Aubinet, M.; Feigenwinter, C.; Heinesch, B.; Bernhöfer, C.; Canepa, E.; Lindroth, A.; Montagnani, L.; Rebmann, C.; Sedlak, P.; Van Gorsel, E.: Direct advection measurements do not help to solve the night-time CO2 closure problem: Evidence from three different forests. Agricultural and Forest Meteorology 150 (5), pp. 655 - 664 (2010)
Rebmann, C.; Zeri, M.; Lasslop, G.; Mund, M.; Kolle, O.; Schulze, E. D.; Feigenwinter, C.: Treatment and assessment of the CO2-exchange at a complex forest site in Thuringia, Germany. Agricultural and Forest Meteorology 150 (5), pp. 684 - 691 (2010)
Zeri, M.; Rebmann, C.; Feigenwinter, C.; Sedlake, P.: Analysis of periods with strong and coherent CO2 advection over a forested hill. Agricultural and Forest Meteorology 150 (5), pp. 674 - 683 (2010)
Merbold, L.; Kutsch, W. L.; Corradi, C.; Kolle, O.; Rebmann, C.; Stoy, P. C.; Zimov, S. A.; Schulze, E.-D.: Artificial drainage and associated carbon fluxes (CO2/CH4) in a tundra ecosystem. Global Change Biology 15 (11), pp. 2599 - 2614 (2009)
Moderow, U.; Aubinet, M.; Feigenwinter, C.; Kolle, O.; Lindroth, A.; Molder, M.; Montagnani, L.; Rebmann, C.; Bernhofer, C.: Available energy and energy balance closure at four coniferous forest sites across Europe. Theoretical and Applied Climatology 98 (3-4), pp. 397 - 412 (2009)
Moyano, F. E.; Kutsch, W. L.; Rebmann, C.: Soil respiration fluxes in relation to photosynthetic activity in broad-leaf and needle-leaf forest stands. Agricultural and Forest Meteorology 148 (1), pp. 135 - 143 (2008)
Göckede, M.; Rebmann, C.; Foken, T.: A combination of quality assessment tools for eddy covariance measurements with footprint modelling for the characterisation of coplex sites. Agricultural and Forest Meteorology 127 (3-4), pp. 175 - 188 (2004)
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.
Land surface temperatures are shaped mostly by the heating by sunlight, but also by evaporation and convective heat transfer in the vertical. A new study determined the role of these two processes by employing a physical limit.
Axel Kleidon discusses contemporary issues relating to the Earth system, thermodynamics, energy conversion, and the water cycle, and explains the current state of scientific knowledge in these areas.