Protecting climate with forests

Policies for climate mitigation on land rarely acknowledge biophysical factors, such as reflectivity, evaporation, and surface roughness. Yet such factors can alter temperatures much more than carbon sequestration does, and often in a conflicting way. We outline a framework for examining biophysical factors in mitigation policies and provide some best-practice recommendations based on that framework. Tropical projects—avoided deforestation, forest restoration, and afforestation—provide the greatest climate value, because carbon storage and biophysics align to cool the Earth. In contrast, the climate benefits of carbon storage are often counteracted in boreal and other snow-covered regions, where darker trees trap more heat than snow does. Managers can increase the climate benefit of some forest projects by using more reflective and deciduous species and through urban forestry projects that reduce energy use. Ignoring biophysical interactions could result in millions of dollars being invested in some mitigation projects that provide little climate benefit or, worse, are counter-productive.

[1]  John E. Walsh,et al.  Integrated regional changes in arctic climate feedbacks: Implications for the global climate system , 2006 .

[2]  Gregg Marland,et al.  The climatic impacts of land surface change and carbon management, and the implications for climate-change mitigation policy , 2003 .

[3]  Keith A. Smith,et al.  N 2 O release from agro-biofuel production negates global warming reduction by replacing fossil fuels , 2007 .

[4]  Alan H. Strahler,et al.  Global land cover mapping from MODIS: algorithms and early results , 2002 .

[5]  S Pacala,et al.  Stabilization Wedges: Solving the Climate Problem for the Next 50 Years with Current Technologies , 2004, Science.

[6]  George W. Koch,et al.  Carbon protection and fire risk reduction: toward a full accounting of forest carbon offsets , 2008 .

[7]  G. Bonan Forests and Climate Change: Forcings, Feedbacks, and the Climate Benefits of Forests , 2008, Science.

[8]  N. Diffenbaugh,et al.  Global climate sensitivity to land surface change: The Mid Holocene revisited , 2002 .

[9]  Bas Eickhout,et al.  CO2 and albedo climate impacts of extratropical carbon and biomass plantations , 2006 .

[10]  Bruce A. McCarl,et al.  Trading Water for Carbon with Biological Carbon Sequestration , 2005, Science.

[11]  Robert E. Dickinson,et al.  Impacts on regional climate of Amazon deforestation , 1992 .

[12]  J. Canadell,et al.  Global and regional drivers of accelerating CO2 emissions , 2007, Proceedings of the National Academy of Sciences.

[13]  Jehn-Yih Juang,et al.  Separating the effects of albedo from eco‐physiological changes on surface temperature along a successional chronosequence in the southeastern United States , 2007 .

[14]  R. Betts Offset of the potential carbon sink from boreal forestation by decreases in surface albedo , 2000, Nature.

[15]  R. B. Jackson,et al.  Vegetation–Climate Feedbacks in the Conversion of Tropical Savanna to Grassland , 2000 .

[16]  J. Lean,et al.  Simulation of the regional climatic impact of Amazon deforestation , 1989, Nature.

[17]  N. C. Strugnell,et al.  First operational BRDF, albedo nadir reflectance products from MODIS , 2002 .

[18]  Mariana Vertenstein,et al.  Effects of land use change on North American climate: impact of surface datasets and model biogeophysics , 2004 .

[19]  J. Randerson,et al.  The Impact of Boreal Forest Fire on Climate Warming , 2006, Science.

[20]  Paulo Nobre,et al.  Amazon Deforestation and Climate Change in a Coupled Model Simulation , 2009 .

[21]  B. Lamont,et al.  Grasstrees reveal contrasting fire regimes in eucalypt forest before and after European settlement of southwestern Australia , 2001 .

[22]  Christopher B. Field,et al.  Feedbacks of Terrestrial Ecosystems to Climate Change , 2007 .

[23]  K. Caldeira,et al.  Combined climate and carbon-cycle effects of large-scale deforestation , 2006, Proceedings of the National Academy of Sciences.

[24]  R. Pielke,et al.  Influence of landscape structure on local and regional climate , 1990, Landscape Ecology.

[25]  Christopher B. Field,et al.  Changing feedbacks in the climate–biosphere system , 2008 .

[26]  R. Betts,et al.  Implications of land ecosystem-atmosphere interactions for strategies for climate change adaptation and mitigation , 2007 .

[27]  R. DeFries,et al.  Human modification of the landscape and surface climate in the next fifty years , 2002 .

[28]  Andrew J. Plantinga,et al.  Co-Benefits from Carbon Sequestration in Forests: Evaluating Reductions in Agricultural Externalities from an Afforestation Policy in Wisconsin , 2003, Land Economics.