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Spurensuche Am Neuen Palais
(2016)
Sechs kurze Krimis über abgründige Verbrechen, unverwechselbare Tatorte (Potsdam-Sanssouci u. a.) und höchst eigenwillige Ermittler/innen, die ein hohes Risiko eingehen, um die rätselhaften Fälle zu lösen und schließlich für Klarheit und Aufklärung zu sorgen.
Unterhaltsam und spannend erzählt von Stefanie Börnicke & Friederike Weimar, Paula-Sophie Brink, Steven Dewart, Martin Thormann, Simone Weilandt. Mit einem Nachwort von Brunhilde Wehinger.
We elaborate a boundary Fourier method for studying an analogue of the Hilbert problem for analytic functions within the framework of generalised Cauchy-Riemann equations. The boundary value problem need not satisfy the Shapiro-Lopatinskij condition and so it fails to be Fredholm in Sobolev spaces. We show a solvability condition of the Hilbert problem, which looks like those for ill-posed
problems, and construct an explicit formula for approximate solutions.
Reconstructing climate from the Dead Sea sediment record using high-resolution micro-facies analyses
(2015)
The sedimentary record of the Dead Sea is a key archive for reconstructing climate in the eastern Mediterranean region, as it stores the environmental and tectonic history of the Levant for the entire Quaternary. Moreover, the lake is located at the boundary between Mediterranean sub-humid to semi-arid and Saharo-Arabian hyper-arid climates, so that even small shifts in atmospheric circulation are sensitively recorded in the sediments. This DFG-funded doctoral project was carried out within the ICDP Dead Sea Deep Drilling Project (DSDDP) that intended to gain the first long, continuous and high-resolution sediment core from the deep Dead Sea basin. The drilling campaign was performed in winter 2010-11 and more than 700 m of sediments were recovered. The main aim of this thesis was (1) to establish the lithostratigraphic framework for the ~455 m long sediment core from the deep Dead Sea basin and (2) to apply high-resolution micro-facies analyses for reconstructing and better understanding climate variability from the Dead Sea sediments.
Addressing the first aim, the sedimentary facies of the ~455 m long deep-basin core 5017-1 were described in great detail and characterised through continuous overview-XRF element scanning and magnetic susceptibility measurements. Three facies groups were classified: (1) the marl facies group, (2) the halite facies group and (3) a group involving different expressions of massive, graded and slumped deposits including coarse clastic detritus. Core 5017-1 encompasses a succession of four main lithological units. Based on first radiocarbon and U-Th ages and correlation of these units to on-shore stratigraphic sections, the record comprises the last ca 220 ka, i.e. the upper part of the Amora Formation (parts of or entire penultimate interglacial and glacial), the last interglacial Samra Fm. (~135-75 ka), the last glacial Lisan Fm. (~75-14 ka) and the Holocene Ze’elim Formation. A major advancement of this record is that, for the first time, also transitional intervals were recovered that are missing in the exposed formations and that can now be studied in great detail.
Micro-facies analyses involve a combination of high-resolution microscopic thin section analysis and µXRF element scanning supported by magnetic susceptibility measurements. This approach allows identifying and characterising micro-facies types, detecting event layers and reconstructing past climate variability with up to seasonal resolution, given that the analysed sediments are annually laminated. Within this thesis, micro-facies analyses, supported by further sedimentological and geochemical analyses (grain size, X-ray diffraction, total organic carbon and calcium carbonate contents) and palynology, were applied for two time intervals:
(1) The early last glacial period ~117-75 ka was investigated focusing on millennial-scale hydroclimatic variations and lake level changes recorded in the sediments. Thereby, distinguishing six different micro-facies types with distinct geochemical and sedimentological characteristics allowed estimating relative lake level and water balance changes of the lake. Comparison of the results to other records in the Mediterranean region suggests a close link of the hydroclimate in the Levant to North Atlantic and Mediterranean climates during the time of the build-up of Northern hemisphere ice sheets during the early last glacial period.
(2) A mostly annually laminated late Holocene section (~3700-1700 cal yr BP) was analysed in unprecedented detail through a multi-proxy, inter-site correlation approach of a shallow-water core (DSEn) and its deep-basin counterpart (5017-1). Within this study, a ca 1500 years comprising time series of erosion and dust deposition events was established and anchored to the absolute time-scale through 14C dating and age modelling. A particular focus of this study was the characterisation of two dry periods, from ~3500 to 3300 and from ~3000 to 2400 cal yr BP, respectively. Thereby, a major outcome was the coincidence of the latter dry period with a period of moist and cold climate in Europe related to a Grand Solar Minimum around 2800 cal yr BP and an increase in flood events despite overall dry conditions in the Dead Sea region during that time. These contrasting climate signatures in Europe and at the Dead Sea were likely linked through complex teleconnections of atmospheric circulation, causing a change in synoptic weather patterns in the eastern Mediterranean.
In summary, within this doctorate the lithostratigraphic framework of a unique long sediment core from the deep Dead Sea basin is established, which serves as a base for any further high-resolution investigations on this core. It is demonstrated in two case studies that micro-facies analyses are an invaluable tool to understand the depositional processes in the Dead Sea and to decipher past climate variability in the Levant on millennial to seasonal time-scales. Hence, this work adds important knowledge helping to establish the deep Dead Sea record as a key climate archive of supra-regional significance.
Während des Ersten Weltkrieges kam der deutsche Dramatiker und Erzähler Alfred Brust mit dem chassidischen Judentum im litauischen Kowno und Wilna in Berührung. So wie Sammy Gronemann, Arnold Zweig und andere Autoren, die in der Zensur- Abteilung von ‚Ober Ost‘ beschäftigt waren, war Brust tief beeindruckt von dessen archaischer Kultur. Diese schien ihm im Gegensatz zur Dekadenz der modernen Welt zu stehen. Beeinflusst vom expressionistischen Topos einer inneren Wandlung des Menschen entwickelte er in den folgenden Jahren die Idee einer Translation spiritueller und moralischer Werte von den osteuropäischen Juden auf die (deutschen) Ostpreußen. Für ihn galt: Die „Juden sind der Adel der Bewegung“. Brust stand in Kontakt mit Richard Dehmel, Hugo von Hofmannsthal, Florens Christian Rang und Martin Buber, selbst Walter Benjamin war zeitweise an ihm interessiert.
Hintergrund: In Deutschland stellt der akute Myokardinfarkt (MI) eine der häufigsten Todesursachen dar. Als Ursache für regionale Unterschiede bei den Mortalitätsraten werden divergente Versorgungsstrukturen vermutet. Ziel der Untersuchung war, diese Fragestellung anhand anonymisierter krankenkassenbasierter Abrechnungsdaten zu evaluieren.
Methodik: Standardisierte Hospitalisierungs- sowie Krankenhaus- und Ein-Jahres-Mortalitätsraten nach MI wurden anhand anonymisierter Versichertendaten einer gesetzlichen Krankenkasse für das Jahr 2012 und die Bundesländer Berlin, Brandenburg und Mecklenburg-Vorpommern ermittelt (n=1.387.084, 46.3% male, 60.9 ± 18,2 years). Weiterhin wurden prädiktive Einflussfaktoren auf die Ein-Jahres-Mortalität, auf die Durchführung invasiver Prozeduren und auf eine leitliniengerechte pharmakotherapeutische Sekundärprävention analysiert.
Ergebnisse: 6.733 Patienten (73,7 ±13,0 Jahre, 56,7% männlich) wurden identifiziert. Obwohl für das Bundesland Berlin eine höhere Hospitalisierungsrate als in Mecklenburg-Vorpommern ermittelt werden konnte, ließen sich bei der Krankenhaus- und 1-Jahres-Mortalität keine signifikant abweichenden Raten zwischen den Bundesländern beobachten. Die Durchführung einer Koronarangiographie (OR: 0,42 [0,35-0,51]) und eine leitliniengerechte Pharmakotherapie (OR: 0,14 [0,12-0,17] waren mit einer geringeren 1-Jahres-Mortalität assoziiert. Die Durchführung einer Koronarangiographie und eine leitliniengerechte Pharmakotherapie von Patienten nach Myokardinfarkt wurde hingegen primär durch Alter und Geschlecht, nicht aber durch das Bundesland determiniert.
Folgerung: Eine regional divergierende stationäre und postinfarzielle Versorgung auf Bundesland-Ebene kann anhand der vorliegenden Daten nicht nachgewiesen werden.
Die vorliegende Dissertation analysiert die Mentalitäten der bürgerlichen Bewohner Bogotas 19. Jahrhundert. Einblicke in die Fremd- und Eigenperspektiven der Bogotaner werden durch die Analyse von Reiseliteratur gewonnen. Methodologisch stützt sich die Arbeit auf den Vergleich zwischen europäischen Reiseberichten aus dem 19. Jh., Chroniken aus dem 16. Jh. sowie zwei kolumbianische Romane aus dem frühen 20.. Jh. Die Texte werden historiographisch behandelt; obwohl sie unterschiedlichen literarischen Genres angehören, weisen sie einen gemeinsamen autobiographischen Charakter auf. Aus den Erfahrungen und Gedanken der Reisenden werden v.a. die Auswirkungen der geographischen und sozialen Isolation thematisiert, sowie die Einflüsse von politischen und religiösen Diskursen auf die Bildung von bürgerlichem Gedankengut.
The non-linear behaviour of the atmospheric dynamics is not well understood and makes the evaluation and usage of regional climate models (RCMs) difficult. Due to these non-linearities, chaos and internal variability (IV) within the RCMs are induced, leading to a sensitivity of RCMs to their initial conditions (IC). The IV is the ability of RCMs to realise different solutions of simulations that differ in their IC, but have the same lower and lateral boundary conditions (LBC), hence can be defined as the across-member spread between the ensemble members.
For the investigation of the IV and the dynamical and diabatic contributions generating the IV four ensembles of RCM simulations are performed with the atmospheric regional model HIRHAM5. The integration area is the Arctic and each ensemble consists of 20 members. The ensembles cover the time period from July to September for the years 2006, 2007, 2009 and 2012. The ensemble members have the same LBC and differ in their IC only. The different IC are arranged by an initialisation time that shifts successively by six hours. Within each ensemble the first simulation starts on 1st July at 00 UTC and the last simulation starts on 5th July at 18 UTC and each simulation runs until 30th September. The analysed time period ranges from 6th July to 30th September, the time period that is covered by all ensemble members. The model runs without any nudging to allow a free development of each simulation to get the full internal variability within the HIRHAM5.
As a measure of the model generated IV, the across-member standard deviation and the across-member variance is used and the dynamical and diabatic processes influencing the IV are estimated by applying a diagnostic budget study for the IV tendency of the potential temperature developed by Nikiema and Laprise [2010] and Nikiema and Laprise [2011]. The diagnostic budget study is based on the first law of thermodynamics for potential temperature and the mass-continuity equation. The resulting budget equation reveals seven contributions to the potential temperature IV tendency.
As a first study, this work analyses the IV within the HIRHAM5. Therefore, atmospheric circulation parameters and the potential temperature for all four ensemble years are investigated. Similar to previous studies, the IV fluctuates strongly in time. Further, due to the fact that all ensemble members are forced with the same LBC, the IV depends on the vertical level within the troposphere, with high values in the lower troposphere and at 500 hPa and low values in the upper troposphere and at the surface. By the same reason, the spatial distribution shows low values of IV at the boundaries of the model domain.
The diagnostic budget study for the IV tendency of potential temperature reveals that the seven contributions fluctuate in time like the IV. However, the individual terms reach different absolute magnitudes. The budget study identifies the horizontal and vertical ‘baroclinic’ terms as the main contributors to the IV tendency, with the horizontal ‘baroclinic’ term producing and the vertical ‘baroclinic’ term reducing the IV. The other terms fluctuate around zero, because they are small in general or are balanced due to the domain average.
The comparison of the results obtained for the four different ensembles (summers 2006, 2007, 2009 and 2012) reveals that on average the findings for each ensemble are quite similar concerning the magnitude and the general pattern of IV and its contributions. However, near the surface a weaker IV is produced with decreasing sea ice extent. This is caused by a smaller impact of the horizontal 'baroclinic' term over some regions and by the changing diabatic processes, particularly a more intense reducing tendency of the IV due to condensative heating. However, it has to be emphasised that the behaviour of the IV and its dynamical and diabatic contributions are influenced mainly by complex atmospheric feedbacks and large-scale processes and not by the sea ice distribution.
Additionally, a comparison with a second RCM covering the Arctic and using the same LBCs and IC is performed. For both models very similar results concerning the IV and its dynamical and diabatic contributions are found. Hence, this investigation leads to the conclusion that the IV is a natural phenomenon and is independent from the applied RCM.
Der andere Weg zur Wahrheit
(2015)
Vorliegender Aufsatz befasst sich mit der Auseinandersetzung des Philosophen Franz Rosenzweig mit der Jesus-Figur. Dabei werden zwei Texte Rosenzweigs in den Blick genommen: „Atheistische Theologie“ (1914) und „Der Stern der Erlösung“ (1921). Hinzu kommen der Briefwechsel, den er mit Margrit und Eugen Rosenstock zwischen 1917 und 1929 führt und ein Text von Eduard Strauß, den letzterer im Rahmen seiner Tätigkeit im Frankfurter Jüdischen Lehrhaus entworfen hat. Durch diese Texte wird gezeigt, wie die Analyse der Jesus-Figur zur Auseinandersetzung mit seiner Historisierung durch die protestantische Theologie wird. Neben Rosenzweig, Buber und Strauß tragen weitere jüdische Gelehrte zu dieser Debatte bei. Diese Debatten um die Geschichtlichkeit Jesu werden auch in den Kontext des Verhältnisses zwischen Christentum und Judentum und ferner in Rosenzweigs Bemühungen um einen christlichjüdischen Dialog eingebettet.
We continue our study of invariant forms of the classical equations of mathematical physics,
such as the Maxwell equations or the Lamé system, on manifold with boundary. To this end we interpret them in terms of the de Rham complex at a certain step. On using the structure of the complex we get an insight to predict a degeneracy deeply encoded
in the equations. In the present paper we develop an invariant approach to the classical Navier-Stokes equations.