A GCM study of future climate response to aerosol pollution reductions

We use the global atmospheric GCM aerosol model ECHAM5-HAM to asses possible impacts of future air pollution mitigation strategies on climate. Air quality control strategies focus on the reduction of aerosol emissions. Here we investigate the extreme case of a maximum feasible end-of-pipe abatement of aerosols in the near term future (2030) in combination with increasing greenhouse gas (GHG) concentrations. The temperature response of increasing GHG concentrations and reduced aerosol emissions leads to a global annual mean equilibrium temperature response of 2.18 K. When aerosols are maximally abated only in the Industry and Powerplant sector, while other sectors stay with currently enforced regulations, the temperature response is 1.89 K. A maximum feasible abatement applied in the Domestic and Transport sector, while other sectors remain with the current legislation, leads to a temperature response of 1.39 K. Increasing GHG concentrations alone lead to a temperature response of 1.20 K. We also simulate 2–5% increases in global mean precipitation among all scenarios considered, and the hydrological sensitivity is found to be significantly higher for aerosols than for GHGs. Our study, thus highlights the huge potential impact of future air pollution mitigation strategies on climate and supports the need for urgent GHG emission reductions. GHG and aerosol forcings are not independent as both affect and are influenced by changes in the hydrological cycle. However, within the given range of changes in aerosol emissions and GHG concentrations considered in this study, the climate response towards increasing GHG concentrations and decreasing aerosols emissions is additive.

[1]  S. Twomey The Influence of Pollution on the Shortwave Albedo of Clouds , 1977 .

[2]  F. Wentz,et al.  How Much More Rain Will Global Warming Bring? , 2007, Science.

[3]  R. Sausen,et al.  A comparison of climate response to different radiative forcings in three general circulation models: towards an improved metric of climate change , 2003 .

[4]  Kirsten L. Findell,et al.  Strong sensitivity of late 21st century climate to projected changes in short-lived air pollutants , 2008 .

[5]  V. Eyring,et al.  Emissions from international shipping: 2. Impact of future technologies on scenarios until 2050 , 2005 .

[6]  Yoko Tsushima,et al.  Importance of the mixed-phase cloud distribution in the control climate for assessing the response of clouds to carbon dioxide increase: a multi-model study , 2006 .

[7]  John H. Seinfeld,et al.  Climate response of direct radiative forcing of anthropogenic black carbon , 2005 .

[8]  Jonathan M. Gregory,et al.  Mechanisms for the land/sea warming contrast exhibited by simulations of climate change , 2008 .

[9]  David G. Streets,et al.  Two‐decadal aerosol trends as a likely explanation of the global dimming/brightening transition , 2006 .

[10]  D. Randall,et al.  Climate models and their evaluation , 2007 .

[11]  Christopher S. Bretherton,et al.  Climate sensitivity and cloud response of a GCM with a superparameterization , 2006 .

[12]  U. Lohmann,et al.  Cloud microphysics and aerosol indirect effects in the global climate model ECHAM5-HAM , 2007 .

[13]  Alexei G. Sankovski,et al.  Special report on emissions scenarios : a special report of Working group III of the Intergovernmental Panel on Climate Change , 2000 .

[14]  T. Raddatz,et al.  Is the Climate Sensitivity Even More Uncertain , 2008 .

[15]  Jean-Francois Lamarque,et al.  Multimodel projections of climate change from short‐lived emissions due to human activities , 2008 .

[16]  I. Musat,et al.  On the contribution of local feedback mechanisms to the range of climate sensitivity in two GCM ensembles , 2006 .

[17]  P. Bergamaschi,et al.  European Geosciences Union Atmospheric Chemistry , 2004 .

[18]  R. Betts,et al.  Changes in Atmospheric Constituents and in Radiative Forcing. Chapter 2 , 2007 .

[19]  O. Boucher,et al.  The aerosol-climate model ECHAM5-HAM , 2004 .

[20]  G. Boer,et al.  The modification of greenhouse gas warming by the direct effect of sulphate aerosols , 1998 .

[21]  F. Chauvin,et al.  Sensitivity of the hydrological cycle to increasing amounts of greenhouse gases and aerosols , 2002 .

[22]  Lennart Bengtsson,et al.  Transient Climate Change Simulations with a Coupled Atmosphere–Ocean GCM Including the Tropospheric Sulfur Cycle , 1999 .

[23]  S. Solomon,et al.  How Often Will It Rain , 2005 .

[24]  G. Boer Climate change and the regulation of the surface moisture and energy budgets , 1993 .

[25]  Johann Feichter,et al.  Simulation of the tropospheric sulfur cycle in a global climate model , 1996 .

[26]  Roger Jones,et al.  Regional climate projections , 2007 .

[27]  R. Sausen,et al.  Is the climate sensitivity to ozone perturbations enhanced by stratospheric water vapor feedback? , 2001 .

[28]  Kaarle Kupiainen,et al.  Scenarios of global anthropogenic emissions of air pollutants and methane until 2030 , 2007 .

[29]  C. Long,et al.  From Dimming to Brightening: Decadal Changes in Solar Radiation at Earth's Surface , 2005, Science.

[30]  T. L. Schneider,et al.  Climate forcing due to tropospheric and stratospheric ozone , 1999 .

[31]  J. Houghton,et al.  Climate change 2001 : the scientific basis , 2001 .

[32]  H. L. Miller,et al.  Global climate projections , 2007 .

[33]  Alexei G. Sankovski,et al.  Special report on emissions scenarios , 2000 .

[34]  Markus Amann,et al.  A Good Climate for Clean Air: Linkages between Climate Change and Air Pollution. An Editorial Essay , 2004 .

[35]  J. Hansen,et al.  Radiative forcing and climate response , 1997 .

[36]  J. Haywood,et al.  Sensitivity of global sulphate aerosol production to changes in oxidant concentrations and climate , 2007 .

[37]  U. Lohmann,et al.  Nonlinear Aspects of the Climate Response to Greenhouse Gas and Aerosol Forcing , 2004 .

[38]  Leon D. Rotstayn,et al.  Tropical Rainfall Trends and the Indirect Aerosol Effect , 2002 .

[39]  John H. Seinfeld,et al.  Role of Climate Change in Global Predictions of Future Tropospheric Ozone and Aerosols , 2006 .

[40]  M. Blackburn,et al.  An examination of climate sensitivity for idealised climate change experiments in an intermediate general circulation model , 2000 .

[41]  J. Hansen,et al.  Efficacy of climate forcings , 2005 .

[42]  E. Maier‐Reimer,et al.  Response of dimethylsulfide (DMS) in the ocean and atmosphere to global warming , 2007 .

[43]  J.G.J. Olivier,et al.  Global emission sources and sinks , 2001 .

[44]  Michael F. Wehner,et al.  Testing the linearity of the response to combined greenhouse gas and sulfate aerosol forcing , 2004 .

[45]  L. Nazarenko,et al.  Varying trends in surface energy fluxes and associated climate between 1960 and 2002 based on transient climate simulations , 2005 .

[46]  O. Boucher,et al.  Aerosol forcing, climate response and climate sensitivity in the Hadley Centre climate model , 2007 .

[47]  Jens Debernard,et al.  On the additivity of climate response to anthropogenic aerosols and CO2, and the enhancement of future global warming by carbonaceous aerosols , 2008 .

[48]  U. Lohmann,et al.  Influence of future air pollution mitigation strategies on total aerosol radiative forcing , 2008 .

[49]  Jean-Francois Lamarque,et al.  Sea-salt aerosol response to climate change: Last Glacial Maximum, preindustrial, and doubled carbon dioxide climates , 2006 .

[50]  K. Riahi,et al.  Greenhouse Gas Emissions in a Dynamics-as-Usual Scenario of Economic and Energy Development , 2000 .

[51]  W. Collins,et al.  Global climate projections , 2007 .

[52]  A. Sterl,et al.  The ERA‐40 re‐analysis , 2005 .

[53]  David G. Streets,et al.  Influences of man-made emissions and climate changes on tropospheric ozone, methane, and sulfate at 2030 from a broad range of possible futures , 2006 .

[54]  A. Jones,et al.  Climate sensitivity to black carbon aerosol from fossil fuel combustion , 2004 .

[55]  Ulrike Lohmann,et al.  Can aerosols spin down the water cycle in a warmer and moister world? , 2004 .

[56]  I. Tegen,et al.  Relative importance of climate and land use in determining present and future global soil dust emission , 2004 .

[57]  N. Mahowald,et al.  Change in atmospheric mineral aerosols in response to climate: Last glacial period, preindustrial, modern, and doubled carbon dioxide climates , 2006 .

[58]  J. Berdowski,et al.  The climate system , 2001 .

[59]  B. Albrecht Aerosols, Cloud Microphysics, and Fractional Cloudiness , 1989, Science.