Titlebook: Biogeochemistry of Forested Catchments in a Changing Environment; A German Case Study Egbert Matzner Book 2004 Springer-Verlag Berlin Heide

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Introduction to ‘Connecting Peace and War’imate change as a global and hemispherical phenomenon (macro-scale) is an example. On smaller scales, the atmosphere interacts intensively with terrestrial ecosystems, and thus plays a key role in ecosystem processes. An important example is the input of liquid water through precipitation, which is

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Introduction on the ‘State of the State’logy. While leaves and their stomata are the causal agents of stand transpiration and canopy conductance, and their position and orientation are known to be decisive for their gas-exchange contribution, the spatial distribution pattern of leaves inside a forest cannot yet be considered in stand gas-

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,Kalkulation mit Deckungsbeiträgen, release of terrestrial ecosystems. Whether temperate ecosystems will act as sources or sinks of carbon under altered environmental conditions depends on the way in which the balance of these processes is shifted in the short term, and in the long term. Soils of forest ecosystems are generally regar

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https://doi.org/10.1007/978-3-658-05199-0 if the assimilation is larger than the respiration. Alternatively, increasing temperatures due to climate change (IPCC 2001) may be a reason for increasing respiratory fluxes. While low-altitude spruce sites in Germany are significant carbon sinks (e.g. Bernhofer et al. 2003), sites above 600 m a.s

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Elmar Bräkling,Jörg Lux,Tobias Udingnteith 1980) which is based on the energy balance equation. This method describes the interaction with the surface by a resistance approach and relies on the constant flux layer approach which is equivalent to the classical K approach (see, e.g., Stull 1988; Kramm 1995). The PM method is mainly forc