Pitelka, L. F.; Gardner, R. H.; Ash, J.; Berry, S.; Gitay, H.; Noble, I. R.; Saunders, A.; Bradshaw, R. H. W.; Brubaker, L.; Clark, J. S.et al.; Davis, M. B.; Sugita, S.; Dyer, J. M.; Hengeveld, R.; Hope, G.; Huntley, B.; King, G. A.; Lavorel, S.; Mack, R. N.; Malanson, G. P.; Mcglone, M.; Prentice, I. C.; Rejmanek, M.: Plant migration and climate change. American Scientist 85 (5), S. 464 - 473 (1997)
Schimel, D. S.; Emanuel, W.; Rizzo, B.; Smith, T.; Woodward, F. I.; Fisher, H.; Kittel, T. G. F.; Mckeown, R.; Painter, T.; Rosenbloom, N.et al.; Ojima, D. S.; Parton, W. J.; Kicklighter, D. W.; Mcguire, A. D.; Melillo, J. M.; Pan, Y.; Haxeltine, A.; Prentice, I. C.; Sitch, S.; Hibbard, K.; Nemani, R.; Pierce, L.; Running, S.; Borchers, J.; Chaney, J.; Neilson, R.; Braswell, B. H.: Continental scale variability in ecosystem processes: Models, data, and the role of disturbance. Ecological Monographs 67 (2), S. 251 - 271 (1997)
Texier, D.; De Noblet, N.; Harrison, S. P.; Haxeltine, A.; Jolly, D.; Joussaume, S.; Laarif, F.; Prentice, I. C.; Tarasov, P.: Quantifying the role of biosphere-atmosphere feedbacks in climate change: coupled model simulations for 6000 years BP and comparison with palaeodata for northern Eurasia and northern Africa. Climate Dynamics 13 (12), S. 865 - 882 (1997)
Haxeltine, A.; Prentice, I. C.; Creswell, I. D.: A coupled carbon and water flux model to predict vegetation structure. Journal of Vegetation Science 7 (5), S. 651 - 666 (1996)
Joos, F.; Prentice, I. C.: A Paleo-perspective on changes in atmospheric CO2 and climate. In: The global carbon cycle, Bd. 62, S. 165 - 186 (Hg. Field, C. B.; Raupach, M. R.). Island Press, Washington (2004)
Spessa, A.; Mcbeth, B.; Thonicke, K.; Prentice, I. C.: Modelling the relationship between fire frequency, rainfall and vegetation in the Kimberleys region Australia, using a fire model coupled to a DGVM. In: Proceedings of the 3rd International Wildland Fire Conference, 4-6 Oct. 2003, Sydney (Hg. Goldammer, J.; Viegas, D.) (2003)
Guiot, J.; Prentice, I. C.; Peng, C.; Jolly, D.; Laarif, F.; Smith, B.: Reconstruction and modelling past changes in terrestrial primary production. In: Terrestrial global productivity, S. 479 - 498 (Hg. Roy, J.; Saugier, B.; Mooney, H. A.). Academic Press, San Diego (2001)
Prentice, I. C.: Max-Planck-Institut für Biogeochemie. In: Jahrbuch 2001 der Max-Planck-Gesellschaft zur Förderung der Wissenschaften, S. 427 - 435. Vandenhoeck & Ruprecht, Göttingen (2001)
Prentice, I. C.: Interactions of climate change and the terrestrial biosphere. In: Geosphere-biosphere interactions and climate, S. 176 - 198 (Hg. Bengtsson, L.; Hammer, C. U.). Pontifical Academy of Sciences, Cambridge (2001)
Prentice, I. C.; Farquhar, G. D.; Fasham, M. J. R.; Goulden, M. L.; Heimann, M.; Jaramillo, V. J.; Kheshgi, H. S.; Le Quéré, C.; Scholes, R. J.; Wallace, D. W. R.: The carbon cycle and atmospheric carbon dioxide. In: Climate Change 2001: the scientific basis, S. 183 - 237 (Hg. Houghton, J. T.; Ding, Y.; Griggs, D. J.; Noguer, M.; Van Der Linden, P. J. et al.). Cambridge University Press, Cambridge (2001)
Prentice, I. C.; Raynaud, D.: Palaeobiogeochemistry. In: Global biogeochemical cycles in the climate system, S. 87 - 94 (Hg. Schulze, E.-D.; Harrison, S. P.; Heimann, M.; Holland, E. A.; Lloyd, J. et al.). Academic Press, San Diego (2001)
Wallace, D. W. R.; Prentice, I. C.; Schimel, D.: The global carbon cycle. In: Contributions to global change research, S. 22 - 29 (Hg. Heinen, D.). German National Committee on Global Change Research, Bonn (2001)
Francois, L.; Kaplan, J. O.; Otto, D.; Roelandt, C.; Harrison, S. P.; Prentice, I. C.; Warnant, P.; Ramstein, G.: Comparison of vegetation distributions and terrestrial carbon budgets reconstructed for the last glacial maximum with several biosphere models. In: Paleoclimate Modelling Intercomparison Project (PMIP). Proceedings of the third PMIP workshop, La Huardière, Canada, 4-8 October 1999, S. 141 - 145 (Hg. De Vernal, A.; Braconnot, P.; Joussaume, S.; Taylor, K.) (2000)
Schulze, E.-D.; Prentice, I. C.: Max-Planck-Institut für Biogeochemie. In: Jahrbuch 2000 der Max-Planck-Gesellschaft zur Förderung der Wissenschaften, S. 457 - 464. Vandenhoeck & Ruprecht, Göttingen (2000)
Yu, G.; Sun, X.; Qin, B.; Song, C.; Li, H.; Prentice, I. C.; Harrison, S. P.: Pollend-based reconstruction of vegetation patterns of China in Mid-Holocene. In: Proceedings for the 60th Anniversary of the Founding of Nanjing Institute of Geography and Limnology, S. 369 - 375 (Hg. Nanjing Institute of Geography & Limnology, C.). Chinese Academic of Sciences (III) (2000)
Am 29. April 2025 wurde der BIOMASS-Satellit erfolgreich in die Umlaufbahn gebracht. Die BIOMASS-Mission dient der Kartierung und Überwachung globaler Wälder. Sie soll die Struktur verschiedener Waldtypen kartieren und Daten zur oberirdischen Biomasse liefern.
EU fördert internationales Forschungsprojekt AI4PEX, um Erdsystemmodelle und damit wissenschaftliche Vorhersagen des Klimawandels weiter zu verbessern. Beteiligte Wissenschaftler*innen aus 9 Ländern trafen sich bereits Ende Mai 2024 zum Projektstart am federführenden MPI für Biogeochemie in Jena.
Die Umsatzzeiten des Kohlenstoffs an Land bestimmen die Auswirkungen von Klima-veränderungen auf die Landoberfläche. Die Temperaturempfindlichkeit des Kohlen-stoffumsatzes ist daher von entscheidender Bedeutung. Unsere neue Studie belegt, dass die Feuchtebedingungen die Temperaturempfindlichkeit der Kohlenstoffumsatzzeiten stark verändern.
Diese Pressemitteilung wurde uns freundlicherweise von der TUM zur Verfügung gestellt.
Der Klimawandel bringt Wälder zunehmend unter Druck. Ausgelöst durch Klimaextreme sind in Mitteleuropa in den letzten Jahren große Waldflächen abgestorben. Forschende unter Beteiligung der Technischen Universität München (TUM) haben nun die erste Klimarisikokarte…
A new study shows that future ecosystem functioning will increasingly depend on water availability. Using recent simulations from climate models, an international team of scientists found several “hot spot regions” where increasing water limitation strongly affects ecosystems. These include Central Europe, the Amazon, and western Russia.
Microorganisms in aquifers deep below the earth’s surface produce similar amounts of biomass as those in some marine waters. This is the finding of researchers led by the Friedrich Schiller University Jena and the German Centre for Integrative Biodiversity Research (iDiv). The study has been published in Nature Geoscience.
You can't see them with the naked eye, but our forest ground is littered with microorganisms. They decompose falling leaves, thereby improving soil quality and counteracting climate change. But how do these single-celled organisms coordinate their tasks? An international research team has been looking into this little-understood process. The results of the study were recently published in Scientific Reports.
Scientists have succeeded in detecting changes in carbon dioxide emissions from fossil fuels much faster than before. Using a new method, they combined atmospheric measurements of carbon dioxide (CO2) and oxygen (O2) from the north coast of the United Kingdom. The study, with the participation of the Max Planck Institute for Biogeochemistry, was published Apr. 22 in Science Advances.
International researchers found a pattern of extreme climate conditions leading to forest dieback. To do this, the team had collected worldwide records of climate-related tree and forest dieback events over the past nearly five decades. The results, recently published in Nature Communications, reveal an ominous scenario for forests in the context of ongoing global warming.
International forest experts analyzed major tree and forest dieback events that occurred globally in the last decades in response to climate extremes. To their surprise many forests were strongly affected that were not considered threatened based on current scientific understanding. The study, led by the MPI-BGC and published in Annual Reviews in Plant Biology, underscores also that further tree and forest dieback is likely to occur.
At the Amazon Tall Tower Observatory (ATTO), the research station of a joint German-Brazilian project in the Brazilian rainforest, scientists have been studying the ecosystems of the Amazon and their interactions with the atmosphere and climate for more than 10 years. Recently, representatives of the Brazilian Ministry of Research and foreign ambassadors visited the station.
An international research team succeeded in identifying global factors that explain the diversity of form and function in plants. Led by the University of Zurich, the Max Planck Institute for Biogeochemistry in Jena and the University of Leipzig, the researchers collected and analyzed plant data from around the world.