Soil processes dominate the long-term response of forest net primary productivity to increased temperature and atmospheric CO2 concentration
Autor: | Medlyn, Belinda E., McMurtrie, Ross E., Dewar, Roderick, Jeffreys, Mark P. |
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Přispěvatelé: | University of Edinburgh, University of New South Wales [Sydney] (UNSW), Unité de bioclimatologie, Institut National de la Recherche Agronomique (INRA) |
Jazyk: | angličtina |
Rok vydání: | 2000 |
Předmět: | |
Zdroj: | Canadian Journal of Forest Research Canadian Journal of Forest Research, NRC Research Press, 2000, 30 (6), pp.873-888. ⟨10.1139/cjfr-30-6-873⟩ |
ISSN: | 0045-5067 1208-6037 |
DOI: | 10.1139/cjfr-30-6-873⟩ |
Popis: | International audience; Predicting the responses of forest growth to elevated temperature (T) and atmospheric CO2 concentration ([CO2]) on decadal time scales presents a formidable challenge because of the many interacting processes involved. A key uncertainty concerns the relative importance of plant and soil processes to the overall long-term response. In this study, the plant-soil model GDAY was used to simulate forest growth responses to T and [CO2] on different time scales for forests in cool and warm climates. An equilibrium-based graphical analysis was used to distinguish the roles played by plant and soil processes in determining the response. Doubled [CO2] caused a large initial increase (20%) in net primary productivity (NPP), but this did not persist in the long term. By contrast, a 2 degrees C increase in T caused a persistent long-term increase in NPP of approximately 10-15%. These responses were similar at cool and warm sites. The equilibrium analysis indicated that soil processes dominated the long-term responses predicted by the model. In particular, the predicted long-term increase in NPP under elevated T reflected an increase in predicted N mineralization and plant N uptake, assuming that a constant fraction of mineralized N is taken up by plants. The analysis highlights key uncertainties for future research. |
Databáze: | OpenAIRE |
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