号
071012 ; 0713 ;
摘要
The Zero Emissions Commitment (ZEC) is the change in global mean temperature expected to occur following the cessation of net CO2 emissions and as such is a critical parameter for calculating the remaining carbon budget. The Zero Emissions Commitment Model Intercomparison Project (ZECMIP) was established to gain a better understanding of the potential magnitude and sign of ZEC, in addition to the processes that underlie this metric. A total of 18 Earth system models of both full and intermediate complexity participated in ZECMIP. All models conducted an experiment where atmospheric CO2 concentration increases exponentially until 1000 PgC has been emitted. Thereafter emissions are set to zero and models are configured to allow free evolution of atmospheric CO2 concentration. Many models conducted additional second-priority simulations with different cumulative emission totals and an alternative idealized emissions pathway with a gradual transition to zero emissions. The inter-model range of ZEC 50 years after emissions cease for the 1000 PgC experiment is 0:36 to 0.29 degrees C, with a model ensemble mean of 0:07 degrees C, median of 0:05 degrees C, and standard deviation of 0.19 degrees C. Models exhibit a wide variety of behaviours after emissions cease, with some models continuing to warm for decades to millennia and others cooling substantially. Analysis shows that both the carbon uptake by the ocean and the terrestrial biosphere are important for counteracting the warming effect from the reduction in ocean heat uptake in the decades after emissions cease. This warming effect is difficult to constrain due to high uncertainty in the efficacy of ocean heat uptake. Overall, the most likely value of ZEC on multi-decadal timescales is close to zero, consistent with previous model experiments and simple theory.
引用
收藏
页码:2987 / 3016
页数:30
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