Buchmann, N.; Bonal, D.; Barigah, T. S.; Guehl, J. M.; Ehleringer, J. R.: Insights into the carbon dynamics of tropical primary rainforests using stable carbon isotope analyses. In: Ecology and management of a neotropical rainforest: lessons drawn from Paracou, a long-term exeperimental research site in French Guiana, pp. 95 - 113 (Eds. Gourlet-Fleury, S.; Guehl, J. M.; Laroussinie, O.). Elsevier, Paris (2004)
Janssens, I. A.; Dore, S.; Epron, D.; Lankreijer, H.; Buchmann, N.; Longdoz, B.; Brossaud, J.; Montagnani, L.: Climatic influences on seasonal and spatial differences in soil CO" efflux. In: Fluxes of Carbon, Water and Energy of European Forests, Vol. 163, pp. 233 - 253 (Ed. Valentini, R.). Springer, Heidelberg (2003)
Lankreijer, H.; Janssens, I. A.; Buchmann, N.; Longdoz, B.; Epron, D.; Dore, S.: Measurement of soil respiration. In: Fluxes of Carbon, Water and Energy of European Forests, Vol. 163, pp. 37 - 54 (Ed. Valentini, R.). Springer, Heidelberg (2003)
Hooper, D.; Buchmann, N.; Degrange, V.; Díaz, S. M.; Gessner, M. O.; Grime, P.; Hulot, F.; Mermillod-Blondin, F.; Van Peer, L.; Roy, J.et al.; Symstad, A.; Solan, M.; Spehn, E.: Species diversity, functional diversity and ecosystem functioning. In: Biodiversity and ecosystems functioning: a current synthesis, pp. 195 - 208 (Eds. Loreau, M.; Naeem, S.; Inchausti, P.). Oxford University Press, Oxford (2002)
Krause, R.; Buchmann, N.; Churkina, G.; Freibauer, A.: Development of a database for climate research. In: Environmental communication in the information society: proceedings of the 16th International Conference Informatics for Environmental Protection, September 25 - 27, 2002, University of Technology, Vienna, Austria, Vol. 2, pp. 643 - 646 (Eds. Pillmann, W.; Tochtermann, K.). International Society for Envirnonmental Protection, Vienna, Austria (2002)
Wichura, B.; Buchmann, N.; Foken, T.: Carbon dioxide exchange characteristics above a spruce forest. In: 25th Conference on Agricultural and Forest Meteorology: 20 - 24 May 2002, Norfolk, Virginia, pp. 63 - 64. American Meteorological Society, Boston (2002)
Buchmann, N.; Kaplan, J. O.: Carbon isotope discrimination of terrestrial ecosystems - how well do observed and modeled results match? In: Global biogeochemical cycles in the climate system, pp. 253 - 266 (Eds. Schulze, E.-D.; Heimann, M.; Harrison, S. P.; Holland, E.; Lloyd, J. et al.). Academic Press, San Diego (2001)
Gebauer, G.; Zeller, B.; Schmidt, G.; May, C.; Buchmann, N.; Colin-Belgrand, M.; Dambrine, E.; Martin, F.; Schulze, E.-D.; Bottner, P.: The fate of N-15-labelled nitrogen inputs to coniferous and broadleaf forests. In: Carbon and Nitrogen Cycling in European Forest Ecosystems, Vol. 142, pp. 144 - 170 (2000)
Matteucci, G.; Dore, S.; Stivanello, S.; Rebmann, C.; Buchmann, N.: Soil respiration in beech and spruce forests in Europe: Trends, controlling factors, annual budgets and implications for the ecosystem carbon balance. In: Carbon and Nitrogen Cycling in European Forest Ecosystems, Vol. 142, pp. 217 - 236 (Ed. Schulze, E.-D.). Springer, Berlin (2000)
Wichura, B.; Buchmann, N.; Foken, T.: Fluxes of the stable carbon isotope 13C above a spruce forest measured by hyperbolic relaxed eddy accumulation method. In: 14th Symposium on Boundary Layers and Turbulence. 14th Symposium on Boundary Layers and Turbulence, Boston. (2000)
Extreme precipitation should increase with warmer temperatures. Data from tropical regions show that this correlation is obscured by the cooling effect of clouds. When cloud effects are corrected, the increase in extreme precipitation with rising temperatures becomes apparent.
More frequent strong storms are destroying ever larger areas of the Amazon rainforest. Storm damage was mapped between 1985 and 2020. The total area of affected forests roughly quadrupled in the period studied.
The Global Carbon Project shows that fossil CO2 emissions will continue to rise in 2024. There is no sign of the rapid and substantial decline in emissions that would be needed to limit the impact of climate change
The Chinese Academy of Sciences (CAS) and the German National Academy of Sciences Leopoldina will hold a joint conference on the challenges of achieving carbon neutrality in Berlin on October 29-30, 2024.
Experts from science, journalism, local authorities and non-governmental organizations consider a change of course in communication on climate issues to be urgently needed. The appeal was published on the occasion of the K3 Congress on Climate Communication with around 400 participants in Graz.
A study by Leipzig University, the German Centre for Integrative Biodiversity Research Halle-Jena-Leipzig (iDiv) and the MPI for Biogeochemistry shows that gaps in the canopy of a mixed floodplain forest have a direct influence on the temperature and moisture in the forest soil, but only a minor effect on soil activity.
EU funds the international research project AI4PEX to further improve Earth system models and thus scientific predictions of climate change. Participating scientists from 9 countries met at the end of May 2024 to launch the project at the MPI for Biogeochemistry in Jena, which is leading the project.
Thuringia is severely affected by climate change, which is already reflected in extreme weather events and rising temperatures. The Climate Council is calling for the consistent implementation and tightening of climate policy targets in order to achieve climate neutrality by 2045. The coming legislative period is crucial for the future of Thuringia.
From the Greek philosopher Aristotle to Charles Darwin to the present day, scientists have dealt with this fundamental question of biology. Contrary to public perception, however, it is still largely unresolved. Scientists have now presented a new approach for the identification and delimitation of species using artificial intelligence (AI).
When it comes to studying climate change, we generally assume that the total amount of carbon emissions determines how much the planet will warm. A new study suggests that not only the amount, but also the timing of those emissions controls the amount of surface warming that occurs on human time-scale.