Time Scales of Terrestrial Carbon Response Related to Land-Use Application: Implications for Initializing an Earth System Model

AbstractThe dynamic vegetation and carbon cycling component, LM3V, of the Geophysical Fluid Dynamics Laboratory (GFDL) prototype Earth system model (ESM2.1), has been designed to simulate the effects of land use on terrestrial carbon pools, including secondary vegetation regrowth. Because of the long time scales associated with the carbon adjustment, special consideration is required when initializing the ESM when historical simulations are conducted. Starting from an equilibrated, preindustrial climate and potential vegetation state in an offline land-only model (LM3V), estimates of historical land use are instantaneously applied in five experiments beginning in the following calendar years: 1500, 1600, 1700, 1750, and 1800. This application results in the land carbon pools experiencing an abrupt change—a carbon shock—and the secondary vegetation needs time to regrow into consistency with the harvesting history. The authors find that it takes approximately 100 years for the vegetation to recover from the...

[1]  Karl E. Taylor,et al.  An overview of CMIP5 and the experiment design , 2012 .

[2]  A. Thomson,et al.  Harmonization of Global Land-Use Scenarios for the Period 1500-2100 for the 5th IPCC Assessment , 2009 .

[3]  M. Claussen,et al.  Effects of anthropogenic land cover change on the carbon cycle of the last millennium , 2009 .

[4]  S. Frolking,et al.  Harmonisation of global land-use scenarios for the period 1500–2100 for IPCC-AR5 , 2009 .

[5]  George C. Hurtt,et al.  Carbon cycling under 300 years of land use change: Importance of the secondary vegetation sink , 2009 .

[6]  R. Knox,et al.  Reconstructed historical land cover and biophysical parameters for studies of land-atmosphere interactions within the eastern United States , 2008 .

[7]  R. Dickinson,et al.  Couplings between changes in the climate system and biogeochemistry , 2007 .

[8]  Yoshiki Yamagata,et al.  Factoring out natural and indirect human effects on terrestrial carbon sources and sinks , 2007 .

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

[10]  S. Malyshev,et al.  The underpinnings of land‐use history: three centuries of global gridded land‐use transitions, wood‐harvest activity, and resulting secondary lands , 2006 .

[11]  S. Klein,et al.  GFDL's CM2 Global Coupled Climate Models. Part I: Formulation and Simulation Characteristics , 2006 .

[12]  Andrew T. Wittenberg,et al.  GFDL's CM2 Global Coupled Climate Models. Part III: Tropical Pacific Climate and ENSO , 2006 .

[13]  Atul K. Jain,et al.  Modeling the effects of two different land cover change data sets on the carbon stocks of plants and soils in concert with CO2 and climate change , 2005 .

[14]  R. Houghton,et al.  Revised estimates of the annual net flux of carbon to the atmosphere from changes in land use and land management 1850–2000 , 2003 .

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

[16]  S. Pacala,et al.  Projecting the future of the U.S. carbon sink , 2001, Proceedings of the National Academy of Sciences of the United States of America.

[17]  P. Ciais,et al.  Consistent Land- and Atmosphere-Based U.S. Carbon Sink Estimates , 2001, Science.

[18]  I. C. Prentice,et al.  Carbon balance of the terrestrial biosphere in the Twentieth Century: Analyses of CO2, climate and land use effects with four process‐based ecosystem models , 2001 .

[19]  Michael T. Coe,et al.  Testing the performance of a dynamic global ecosystem model: Water balance, carbon balance, and vegetation structure , 2000 .

[20]  R. Houghton The annual net flux of carbon to the atmosphere from changes in land use 1850–1990* , 1999 .

[21]  Stephen W. Pacala,et al.  LINEAR ANALYSIS OF SOIL DECOMPOSITION: INSIGHTS FROM THE CENTURY MODEL , 1998 .