Articles | Volume 12, issue 2
Biogeosciences, 12, 467–487, 2015
Biogeosciences, 12, 467–487, 2015

Research article 27 Jan 2015

Research article | 27 Jan 2015

Carbon storage versus albedo change: radiative forcing of forest expansion in temperate mountainous regions of Switzerland

J. Schwaab1,5, M. Bavay1, E. Davin4, F. Hagedorn2, F. Hüsler3, M. Lehning1,6, M. Schneebeli1, E. Thürig2, and P. Bebi1 J. Schwaab et al.
  • 1WSL – Institute for Snow and Avalanche Research SLF, 7260 Davos, Switzerland
  • 2Swiss Federal Institute for Forest, Snow and Landscape Research WSL, 8903 Birmensdorf, Switzerland
  • 3Institute of Geography and Oeschger Center for Climate Change Research, University of Bern, 3012 Bern, Switzerland
  • 4Institute for Atmospheric and Climate Sciences, ETH Zürich, 8092 Zürich, Switzerland
  • 5Institute for Spatial and Landscape Planning, ETH Zürich, 8093 Zürich, Switzerland
  • 6CRYOS, School of Architecture, Civil and Environmental Engineering, EPFL, 1015 Lausanne, Switzerland

Abstract. In this study, we assess the climate mitigation potential from afforestation in a mountainous snow-rich region (Switzerland) with strongly varying environmental conditions. Using radiative forcing calculations, we quantify both the carbon sequestration potential and the effect of albedo change at high resolution. We calculate the albedo radiative forcing based on remotely sensed data sets of albedo, global radiation and snow cover. Carbon sequestration is estimated from changes in carbon stocks based on national inventories. We first estimate the spatial pattern of radiative forcing (RF) across Switzerland assuming homogeneous transitions from open land to forest. This highlights where forest expansion still exhibits climatic benefits when including the radiative forcing of albedo change. Second, given that forest expansion is currently the dominant land-use change process in the Swiss Alps, we calculate the radiative forcing that occurred between 1985 and 1997. Our results show that the net RF of forest expansion ranges from −24 W m−2 at low elevations of the northern Prealps to 2 W m−2 at high elevations of the Central Alps. The albedo RF increases with increasing altitude, which offsets the CO2 RF at high elevations with long snow-covered periods, high global radiation and low carbon sequestration. Albedo RF is particularly relevant during transitions from open land to open forest but not in later stages of forest development. Between 1985 and 1997, when overall forest expansion in Switzerland was approximately 4%, the albedo RF offset the CO2 RF by an average of 40%. We conclude that the albedo RF should be considered at an appropriately high resolution when estimating the climatic effect of forestation in temperate mountainous regions.

Final-revised paper