Analysing countries' contribution to climate change:: scientific and policy-related choices

被引:70
作者
den Elzen, M
Fuglestvedt, J
Höhne, N
Trudinger, C
Lowe, J
Matthews, B
Romstad, B
de Campos, CP
Andronova, N
机构
[1] Netherlands Environm Assessment Agcy, NL-3710 BA Bilthoven, Netherlands
[2] ECOFYS Energy & Environm, Cologne, Germany
[3] CICERO, Ctr Int Climate & Environm Res, Oslo, Norway
[4] CSIRO, Aspendale, Vic, Australia
[5] Catholic Univ Louvain, Inst Astron & Geophys, B-1348 Louvain, Belgium
[6] Univ Fed Rio de Janeiro, Int Virtual Inst Global Change, Rio De Janeiro, Brazil
[7] Univ Illinois, Dept Atmospher Sci, Urbana, IL 61801 USA
关键词
climate change; regional historical emissions; contribution to global climate change; Brazilian proposal; climate models;
D O I
10.1016/j.envsci.2005.06.007
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
This paper evaluates the influence of different policy-related and scientific choices on the calculated regional contributions to global climate change (the "Brazilian Proposal"). Policy-related choices include the time period of emissions, the mix of greenhouse gases and different indicators of climate change impacts. The scientific choices include historical emissions and model representations of the climate system. We generated and compared results of several simple climate models. We find that the relative contributions of different nations to global climate change-from emissions of greenhouse gases alone-are quite robust, despite the varying model complexity and differences in calculated absolute changes. For the default calculations, the average calculated contributions to the global mean surface temperature increase in 2000 are about 40% from OECD, 14% from Eastern Europe and Former Soviet Union, 24% from Asia and 22% from Africa and Latin America. Policy-related choices, such as time period of emissions, climate change indicator and gas mix generally have larger influence on the results than scientific choices. More specifically, choosing a later attribution start date (1990 instead of 1890) for historical emissions, decreases the contributions of regions that started emitting early, such as the OECD countries by 6 percentage points, whereas it increases the contribution of late emitters such as Asia by 8 percentage points. However, only including the fossil CO, emissions instead of the emissions of all Kyoto gases (fossil and land use change), increases the OECD contributions by 21 percentage points and decreases the contribution of Asia by 14 percentage points. (c) 2005 Elsevier Ltd. All rights reserved.
引用
收藏
页码:614 / 636
页数:23
相关论文
共 49 条
[1]  
ANDRES RJ, 1998, TELLUS B, V51, P1751
[2]   Importance of Sulfate Aerosol in Evaluating the Relative Contributions of Regional Emissions to the Historical Global Temperature Change [J].
Natalia Andronova ;
Michael Schlesinger .
Mitigation and Adaptation Strategies for Global Change, 2004, 9 (4) :383-390
[3]  
[Anonymous], 2001, CLIMATE CHANGE 2001
[4]  
[Anonymous], TRENDS COMPENDIUM DA
[5]  
CUBASCH U, 2001, CLIMATE CHANGE 2001, P892
[6]   Historical CO2 emission and concentrations due to land use change of croplands and pastures by country [J].
de Campos, CP ;
Muylaert, MS ;
Rosa, LP .
SCIENCE OF THE TOTAL ENVIRONMENT, 2005, 346 (1-3) :149-155
[7]   Responsibility for past and future global warming: Uncertainties in attributing anthropogenic climate change [J].
Den Elzen, M ;
Schaeffer, M .
CLIMATIC CHANGE, 2002, 54 (1-2) :29-73
[8]   Differentiating future commitments on the basis of countries' relative historical responsibility for climate change: Uncertainties in the 'Brazilian proposal' in the context of a policy implementation [J].
Den Elzen, MGJ ;
Schaeffer, M ;
Lucas, PL .
CLIMATIC CHANGE, 2005, 71 (03) :277-301
[9]  
DENELZEN MGJ, 2002, 728001022 MNP
[10]  
DENELZEN MGJ, 1999, 728001011 MNP