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Forest ecosystems and the changing patterns of nitrogen input and acid deposition today and in the future based on a scenario
Authors:Gerald Busch  Gerhard Lammel  Friedrich O Beese  Johann Feichter  Frank J Dentener  Geert-Jan Roelofs
Institution:1. Institute for Soil Science and Forest Nutrition, University of G?ttingen, Büsgenweg 2, D-37077, G?ttingen, Germany
2. Max Planck Institute for Meteorology, Hamburg, Germany
3. Institute for Marine and Atmospheric Research, University of Utrecht, The Netherlands
Abstract:A global assessment of the impact of the anthropogenic perturbation of the nitrogen and sulfur cycles on forest ecosystems is carried out for both the present-day 1980-1990] and for a projection into the future 2040-2050] under a scenario of economic development which represents a medium path of development according to expert guess IPCC IS92a]. Results show that forest soils will receive considerably increasing loads of nitrogen and acid deposition and that deposition patterns are likely to change. The regions which are most prone to depletion of soils buffering capacity and supercritical nitrogen deposition are identified in the subtropical and tropical regions of South America and Southeast Asia apart from the well known 'hotspots' North-Eastern America and Central Europe. The forest areas likely to meet these two risks are still a minor fraction of the global forest ecosystems, though. But the bias between eutrophication and acidification will become greater and an enhanced growth triggered by the fertilizing effects of increasing nitrogen input cannot be balanced by the forest soils nutrient pools. Results show increasing loads into forest ecosystems which are likely to account for 46% higher acid loads and 36% higher nitrogen loads in relation to the 1980-1990 situation. Global background deposition of up to 5 kg N ha-1 a-1 will be exceeded at more than 25% of global forest ecosystems and at more than 50% of forest ecosystems on acid sensitive soils. More than 33% of forest ecosystems on acid sensitive soils will receive acid loads which exceeds their buffering capacity. About 25% of forest areas with exceeded acid loads will receive critical nitrogen loads.
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