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Savanna regions in West Africa are valuable cultural landscapes and provide a wide range of ecosystem services for human well-being and are frequently affected by human-induced disturbances. Aside from agricultural activities (crop production and animal husbandry), the harvesting of timber and non-timber forest products is crucial for household income, alimentation and medicinal purposes. Most indigenous woody species have undergone increasing anthropogenic pressure as social and economic conditions have changed dramatically during recent decades, resulting in further habitat fragmentation and increased disturbance severity. Human land use activities influence growth conditions for plants by altering various abiotic factors, such as light, nutrient availability and water supply. They are found to alter demographic parameters (e.g., germination, seedling and sapling growth, survival and mortality rates) of woody plant individuals and alter the structure and stability of populations. The degree of anthropogenic disturbance varies between land-cover types, distance to settlements, and protection status. In the context of land-use change, there is an urgent need to better understand and evaluate the impact of land-use on savanna vegetation, particularly on the population biology of common savanna woody species. A major conclusion to be drawn from this thesis is that land use influences savanna vegetation in a complex way and does not necessarily lead to a decline or loss of tree populations and species. It is rather that in a constantly changing landscape, as a result of human-induced disturbances, populations of ubiquitous and some common species can be stable over time. The abundance of some species tends to decline consistently, whereas others benefit from human disturbance. Moreover, the study provides an insight into the structure and dynamics of common, dominant and less dominant savanna woody plants in a communal and a protected area. There is a need for further basic studies to assess the impact of land use and ecological preferences of all species, including repeated density studies that look at survivorship and transition probabilities over a number of seasons as well as longterm in-situ experiments in settlement areas in order to better understand woody plant populations in settlement areas as the few remaining semi-natural sites are likely to decrease in the future. A challenge will be the development of strategies to protect species within a landscape under cultivation.
An exciting in vivo function of ATP-sensitive potassium channels in substantia nigra dopamine neurons Ð Implications for burst firing and novelty coding ÐPhasic burst activity is a key feature of dopamine (DA) midbrain neurons. This particular pattern of excitation of DA neurons occurs via a synaptically triggered transition from low-frequency background spiking to transient high-frequency discharges. Burst-firing mediated phasic DA release is critical for flexible switching of behavioural strategies in response to unexpected rewards, novelty and other salient stimuli. However, the cellular and molecular bases of burst signalling in distinct DA subpopulations of the substantia nigra (SN) or the ventral tegmental area (VTA) are unknown.
DA neuron excitability is controlled by synaptic network inputs, neurotransmitter receptors and ion channels, which generate action potentials and determine frequency and pattern of electrical activity in a complex interplay. ATP-sensitive potassium (K-ATP) channels are widely expressed throughout the brain, where in most cases they are believed to act as metabolically-controlled 'excitation brakes' by matching excitability to cellular energy states. However, their precise physiological in vivo function in DA neurons remains elusive.
To study burst firing and the underlying ionic mechanisms with single cell resolution, in vivo single-unit recordings were combined with juxtacellular neurobiotin labelling as well as immunohistochemical and anatomical identification of individual DA neurons. In vivo recordings were performed in adult isoflurane-anaesthetised wildtype (WT) and global K-ATP channel knockout mice, lacking the pore forming Kir6.2 subunit (Kir6.2-/-). In addition, DA cell-selective functional silencing of K-ATP channel activity in vivo was established using virus-mediated expression of dominant-negative Kir6.2 subunits. Careful control experiments ruled out any significant contributions from nonDA neurons as transduction was effectively limited to SN DA neurons rather than affecting those cells that innervate them. Virus-based K-ATP channel silencing in combination with juxtacellular recording and labelling was achieved to define the electrophysiological phenotype of individually identified, virally-transduced DA neurons in vivo.
Single-unit recordings revealed that K-ATP channels Ð in contrast to their conventional hyperpolarising role Ð in a subpopulation of DA neurons located in the medial SN (m-SN) act as cell-type selective gates for excitatory burst firing in vivo. The percentage of spikes in bursts was threefold reduced in Kir6.2-/- compared to WT mice. Classification of firing patterns based on visual inspection of autocorrelation histograms and on a newly developed spike-train-model confirmed the dramatic shift from phasic burst to tonic single-spike oscillatory firing in Kir6.2-/-. This significant decrease of burstiness was selective for m-SN DA neurons and was not exhibited by DA cells in the lateral SN or VTA. Virus-based K-ATP channel silencing in vivo unequivocally demonstrated that the activity of postsynaptic K-ATP channels was sufficient to disrupt bursting in m-SN DA neuron subtypes. Patch-clamp recordings in brain slices indicated an essential role of K-ATP channels for NMDA-mediated in vitro bursting. In accordance with previous studies in DA midbrain neurons, NMDA receptor stimulation triggered burst-like firing in m-SN DA cells in vitro, but only when K-ATP channels were co-activated in these neurons.
K-ATP channel-gated burst firing in m-SN DA neurons might be functionally relevant in awake, freely moving mice. To explore the behavioural consequences of SN DA neuron subtype-selective K-ATP channel suppression, spontaneous open field (OF) behaviour of mice with bilateral K-ATP silencing across the whole SN (medial + lateral) or in only the lateral SN was tested. Analysis of WT and global Kir6.2-/- mice showed reduced exploratory locomotor activity of Kir6.2-/- in a novel OF environment. Remarkably, K-ATP channel silencing in m-SN DA neurons phenocopied this novelty-exploration deficit, indicating that K-ATP channel-gated burst firing in medial but not lateral SN DA neurons is crucial for WT-like novelty-dependent exploratory behaviour.
In summary, a novel role of K-ATP channels in promoting the excitatory switch from tonic to phasic firing in vivo in a cell-type specific manner was discovered. The present PhD thesis provides several important insights into the pivotal function of K-ATP channels in medial SN DA cells, which project to the dorsomedial striatum, for burst firing and its important consequences for context-dependent exploratory behaviour.
In collaboration with two other research groups transcriptional up-regulation of K-ATP channel and NMDA receptor subunits and high levels of in vivo burst firing were detected in surviving SN DA neurons from Parkinson's disease (PD) patients Ð providing a potential link of K-ATP channel activity to neurodegenerative pathomechanisms of PD. Using high-resolution fMRI imaging another study in humans has recently identified distinct DA midbrain regions that are preferentially activated by either reward or novelty. Taken together, these human data and the results of the present PhD thesis suggest that burst-gating K-ATP channel function in SN DA neurons impacts on phenotypes in disease as well as in health.
The role of the Ca2+-dependent protease calpain in the diabetes-associated platelet hyperreactivity
(2012)
Platelets from diabetic patients are characterised by hyperreactivity resulting in exaggerated adhesion, aggregation and thrombus formation which contribute to the development of cardiovascular complications known to be one of the main causes of diabetes-related mortality. One of the mechanisms suggested to be involved in the diabetes-related platelet hyperactivation is the increased [Ca2+]i which leads to the overactivation of Ca2+-dependent proteases, the calpains. Among the calpain isoforms expressed in platelets the two ubquitiously expressed μ- and m-calpain are thought to play an important role in physiological and pathophysiological processes. Particularly μ-calpain is known to be involved in many steps of physiological platelet activation such as aggregation, adhesion, secretion, and signalling. However, we could show that diabetes was associated with an enhanced activation of both μ- and m-calpain in platelets
In the first part of the study we focussed on the characterization of the molecular mechanism regulating calpain activity. Indeed, although Ca2+ is considered to be the main regulator of the proteolytic activity of the conventional calpains, other mechanisms such as the presence of phospholipids and phosphorylation have been reported to affect their activity. Since most studies reported the phosphorylation of m-calpain we were interested to see whether μ-calpain activity might be also affected by phosphorylation. We could show that the activity of μ-calpain was enhanced by the PKC activator PMA suggesting its possible regulation by phosphorylation. However, whether PKC directly targeted μ-calpain remains unclear. Given that substrate recognition is important for a protease to process its substrate and since no common consensus could be attributed to calpain substrates, our next interest was to understand the mechanism regulating the recognition of its substrates by calpain. Since phosphorylation has been reported to protect different proteins from calpain degradation we investigated whether the calpain substrate CD31 could be phosphorylated in platelets and whether this could affect its recognition by calpain. Although we could show that the tyrosine phosphorylation of CD31 was increased after activation of platelets by thrombin and that this effect was attenuated in platelets from diabetic patients, tyrosine phosphorylation of CD31 seemed to have no effect on its sensitivity to calpain-mediated proteolysis.
After the analysis of the mechanism regulating calpain activity as well as its interaction with its substrates, our next interest was the identification of new calpain substrates in platelets. Since a previous study from our group showed that PPARγ agonists could indirectly reverse the diabetes-associated calpain activation we performed DIGE analysis of platelet samples from diabetic patients before and after PPARγ agonist treatment. Using this approach we could identify four novel calpain substrates in platelets: Integrin-linked kinase (ILK), α parvin, CLP36 and septin-5. Next, we assessed the effect of calpain-mediated cleavage on the function of these newly identified proteins. We could show that μ-calpain was essential for the dissociation of ILK from the IPP complex and its activation while m-calpain-mediated cleavage led to its cleavage and inactivation. Functionally, we also showed that μ-calpain was involved in platelet adhesion while m-calpain was important for spreading.
The next protein we analysed was septin-5, a small GTPase known to regulate platelet degranulation by association with other septins and syntaxin-4. We found that the interaction between septin-5 and syntaxin-4 was inhibitory for platelet degranulation. We could demonstrate that the μ-calpain-mediated cleavage dissociated septin-5 from syntaxin 4 and led to increased secretion of platelet α-granules. Next, we investigated the in vivo role of calpain in the diabetes-associated platelet hyperreactivity. We induced diabetes in mice and could reproduce calpain activation in platelets such as that found in human. Indeed, calpain activation in murine platelets also led to the cleavage of several calpain substrates including ILK and septin-5. Moreover, platelets from diabetic mice demonstrated an increased aggregation and thrombus formation in vivo. Treatment of the animals with the calpain inhibitor A-705253 (30 mg/kg/day for 10 days) significantly restored platelet function and substrate cleavage. In conclusion, in this part of the study, we could show that the increased calpain-dependent α-granule secretion and platelet adhesion may account for the enhanced vascular proliferation and thrombus formation in diabetes and calpain inhibition represents a promising way to prevent atherothrombosis development.
In the last part of the study we analysed another enzyme known to play a crucial role in diabetes, the AMPK which is an energy-sensing kinase known to be impaired in diabetes. We could show that the two catalytic subunits AMPK α1 and α2 are expressed in platelets. The AMPKα2 seemed to be the subunit involved in platelet activation since AMPKα2-deficient mice demonstrated a defect in clot retraction and the stabilization of the thrombus while the animals showed a normal bleeding time. Mechanistically, we showed in platelets that the upstream kinase of AMPKα2 is LKB1 which was activated by thrombin stimulation via a PI-3K-dependent pathway. AMPKα2 then phosphorylated the Src-family kinase Fyn, which is responsible for the phosphorylation of its substrate β3 integrin on Tyr747. These data indicate that AMPKα2, by affecting Fyn phosphorylation and activity, plays a key role in platelet αIIbβ3 integrin signalling, leading to clot retraction and thrombus stability. Although the effect of diabetes in the AMPK-dependent pathway could not be investigated we assume that the dysregulation of this pathway may account for the thrombus destabilization and enhanced embolization encountered in diabetes.
In this thesis, various aspects on the theoretical description of ultracold bosonic atoms in optical lattices are investigated. After giving a brief introduction to the fundamental concepts of BECs, atomic physics, interatomic interactions and experimental procedures in chapter (1), we derive the Bose-Hubbard model from first principles in chapter (2). In this chapter, we also introduce and discuss a technique to efficiently determine Wannier states, which, in contrast to current techniques, can also be extended to inhomogeneous systems. This technique is later extended to higher dimensional, non-separable lattices in chapter (5). The many-body physics and phases of the Bose-Hubbard is shortly presented in chapter (3) in conjunction with Gutzwiller mean-field theory, and the recently devised projection operator approach. We then return to the derivation of an improved microscopic many-body Hamiltonian, which contains higher band contributions in the presence of interactions in chapter (4). We then move on to many-particle theory. To demonstrate the conceptual relations required in the following chapter, we derive Bogoliubov theory in chapter (5.3.4) in three different ways and discuss the connections. Furthermore, this derivation goes beyond the usual version discussed in most textbooks and papers, as it accounts for the fact, that the quasi-particle Hamiltonian is not diagonalizable in the condensate and the eigenvectors have to be completed by additional vectors to form a basis. This leads to a qualitatively different quasi-particle Hamiltonian and more intricate transformation relations as a result. In the following two chapters (7, 8), we derive an extended quasi-particle theory, which goes beyond Bogoliubov theory and is not restricted to weak interactions or a large condensate fraction. This quasi-particle theory naturally contains additional modes, such as the amplitude mode in the strongly interacting condensate. Bragg spectroscopy, a momentum-resolved spectroscopic technique, is introduced and used for the first experimental detection of the amplitude mode at finite quasi-momentum in chapter (9). The closely related lattice modulation spectroscopy is discussed in chapter (10). The results of a time-dependent simulation agree with experimental data, suggesting that also the amplitude mode, and not the sound mode, was probed in these experiments. In chapter (11) the dynamics of strongly interacting bosons far from equilibrium in inhomogeneous potentials is explored. We introduce a procedure that, in conjunction with the collapse and revival of the condensate, can be used to create exotic condensates, while particularly focusing on the case of a quadratic trapping potential. Finally, in chapter (12), we turn towards the physics of disordered systems derive and discuss in detail the stochastic mean-field theory for the disordered Bose-Hubbard model.
The ongoing debate on deforestation in the tropics usually points out agriculture and logging as the main causes. The two activities are often linked and the trails created by logging com-panies with their heavy machines are afterwards used by farmers to penetrate deep into the forest and cultivate. Shifting cultivation is a widespread agricultural practice in the tropics and its sustainability is often a matter of controversy. It is necessary to investigate forest recovery after shifting cultivation, analyze its succession stages for comparison with regeneration after natural disturbance, and evaluate its role for discussing the hazards of deforestation.
The study of systems whose properties are governed by electronic correlations is a corner stone of modern solid-state physics. Often, such systems feature unique and distinct properties like Mott metal-insulator transitions, rich phase diagrams, and high sensitivity to subtle changes in the applied conditions. Whereas the standard approach to electronic structure calculations, density functional theory (DFT), is able to address the complexity of real-world materials but is known to have serious limitations in the description of correlations, the dynamical mean-field theory (DMFT) has become an established method for the treatment of correlated fermions, first on the level of minimal models and later in combination with DFT, termed LDA+DMFT.
This thesis presents theoretical calculations on different materials exhibiting correlated physics, where we aim at covering a range in terms of systems --from rather weakly correlated to strongy correlated-- as well as in terms of methods, from DFT calculations to combined LDA+DMFT calculations. We begin with a study on a selection of iron pnictides, a recently discovered family of high-temperature superconductors with varying degree of correlation strength, and show that their magnetic and optical properties can be assessed to some degree within DFT, despite the correlated nature of these systems. Next, extending our analysis to the inclusion of correlations in the framework of LDA+DMFT, we discuss the electronic structure of the iron pnictide LiFeAs which we find to be well described by Fermi liquid theory with regard to many of its properties, yet we see distinct changes in its Fermi surface upon inclusion of correlations. We continue the study of low-energy properties and specifically Fermi surfaces on two more iron pnictides, LaFePO and LiFeP, and predict a topology change of their Fermi surfaces due to the effect of correlations, with possible implications for their superconducting properties. In our last study, we close the circle by presenting LDA+DMFT calculations on an organic molecular crystal on the verge of a Mott metal-insulator transition; there, we find the spectral and optical properties to display signatures of strong electronic correlations beyond Fermi liquid theory.
With the increasing energies and intensities of heavy-ion accelerator facilities, the problem of an excessive activation of the accelerator components caused by beam losses becomes more and more important. Numerical experiments using Monte Carlo transport codes are performed in order to assess the levels of activation. The heavy-ion versions of the codes were released approximately a decade ago, therefore the verification is needed to be sure that they give reasonable results. Present work is focused on obtaining the experimental data on activation of the targets by heavy-ion beams. Several experiments were performed at GSI Helmholtzzentrum für Schwerionenforschung. The interaction of nitrogen, argon and uranium beams with aluminum targets, as well as interaction of nitrogen and argon beams with copper targets was studied. After the irradiation of the targets by different ion beams from the SIS18 synchrotron at GSI, the γ-spectroscopy analysis was done: the γ-spectra of the residual activity were measured, the radioactive nuclides were identified, their amount and depth distribution were detected. The obtained experimental results were compared with the results of the Monte Carlo simulations using FLUKA, MARS and SHIELD. The discrepancies and agreements between experiment and simulations are pointed out. The origin of discrepancies is discussed. Obtained results allow for a better verification of the Monte Carlo transport codes, and also provide information for their further development. The necessity of the activation studies for accelerator applications is discussed. The limits of applicability of the heavy-ion beam-loss criteria were studied using the FLUKA code. FLUKA-simulations were done to determine the most preferable from the radiation protection point of view materials for use in accelerator components.
In dieser Arbeit werden Schmelz- und Anreicherungsprozesse des Erdmantels, sowie Kristallisationsereignisse der Erdkruste zweier ausgewählter Gebiete in Namibia und Spanien mithilfe geochemischer Methoden rekonstruiert und in einen zeitlichen Zusammenhang gebracht. Ein Vergleich der gewonnenen Ergebnisse beider Kompartimente soll dabei weitere Informationen liefern inwieweit Prozesse des Erdmantels und der Erdkruste miteinander verknüpft waren. Insbesondere soll ein weitere Beitrag zur aktuellen Diskussion geliefert werden, bei der sich das sogenannte „pulsed growth“ und „steady accumulation“ Modell gegenüberstehen (siehe Zusammenstellung Pearson et al., 2007). Zudem tragen die neu gewonnenen Daten dazu bei, die regionalen geologischen Gegebenheiten im besonderen Hinblick auf die geotektonische Geschichte besser zu verstehen.
Das Gibeon Kimberlit Feld befindet sich in der tektonischen Einheit des Rehoboth Terranes in Namibia und ist gekennzeichnet von Vulkanismus vor etwa 72.5 Ma (Davies et al., 2001), der Granat Peridotite und krustale Xenolithe mit an die Oberfläche beförderte. Eine klare Einordnung des Rehoboth Terranes in die Gesamtheit des Süd Afrikanischen Plattenverbunds ist noch nicht vollständig geklärt.
Die Südöstliche vulkanische Provinz in Spanien (SEVP) mit besonderem Hinblick auf die Region um Casas de Tallante stellt das zweite Probengebiet für diese Arbeit dar. Vor etwa 2.6 Ma (Bellon et al., 1983) kam es zur Extrusion von alkali-basaltischen Schmelzen, die zahlreiche Spinell / Plagioklas Peridotite mit sich brachten. Tufflagen, sowie die Matrix der Basalte ermöglichen einen Einblick in die untere Kruste der Region.
Untersuchungen der Erdmantelproben aus Namibia auf ihre Haupt- und Spurenelementchemie, sowie Lu-Hf und Sm-Nd Isotopie zeigten, dass zwei verschiedene Manteltypen vorliegen („N“ und „σ“ Typ), die zu einem Zeitpunkt um etwa 850 Ma („N“) und 1.9 Ga („σ“) angereichert wurden. Eine letzte Anreicherung beider Typen fand vermutlich während der Pan–Afrikanischen Orogenese um etwa 450 Ma statt. Die Reinterpretation eines zuvor publizierten Datensatzes (Pearson et al., 2004), suggeriert, dass es zu einer ersten Verarmung der σ Peridotite um etwa 2.9 Ga kam.
Untersuchungen der U-Pb und Hf Isotopie an Zirkonen aus der unteren Kruste des Probengebiets in Namibia ergaben, dass es zur Bildung von juvenilem Krustenmaterial vermutlich bereits im Archaikum kam (wie bereits vorgeschlagen durch z.B. Hoal et al., 1995; Franz et al., 1996), sowie in den Zeiträumen von 2.3 bis 2.7 und 1.5 bis 1.6 Ga, mit jeweils anschließendem krustalem Recycling und Krustenmischung. Eine Übereinstimmung von Mantel- und Krustenevents konnte für die Zeiträume von etwa 1.8, 0.8 - 0.9 Ga und 0.4 – 0.5 Ga gefunden werden. Eine mögliche erste Verarmung des σ Mantels wird bestätigt durch Zirkonalter im Bereich von 2.7 bis 2.9 Ga.
Die Analyse ausgewählter Spinell / Plagioklas Peridotite aus der SEVP, ergaben, dass ein heterogener Mantel mit mindestens 3 verschiedenen Typen vorliegt. Eine Korrelation der Lu-Hf Isotopie von 3 Proben dieses Probensatzes, sowie den Hf Isotopien einer weiteren Probe von Bianchini et al. (2011) suggerieren, dass es eventuell zu einem Verarmungsereignis zu einem Zeitpunkt von etwa 550 Ma kam. Sr Isotopien von Klinopyroxenen und Plagioklasen im Vergleich ergaben, dass die Sr Isotopie der Plagioklase, im Gegensatz zu den Klinopyroxenen, von denen der Alkali Basalte überprägt wurden.
Zirkonanalysen aus Lokalitäten innerhalb der SEVP (U-Pb, Hf) ergaben ein weitreichendes Altersspektrum, beginnend bei etwa 2-3 Ma bis hin ins Archaikum (2.7 bis 2.9 Ga) mit Provenance Ursprung aus Gondwana und dem Arabisch-Nubischen Schild. Die Kombination der U-Pb Altersinformationen mit den entsprechenden Hf Isotopien, zeigten, dass es vermutlich bereits im Archaikum zu juveniler Krustenbildung kam. Zirkone > 100 µm datieren den Zeitpunkt der Eruption der Alkali Basalte mit Altern um etwa 2.6 Ma und Hf Isotopien, die einem leicht verarmten Mantel entsprechen. Ein mögliches Verarmungsereignis im Erdmantel zu einem Zeitpunkt von etwa 550 Ma, ist im Einklang mit Krustenrecycling zu selbigem Zeitpunkt.
Die neugewonnenen Daten dieser Arbeit unterstützten das „pulsed growth“ Modell.
Literatur
Bellon, H., Bordet, P. and Montenat, C., 1983. Chronology of the Neogene Magmatism from Betic Ranges (Southern Spain). Bulletin De La Societe Geologique De France, 25(2): 205-217.
Bianchini, G., Beccaluva, L., Nowell, G.M., Pearson, D.G. and Siena, F., 2011. Mantle xenoliths from Tallante (Betic Cordillera): Insights into the multi-stage evolution of the south Iberian lithosphere. Lithos, 124(3-4): 308-318.
Davies, G.R., Spriggs, A.J. and Nixon, P.H., 2001. A non-cognate origin for the Gibeon kimberlite megacryst suite, Namibia: Implications for the origin of Namibian kimberlites. Journal of Petrology, 42(1): 159-172.
Franz, L., Brey, G.P. and Okrusch, M., 1996b. Steady state geotherm, thermal disturbances, and tectonic development of the lower lithosphere underneath the Gibeon Kimberlite Province, Namibia. Contributions to Mineralogy and Petrology, 126(1-2): 181-198.
Hoal, B.G., Hoal, K.E.O., Boyd, F.R. and Pearson, D.G., 1995. Age constraints on crustal and mantle lithosphere beneath the Gibeon kimberlite field, Namibia. South African Journal of Geology, 98(2): 112-118.
Pearson, D.G., Irvine, G.J., Ionov, D.A., Boyd, F.R. and Dreibus, G.E., 2004. Re-Os isotope systematics and platinum group element fractionation during mantle melt extraction: a study of massif and xenolith peridotite suites. Chemical Geology, 208(1-4): 29-59.
Pearson, D.G., Parman, S.W. and Nowell, G.M., 2007. A link between large mantle melting events and continent growth seen in osmium isotopes. Nature, 449(7159): 202-205.
Die Wechselwirkung zwischen zwei verschiedenartigen Wellenphänomenen in einer Höhe von ca. 10 bis 100 km, der mittleren Atmosphäre, ist das zentrale Thema der vorliegenden Arbeit. Schwerewellen entstehen durch Oszillationen der Luft in einer stabil geschichteten Atmosphäre. Durch die Vielzahl von Schwerewellen-Paketen, die in der Troposphäre durch Gebirge, Gewitter, Fronten und andere dynamische Prozesse angeregt werden, wird Energie und Impuls in die mittleren Atmosphäre transportiert. Durch den turbulenten Zerfall von brechenden Schwerewellen wird auf die mittlere Strömung eine Kraft ausgeübt, welche im Bereich der Mesopause bei ca. 90 km maximal wird. Daraus resultiert die sogenannte interhemispherische residuelle Zirkulation, die in der Mesosphäre den Sommer- mit dem Winterpol verbindet und die beeindruckend kalte Sommer-Mesopause mit Temperaturen von unter −140°C verursacht. Thermische Gezeiten sind ein weiterer wichtiger Teil in der Dynamik der mittleren Atmosphäre. Sie werden durch die Erwärmung der Tagseite der Erde angeregt und sind globale Schwingungen mit Perioden von 24 Stunden und harmonischen Vielfachen. Mit Wind- und Temperatur-Amplituden von bis zu 50 m/s und 30 K dominieren sie die Tagesvariabilität im Mesopausen-Bereich.
In der Mesosphäre wird die Wechselwirkung zwischen Schwerewellen und thermischen Gezeiten wichtig. Dort wird durch die Gezeitenwinde das Brechen von Schwerewellen zeitlich moduliert und eine periodische Kraft erzeugt, welche auf die Gezeiten rückwirkt. Doch selbst unter Zuhilfenahme modernster Hochleistungsrechner kann in komplexen Zirkulationsmodellen nur ein Bruchteil des turbulenten sowie des Wellen-Spektrums aufgelöst werden. Der Effekt der nichtaufgelösten Skalen, wie Turbulenz und Schwerewellen, muss somit in effizienter Weise parametrisiert werden. Üblicherweise wird in Schwerewellen-Parametrisierungen die horizontale und zeitliche Variation des Hintergrundmediums vernachlässigt. Es entsteht eine vertikale Säule, in der sich stationäre Schwerewellen-Züge instantan nach oben ausbreiten. Es ist jedoch äußerst fraglich, inwieweit eine solche Beschreibung, auf der ein Großteil früherer Untersuchungen basiert, für das Ergründen der Schwerewellen-Gezeiten-Wechselwirkung hinreicht. Für diese Arbeit wurde deswegen das Ziel gesetzt, die Defizite der konventionellen Beschreibung der Schwerewellen-Ausbreitung in realistischen Gezeiten zu quantifizieren.
Die "Ray Tracing"-Methode wird auf die Problemstellung der Schwerewellen-Gezeiten-Wechselwirkung angewendet. In der "Ray Tracing"-Methode werden Schwerewellen-Pakete entlang ihrer Ausbreitungspfade explizit verfolgt und Veränderungen der Schwerewellen-Eigenschaften durch den Einfluss der Hintergrundströmung berücksichtigt. Vom Autor wurde das globale "Ray Tracing"-Modell RAPAGI (RAy PArameterization of Gravity-wave Impacts) entwickelt und mit realistischen Gezeitenfeldern aus dem Zirkulationsmodell HAMMONIA (HAmburg MOdel of the Neutral and Ionized Atmosphere) betrieben. In verschiedenen "Ray Tracing"-Experimenten wird für ein einfaches Schwerewellen-Ensemble gezeigt, wie horizontale Gradienten des Hintergrundmediums sowie dessen Zeitabhängigkeit wesentlichen Einfluss auf die Ausbreitung und Dissipation von Schwerewellen nehmen. Zum einen führt die durch Gezeitenwellen hervorgerufene Transienz zu einer tageszeitlichen Modulation der absoluten Schwerewellen-Frequenz.
Die dadurch induzierten Variationen der horizontalen Phasengeschwindigkeit der Schwerewellen können die anfängliche Phasengeschwindigkeit um bis zu eine Größenordnung übertreffen und folgen dem Verlauf des Hintergrundwindes. Die kritische Filterung von Schwerewellen wird durch diese Modulation abgeschwächt, was im Vergleich zu konventionellen Schwerewellen-Parametrisierungen zu einer im Mittel um 30 % geringeren Kraftwirkung auf die Gezeiten führt. Zum anderen werden durch horizontale Gradienten in der gesamten Hintergrundströmung Schwerewellen-Pakete horizontal abgelenkt. Wellen, die gegen die Hintergrundströmung laufen, werden in der Stratosphäre in die Maxima der Wind-Jets hineingeführt. Durch dieses Verhalten wird analog zum Fermatschen Prinzip der geometrischen Optik die Laufzeit der Schwerewellen in der mittleren Atmosphäre minimiert. Es entsteht eine Fokussierung von Schwerewellen-Feldern, bei gleichzeitiger Zunahme der horizontalen Wellenzahl in den Experimenten im Mittel um ca. 10 %. Dadurch reduziert sich der Schwerewellen-Impulsfluss und die mittlere und ebenfalls die periodische Kraft auf die Hintergrundströmung im Mittel um weitere 20 % bis 30 %. Konventionelle Schwerewellen-Parametrisierungen scheinen somit die Kraftwirkung von brechenden Schwerewellen zu uberschätzen. Aus den Ergebnissen der Arbeit wird klar, dass Schwerewellen-Parametrisierungen nicht "blind" für jede Untersuchung genutzt werden können. Alle Annahmen und Näherungen in Parametrisierungen müssen je nach Zielstellung neu getestet werden.
There is increasing evidence that climate change will have a severe impact on species’ distributions by altering the climatic conditions within their present ranges. Especially species inhabiting stream ecosystems are expected to be strongly affected due to warming temperatures and changes in precipitation patterns. The aim of this thesis was to
investigate how distributions of aquatic insects, i.e., benthic stream macroinvertebrates would be impacted by warming climates. The methods comprised of an ensemble forecasting technique based on species distribution models (SDMs) and climate change scenarios of the Intergovernmental Panel on Climate Change of the year 2080. Future model projections were generated for a wide variety of species from a number of taxonomic orders for two spatial scales: a stream network within the lower mountain ranges of Germany, and the entire territory across Europe. In addition, the effect of the modelling technique on habitat suitability projections was investigated by modifying the choice of study area (continuous area vs. stream network) and the choice of predictors (standard vs. corrected set).
Projections of future habitat suitability showed that potential climate-change impacts would be dependent on species’ thermal preferences, and with a similar pattern for both spatial scales. Future habitat suitability was projected to remain for most or all of the modelled species, and species were projected to track their climatically suitable conditions by shifting uphill along the river continuum within the lower mountain ranges, and into a north-easterly direction across Europe. Cold-adapted headwater and high-latitude species were projected to lose suitable habitats, whereas gains would be expected for warm-adapted river and low-latitude species along the river continuum and across Europe, respectively. Additionally, habitat specialist species in terms of endemics of the Iberian Peninsula were identified as potential climate-change losers, highlighting their restricted habitat availability and therefore vulnerability to warming climates.
The main findings of this thesis underline the high susceptibility of stream macroinvertebrates to ongoing climate change, and give insights into patterns of possible consequences due to changes in species’ habitat suitability. Concerning the methodology, a clear recommendation can be given for future modelling approaches of stream macroinvertebrates by building models within a stream network and with a careful choice of environmental predictors, to reduce uncertainties and thus to improve model projections.