B31A-0525
Forest Management in Earth System Modelling: a Vertically Discretised Canopy Description for ORCHIDEE and Effects on European Climate Since 1750

Wednesday, 16 December 2015
Poster Hall (Moscone South)
Matthew McGrath1, Sebastiaan Luyssaert1, Kim Naudts2, Yiying Chen3, James Ryder1, Juliane Otto4, Aude Valade5 and ORCHIDEE Project Team, (1)LSCE Laboratoire des Sciences du Climat et de l'Environnement, Gif-Sur-Yvette Cedex, France, (2)Max Planck Institute for Meteorology, Hamburg, Germany, (3)Civil & Environmental Engineering, National Singapore University, Singapore, Singapore, (4)Helmholtz-Zentrum Geesthacht, Climate Service Center 2.0, Hamburg, Germany, (5)Institut Pierre Simon Laplace, Paris, France
Abstract:

Forest management has the potential to impact surface physical characteristics to the same degree that changes in land cover do. The impacts of land cover changes on the global climate are well-known. Despite an increasingly detailed understanding of the potential for forest management to affect climate, none of the current generation of Earth system models account for forest management through their land surface modules. We addressed this gap by developing and reparameterizing the ORCHIDEE land surface model to simulate the biogeochemical and biophysical effects of forest management. Through vertical discretization of the forest canopy and corresponding modifications to the energy budget, radiation transfer, and carbon allocation, forest management can now be simulated much more realistically on the global scale. This model was used to explore the effect of forest management on European climate since 1750. Reparameterization was carried out to replace generic forest plant functional types with real tree species, covering the most dominant species across the continent. Historical forest management and land cover maps were created to run the simulations from 1600 until the present day. The model was coupled to the atmospheric model LMDz to explore differences in climate between 1750 and 2010 and attribute those differences to changes in atmospheric carbon dioxide concentrations and concurrent warming, land cover, species composition, and wood extraction. Although Europe's forest are considered a carbon sink in this century, our simulations show the modern forests are still experiencing carbon debt compared to their historical values.