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Biogeosciences An interactive open-access journal of the European Geosciences Union
Biogeosciences, 11, 7251-7267, 2014
http://www.biogeosciences.net/11/7251/2014/
doi:10.5194/bg-11-7251-2014
© Author(s) 2014. This work is distributed
under the Creative Commons Attribution 3.0 License.
Research article
17 Dec 2014
Biogeophysical impacts of peatland forestation on regional climate changes in Finland
Y. Gao1,2, T. Markkanen1, L. Backman1, H. M. Henttonen3, J.-P. Pietikäinen1, H. M. Mäkelä1, and A. Laaksonen1,4 1Finnish Meteorological Institute, P.O. Box 503, 00101 Helsinki, Finland
2University of Helsinki, Department of Physics, P.O. Box 64, 00014 Helsinki, Finland
3Finnish Forest Research Institute, P.O. Box 18, 01301 Vantaa, Finland
4University of Eastern Finland, Department of Applied Physics, P.O. Box 1627, 70211 Kuopio, Finland
Abstract. Land cover changes can impact the climate by influencing the surface energy and water balance. Naturally treeless or sparsely treed peatlands were extensively drained to stimulate forest growth in Finland over the second half of 20th century. The aim of this study is to investigate the biogeophysical effects of peatland forestation on regional climate in Finland. Two sets of 18-year climate simulations were done with the regional climate model REMO by using land cover data based on pre-drainage (1920s) and post-drainage (2000s) Finnish national forest inventories. In the most intensive peatland forestation area, located in the middle west of Finland, the results show a warming in April of up to 0.43 K in monthly-averaged daily mean 2 m air temperature, whereas a slight cooling from May to October of less than 0.1 K in general is found. Consequently, snow clearance days over that area are advanced up to 5 days in the mean of 15 years. No clear signal is found for precipitation. Through analysing the simulated temperature and energy balance terms, as well as snow depth over five selected subregions, a positive feedback induced by peatland forestation is found between decreased surface albedo and increased surface air temperature in the snow-melting period. Our modelled results show good qualitative agreements with the observational data. In general, decreased surface albedo in the snow-melting period and increased evapotranspiration in the growing period are the most important biogeophysical aspects induced by peatland forestation that cause changes in climate. The results from this study can be further integrally analysed with biogeochemical effects of peatland forestation to provide background information for adapting future forest management to mitigate climate warming effects. Moreover, they provide insights about the impacts of projected forestation of tundra at high latitudes due to climate change.

Citation: Gao, Y., Markkanen, T., Backman, L., Henttonen, H. M., Pietikäinen, J.-P., Mäkelä, H. M., and Laaksonen, A.: Biogeophysical impacts of peatland forestation on regional climate changes in Finland, Biogeosciences, 11, 7251-7267, doi:10.5194/bg-11-7251-2014, 2014.
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This work studies the biogeophysical impacts of peatland forestation on regional climate conditions in Finland by a regional climate model with two land cover maps produced from Finnish national forest inventories. A warming in spring and a slight cooling in the growing season are found in peatland forestation area, which are mainly induced by the decreased surface albedo and increased ET, respectively. The snow clearance days are advanced. The results are also compared with observational data.
This work studies the biogeophysical impacts of peatland forestation on regional climate...
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