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)
The BIOMASS satellite was successfully launched into orbit on 29 April 2025. The BIOMASS mission is designed to map and monitor global forests. It will map the structure of different forest types and provide data on above-ground biomass.
Thanks to FLUXCOM-X, the next generation of data driven, AI-based earth system models, scientists can now see the Earth’s metabolism at unprecedented detail – assessed everywhere on land and every hour of the day.
Extreme climate events endanger groundwater quality and stability, when rain water evades natural purification processes in the soil. This was demonstrated in long-term groundwater analyses using new analytical methods.
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.
David Hafezi Rachti was awarded twice: for his EGU poster with this year’s “Outstanding Student and PhD candidate Presentation” (OSPP) and for his Bachelor thesis, he received the 1st prize of the “Young Climate Scientist Award 2024”.
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 recent study by scientists from the Max Planck Institute for Biogeochemistry and the University of Leipzig suggests that increasing droughts in the tropics and changing carbon cycle responses due to climate change are not primarily responsible for the strong tropical response to rising temperatures. Instead, a few particularly strong El Niño events could be the cause.