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      Case study for the assessment of the biogeophysical effects of a potential afforestation in Europe

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          Abstract

          Background

          A regional-scale sensitivity study has been carried out to investigate the climatic effects of forest cover change in Europe. Applying REMO (regional climate model of the Max Planck Institute for Meteorology), the projected temperature and precipitation tendencies have been analysed for summer, based on the results of the A2 IPCC-SRES emission scenario simulation. For the end of the 21st century it has been studied, whether the assumed forest cover increase could reduce the effects of the greenhouse gas concentration change.

          Results

          Based on the simulation results, biogeophysical effects of the hypothetic potential afforestation may lead to cooler and moister conditions during summer in most parts of the temperate zone. The largest relative effects of forest cover increase can be expected in northern Germany, Poland and Ukraine, which is 15–20% of the climate change signal for temperature and more than 50% for precipitation. In northern Germany and France, potential afforestation may enhance the effects of emission change, resulting in more severe heavy precipitation events. The probability of dry days and warm temperature extremes would decrease.

          Conclusions

          Large contiguous forest blocks can have distinctive biogeophysical effect on the climate on regional and local scale. In certain regions of the temperate zone, climate change signal due to greenhouse gas emission can be reduced by afforestation due to the dominant evaporative cooling effect during summer. Results of this case study with a hypothetical land cover change can contribute to the assessment of the role of forests in adapting to climate change. Thus they can build an important basis of the future forest policy.

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          Most cited references39

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          Land-atmosphere coupling and climate change in Europe.

          Increasing greenhouse gas concentrations are expected to enhance the interannual variability of summer climate in Europe and other mid-latitude regions, potentially causing more frequent heatwaves. Climate models consistently predict an increase in the variability of summer temperatures in these areas, but the underlying mechanisms responsible for this increase remain uncertain. Here we explore these mechanisms using regional simulations of recent and future climatic conditions with and without land-atmosphere interactions. Our results indicate that the increase in summer temperature variability predicted in central and eastern Europe is mainly due to feedbacks between the land surface and the atmosphere. Furthermore, they suggest that land-atmosphere interactions increase climate variability in this region because climatic regimes in Europe shift northwards in response to increasing greenhouse gas concentrations, creating a new transitional climate zone with strong land-atmosphere coupling in central and eastern Europe. These findings emphasize the importance of soil-moisture-temperature feedbacks (in addition to soil-moisture-precipitation feedbacks) in influencing summer climate variability and the potential migration of climate zones with strong land-atmosphere coupling as a consequence of global warming. This highlights the crucial role of land-atmosphere interactions in future climate change.
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            • Record: found
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            Future extreme events in European climate: an exploration of regional climate model projections

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              • Abstract: not found
              • Article: not found

              Consistent geographical patterns of changes in high-impact European heatwaves

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                Author and article information

                Journal
                Carbon Balance Manag
                Carbon Balance Manag
                Carbon Balance and Management
                BioMed Central
                1750-0680
                2013
                1 February 2013
                : 8
                : 3
                Affiliations
                [1 ]Max Planck Institute for Meteorology, Hamburg, Germany
                [2 ]Climate Service Center – eine Einrichtung am Helmholtz-Zentrum Geesthacht, Hamburg, Germany
                [3 ]IIASA, International Institute for Applied Systems Analysis, Laxenburg, Austria
                Article
                1750-0680-8-3
                10.1186/1750-0680-8-3
                3626884
                23369380
                6b4762fb-91ce-4049-bda4-77b74d8206a9
                Copyright ©2013 Gálos et al.; licensee BioMed Central Ltd.

                This is an Open Access article distributed under the terms of the Creative Commons Attribution License ( http://creativecommons.org/licenses/by/2.0), which permits unrestricted use, distribution, and reproduction in any medium, provided the original work is properly cited.

                History
                : 8 November 2012
                : 10 December 2012
                Categories
                Research

                Environmental change
                land cover change,afforestation,biogeophysical feedbacks,climatic extremes,regional climate modelling

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