Ullmann, I.; Lange, O. L.; Ziegler, H.; Ehleringer, J. R.; Schulze, E. D.; Cowan, I. R.: Diurnal courses of leaf conductance and transpiration of mistletoes and their hosts in Central Australia. Oecologia 67 (4), pp. 577 - 587 (1985)
Beck, E.; Schlüter, I.; Scheibe, R.; Schulze, E. D.: Growth rates and population rejuvenation of East African giant groundsels (Dendrosenecia keniodendron). Flora 175 (4), pp. 243 - 248 (1984)
Beck, E.; Schulze, E. D.; Senser, M.; Scheibe, R.: Equilibrium freezing of leaf water and extracellular ice formation in afroalpine "giant rosette" plants. Planta 162 (3), pp. 276 - 282 (1984)
Brinckmann, E.; Tyerman, S. D.; Steudle, E.; Schulze, E. D.: The effect of different growing conditions on water relations parameters of leaf epidermal cells of Tradescantia virginiana L. Oecologia 62 (1), pp. 110 - 117 (1984)
Schulze, E. D.; Bloom, A.: Relationship between mineral nitrogen influx and transpiration in radish and tomato. Plant Physiology 76 (3), pp. 827 - 828 (1984)
Schulze, E. D.; Ehleringer, J. R.: The effect of nitrogen supply on growth and water-use efficiency of sylem tapping mistletoes. Planta 162 (3), pp. 268 - 275 (1984)
Schulze, E. D.; Reif, A.; Küppers, M.: Die pflanzenökologische Bedeutung und Bewertung von Hecken. Berichte der ANL / Hrsg.: Bayerische Akademie für Naturschutz und Landschaftspflege (ANL) Beiheft 3 (Teil 1), pp. 1 - 102 (1984)
Schulze, E. D.; Turner, N. C.; Glatzel, G.: Carbon, water and nutrient relations of two mistletoes and their hosts: A hypothesis. Plant, Cell and Environment 7 (5), pp. 293 - 299 (1984)
Turner, N. C.; Schulze, E. D.; Gollan, T.: Responses of stomata and leaf gas exchange to vapour pressure deficits and soil water content I. Species comparisons at high soil water contents. Oecologia 63 (3), pp. 338 - 342 (1984)
Turner, N. C.; Spurway, R. A.; Schulze, E. D.: Comparison of water potentials measured by in situ psychrometry and pressure chamber in morphologically different species. Plant Physiology 74 (2), pp. 316 - 319 (1984)
Nagarajah, S.; Schulze, E. D.: Responses of Vigna unguiculata (L.) Walp. to atmospheric and soil drought. Australian Journal of Plant Physiology 10 (5), pp. 385 - 394 (1983)
Schulze, E. D.: Photosynthetic CO2 uptake and whole plant growth as related to plant water relations. Berichte der Deutschen Botanischen Gesellschaft 96 (1), pp. 391 - 402 (1983)
Schulze, E. D.; Hall, A. E.; Lange, O. L.; Walz, H.: A portable steady-state porometer for measuring the carbon dioxide and water vapour exchanges of leaves under natural conditions. Oecologia 53 (2), pp. 141 - 145 (1983)
Schulze, E. D.; Schilling, K.; Nagarajah, S.: Carbohydrate partitioning in relation to whole plant production and water use of Vigna unguiculata (L.) Walp. Oecologia 58 (2), pp. 169 - 177 (1983)
Küppers, M.; Hall, A. E.; Schulze, E. D.: Effects of day-to-day changes in root temperature on leaf conductance to water vapour and CO2 assimilation rates of Vigna unguiculata L. Walp. Oecologia 52 (1), pp. 116 - 120 (1982)
Benecke, U.; Schulze, E. D.; Matyssek, R.; Havranek, W. M.: Environmental control of CO2-assimilation and leaf conductance in Larix decidua Mill. I. A comparison of contrasting natural environments. Oecologia 50, pp. 54 - 61 (1981)
Tomos, A. D.; Steudle, E.; Zimmermann, U.; Schulze, E. D.: Water relations of leaf epidermal cells of Tradescantia virginiana. Plant Physiology 68 (5), pp. 1135 - 1143 (1981)
Farquhar, G. D.; Schulze, E. D.; Küppers, M.: Responses to humidity by stomata of Nicotiana glauca L. and Corylus avellana L. are consistent with the optimization of carbon dioxide uptake with respect to water loss. Australian Journal of Plant Physiology 7 (3), pp. 315 - 327 (1980)
Hall, A. E.; Schulze, E. D.: Drought effects on transpiration and leaf water status of cowpea in controlled environments. Australian Journal of Plant Physiology 7 (2), pp. 141 - 147 (1980)
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.
Since the first measurement flight in 1994, the European research infrastructure IAGOS has developed a measurement technique that is used in commercial airplanes and regularly provide extensive climate data from the atmosphere.
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.
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.
Nitrogen fertilizers and nitrogen oxides from fossil fuels pollute the air and drinking water, lead to the over-fertilization of water bodies and terrestrial ecosystems, reduce biodiversity and damage the ozone layer. On balance, however, they have a cooling effect on the climate.