In the Earth, the dynamo action is strongly linked to core freezing. There is a solid inner core, the growth of which provides a buoyancy flux that drives the dynamo. The buoyancy in this case derives from a difference in composition between the solid inner core and the fluid outer core. In planetary bodies smaller than the Earth, however, this core differentiation process may differ - Fe may precipitate at the core-mantle boundary (CMB) rather than in the center and may fall as iron snow and initially remelt with greater depth. A chemical stable sedimentation zone develops that comprises with time the entire core - at that time a solid inner core starts to grow. The dynamics of this system is not well understood and also whether it can generate a magnetic field or not. The Jovian moon Ganymede, which shows a present-day magnetic dipole field, is a candidate for which such a scenario has been suggested. We plan to study this Fe-snow regime with both a numerical and experimental approach. In the numerical study, we use a 2D/3D thermo-chemical convection model that considers crystallization and sinking of iron crystals together with the dynamics of the liquid core phase (for the 3D case the influence of the rotation of the Fe snow process is further studied).The numerical calculations will be complemented by two series of experiments: (1) investigations in metal alloys by means of X-ray radioscopy, and (2) measurements in transparent analogues by optical techniques. The experiments will examine typical features of the iron snow regime. On the one hand they will serve as a tool to validate the numerical approach and on the other hand they will yield important insight into sub-processes of the iron snow regime, which cannot be accessed within the numerical approach due to their complexity.
Goal of the project EcoTopTen 2.0 is increasing the supply and demand for highly energy-efficient ecological products and to motivate consumers through targeted Actions, to reduce greenhouse gas emissions and to relieve the environment. Importantelements are the regular update of EcoTopTen market overviews, cooperations with retailers, the action 'Save 1000 kWh', as well as accompanying social media activities.
Das Projekt DICES analysiert und entwickelt für kleine Inselstaaten (SIDS) Optionen der lokalen Implementierung von Küstenschutzstrategien als notwendige Anpassungsmaßnahmen im Zuge des projektierten Meeresspiegelanstiegs in ihrer ganzen gesellschaftlichen Breite. In Kooperation zwischen Küsteningenieuren, Umweltökonomen und Integrativen Geographen werden kommunales Handeln (societal action) in seiner kulturellen Rahmung untersucht, potentiell einsetzbare 'low-regret'- Strategien im Küstenschutz ermittelt und die Bereitschaft des bürgerlichen Engagements vor Ort an ausgewählten Fallstudien analysiert. Formelle und informelle Institutionen spielen bei der aktiven Umsetzung von Anpassungsmaßnahmen eine genauso wichtige Rolle wie die Bereitschaft der betroffenen Küstengemeinden, sich an alternativen, lokalen Konzepten und darauf fußenden möglichen infrastrukturellen Vorkehrungen zum Küstenschutz zu beteiligen. Daher wird ein besonderer Fokus auf den gesellschaftlichen und politischen Rahmenbedingungen (political reaction) liegen, unter denen Klimaanpassungsmaßnahmen überhaupt wahrgenommen und ergriffen werden können. Das Projekt verbindet auf methodischer und auf inhaltlicher Ebene die aktuelle Diskussion über einen klimawandelbedingten bzw. relativen Anstieg des Meeresspiegels und seine Auswirkungen auf lokaler Ebene mit der Diskussion über Handeln vor Ort als lokale Anpassungsstrategie an global bedingte Veränderungsprozesse. Im Rahmen der Untersuchung von zwei unterschiedlichen kleinen Inselstaaten werden existierende Governance-Strukturen analysiert und mit potentiellen, auf Basis probabilistischer Ansätze entwickelten Handlungsoptionen abgeglichen. Die Fallstudie Malediven wird dabei stellvertretend für einen eher top-down induzierten Governance-Ansatz untersucht, während Papua-Neuguinea mit seiner spezifischen politischen und gesellschaftlichen Organisation für den entgegen gesetzten, vornehmlichen bottom-up Ansatz des bürgerlichen Engagements steht. Die eingesetzte methodische Bandbreite reicht von Haushaltsbefragungen, Choice- und Feldexperimenten über numerische Modellierungen bis hin zu Fokusgruppen-Diskussionen mit Schlüsselpersonen (policy entrepreneurs) des Küstenschutzes. Die unterschiedlichen methodischen Instrumentarien werden integrativ entwickelt und weitgehend parallel in beiden Fallstudien eingesetzt. In der Synthesephase des Projektes werden die Ergebnisse auf Gemeinsamkeiten und Unterschiede hin untersucht und die interdisziplinäre Verschränkung des eingesetzten Methodenkanons kritisch evaluiert. Damit leistet das Projekt einen wichtigen Beitrag zur fallstudienorientierten Analyse von Hemmnissen und Potentialen zum Umgang mit dem Meeresspiegelanstieg als eine Art lokale Bewältigungsstrategie. Die gewonnenen Ergebnisse werden auf ihre Übertragbarkeit hin überprüft und für die internationale SIDS Diskussion fruchtbar gemacht.
Klage der Deutschen Umwelthilfe (DUH) gegen Ausnahmegenehmigung, Schutz des Mosel-Apollofalters, Zahl der Ausnahmegenehmigungen, Gerichtsverfahren; Berichterstattung der Landesregierung im Ausschuss für Landwirtschaft und Weinbau
Aims: Floods in small and medium-sized river catchments have often been a focus of attention in the past. In contrast to large rivers like the Rhine, the Elbe or the Danube, discharge can increase very rapidly in such catchments; we are thus confronted with a high damage potential combined with almost no time for advance warning. Since the heavy precipitation events causing such floods are often spatially very limited, they are difficult to forecast; long-term provision is therefore an important task, which makes it necessary to identify vulnerable regions and to develop prevention measures. For that purpose, one needs to know how the frequency and the intensity of floods will develop in the future, especially in the near future, i.e. the next few decades. Besides providing such prognoses, an important goal of this project was also to quantify their uncertainty. Method: These questions were studied by a team of meteorologists and hydrologists from KIT and GFZ. They simulated the natural chain 'large-scale weather - regional precipitation - catchment discharge' by a model chain 'global climate model (GCM) - regional climate model (RCM) - hydrological model (HM)'. As a novel feature, we performed so-called ensemble simulations in order to estimate the range of possible results, i.e. the uncertainty: we used two GCMs with different realizations, two RCMs and three HMs. The ensemble method, which is quite standard in physics, engineering and recently also in weather forecasting has hitherto rarely been used in regional climate modeling due to the very high computational demands. In our study, the demand was even higher due to the high spatial resolution (7 km by 7 km) we used; presently, regional studies use considerably larger grid boxes of about 100 km2. However, our study shows that a high resolution is necessary for a realistic simulation of the small-scale rainfall patterns and intensities. This combination of high resolution and an ensemble using results from global, regional and hydrological models is unique. Results: By way of example, we considered the low-mountain range rivers Mulde and Ruhr and the more alpine Ammer river in this study, all of which had severe flood events in the past. Our study confirms that heavy precipitation events will occur more frequently in the future. Does this also entail an increased flood risk? Our results indicate that in any case, the risk will not decrease. However, each catchment reacts differently, and different models may produce different precipitation and runoff regimes, emphasizing the need of ensemble studies. A statistically significant increase of floods is expected for the river Ruhr in winter and in summer. For the river Mulde, we observe a slight increase of floods during summer and autumn, and for the river Ammer a slight decrease in summer and a slight increase in winter.
Fragmentation of the natural environment has contributed to major biodiversity loss in South East Asia. Reptiles represent a significant biomass and occupy important functions in our ecosystem. However, these organisms are highly sensitive to relatively minor changes in temperature and habitat alteration. In this study we will investigate the effects of habitat fragmentation and potentially climate change on agamids at several sites in Southeast Asia. We will identify the species richness of agamids, their habitat use, and their diet. By using morphometrics, we aim to correlate morphology and habitat use and diet to explore the ecological niches these lizards occupy. We will also test for microhabitat preferences and optima to understand the ecological impacts on these species caused by forest fragmentation. We hope to use this approach to lay the foundations for macro-ecological modelling proving insights into future distributions and the impact of habitat connectivity.
Cherry leaf roll virus (CLRV) is a plant pathogen of economic and ecologic importance. It is globally distributed in a wide range of forest, fruit, and ornamental trees and shrubs. In several areas of cherry and walnut production CLRV causes severe losses in yield and quality. With current reference to the rapid dissemination and strong symptom expression in Finnish birches and the Germany-wide distribution of CLRV in birches and elderberry, we continuously investigate and gradually reveal CLRV transmission pathways as by pollen, seeds or water. However, modes and interactions responsible for the wide intergeneric host transmission as well as for the exceptional CLRV epidemic in Fennoscandia still remain unknown. In this project systematic studies shall investigate biological vectors as a causal agent to finally derive control mechanisms and strategies to avoid new epidemics in different hosts and geographic regions. Detailed monitoring of the invertebrate fauna of birch stands/forests and elderberry plantations in Germany and Finland shall reveal potential vectors to subsequently study them in detail by approved virus detection methods and transmission experiments. Molecular analyses of the CLRV coat protein shall prove its role as a viral determinant for a virus/vector interaction. Consequently, this project essentially will contribute important answers on the CLRV epidemiology, and this will be a key element within the first network of research on plant viral pathogens in forest trees.
Nutrient and water supply for organisms in soil is strongly affected by the physical and physico-chemical properties of the microenvironment, i.e. pore space topology (pore size, tortuosity, connectivity) and pore surface properties (surface charge, surface energy). Spatial decoupling of biological processes through the physical (spatial) separation of SOM, microorganisms and extracellular enzyme activity is apparently one of the most important factors leading to the protection and stabilization of soil organic matter (SOM) in subsoils. However, it is largely unknown, if physical constraints can explain the very low turnover rates of organic carbon in subsoils. Hence, the objective of P4 is to combine the information from the physical structure of the soil (local bulk density, macropore structure, aggregation, texture gradients) with surface properties of particles or aggregate surfaces to obtain a comprehensive set of physical important parameters. It is the goal to determine how relevant these physical factors in the subsoil are to enforce the hydraulic heterogeneity of the subsoil flow system during wetting and drying. Our hypothesis is that increasing water repellency enforces the moisture pattern heterogeneity caused already by geometrical factors. Pore space heterogeneity will be assessed by the bulk density patterns via x-ray radiography. Local pattern of soil moisture is evaluated by the difference of X-ray signals of dry and wet soil (project partner H.J. Vogel, UFZ Halle). With the innovative combination of three methods (high resolution X-ray radiography, small scale contact angle mapping, both applied to a flow cell shaped sample with undisturbed soil) it will be determined if the impact of water repellency leads to an increase in the hydraulic flow field heterogeneity of the unsaturated sample, i.e. during infiltration events and the following redistribution phase. An interdisciplinary cooperation within the research program is the important link which is realized by using the same flow cell samples to match the spatial patterns of physical, chemical, and biological factors in undisturbed subsoil. This cooperation with respect to spatial pattern analysis will include the analysis of enzyme activities within and outside of flow paths and the spatial distribution of key soil properties (texture, organic carbon, iron oxide content) evaluated by IR mapping. To study dissolved organic matter (DOM) sorption in soils of varying mineral composition and the selective association of DOM with mineral surfaces in context with recognized flow field pattern, we will conduct a central DOM leaching experiment and the coating of iron oxides which are placed inside the flow cell during percolation with marked DOM solution. Overall objective is to elucidate if spatial separation of degrading organisms and enzymes from the substrates may be interconnected with defined physical features of the soil matrix thus explaining subsoil SOM stability and -dynami
In the Bavarian Forest National Park a brief, but intense storm event on 1 August 1983 created large windfall areas. The windfall ecosystems within the protection zone of the park were left develop without interference; outside this zone windfall areas were cleared of dead wood but not afforested. A set of permanent plots (transect design with 10 to 10 m plots) was established in 1988 in spruce forests of wet and cool valley bottoms in order to document vegetation development. Resampling shall take place every five years; up to now it was done in 1993 and 1998. On cleared areas an initial raspberry (Rubus idaeus) shrub community was followed by pioneer birch (Betula pubescens, B. pendula) woodland, a sequence well known from managed forest stands. In contrast to this, these two stages were restricted to root plates of fallen trees in uncleared windfalls; here shade-tolerant tree species of the terminal forest stages established rather quickly from saplings that had already been present in the preceeding forest stand. Soil surface disturbances are identified to be causal to the management pathway of forest development, wereas the untouched pathway is caused by relatively low disturbance levels. The simulation model FORSKA-M is used to analyse different options of further stand development with a simulation time period of one hundred years.
Background: An increasing frequency of massive flooding along the lower Yangtse River in China ended in a disastrous catastrophe in summer 1998 leaving several thousand people homeless, more than 3.600 dead and causing enormous economic damage. Inappropriate land-use techniques and large scale timber felling in the water catchment of the upper Yangtse and its feeder streams were stated to be the main causes. Immediate timber cutting bans were imposed and investigations on land use patterns were initiated by the Chinese Government. The Institute for World Forestry of the Federal Research Centre for Forestry and Forest Products was approached by the Yunnan Academy of Forestry in Kunming to exchange experiences and to cooperate scientifically in the design and application of appropriate afforestation and silvicultural management techniques in the water catchment area of the Yangtse. This cooperation was initiated in 1999 and is based on formal agreements in the fields of agrarian research between the German and Chinese Governments. Objectives: The cooperation was in the first step focussing on the identification of factors which caused the enormous floodings. After their identification measures of prevention were determined and put into practice. In this context experiences made in past centuries in the alpine region of central Europe served as an incentive and example for similar environmental problems and solutions under comparable conditions. Relevant key questions of the cooperation project were: - Analysis of forest related factors influencing the recent floodings of the Yangtse, - Analysis and evaluation of silvicultural management experiences from central Europe for know-how transfer, - Evaluation of rehabilitation measures for successful application in Yunnan, - Dissemination of knowledge through vocational training. Results: - Frequent wild grazing of husbandry is a key factor for forest degeneration beyond unsustainable timber harvests, forest fires and insect calamities leading to increased water run-off in the mountainous region of Yunnan; - Browsing of cattle interrupts succession thus avoiding natural regeneration and leaving a logging ban ineffective; - Mountain pasture in the Alps had similar effects in the past in central Europe. The introduction of controlled grazing has led to an ecologically compatible coexistence of pasture and ecology. Close-to-nature forestry can have positive effects in this sensitive environment. - Afforestation with site adopted broadleaves and coniferous tree species was implemented on demonstration level using advanced techniques in Yunnan.
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