Zur Kenntnis der Azophenole und Amidophenole der Diphenylreihe /

Thesis (doctoral)--Friedrich-Wilhelms-Universität Berlin, 1900.

Beiträge zur Kenntnis der Pyrazolreihe /

Thesis (doctoral)--Universität Jena, 1898.

Beiträge zur Kenntniss des Acetessiganilids /

Thesis (doctoral)--Universität Jena, 1893.

Die Begriffsbestimmung : vornehmlich in ihrer Beziehung zur Pädogogik /

Originally presented as the author's thesis (doctoral)--Universität Jena, 1893.

Surface velocity fields, digital elevation models, ice front positions and grounding line derived from remote sensing data at Dinsmoor-Bombardier-Edgeworth glacier system, Antarctic Peninsula (1992-2014)

The northern Antarctic Peninsula is one of the fastest changing regions on Earth. The disintegration of the Larsen-A Ice Shelf in 1995 caused tributary glaciers to adjust by speeding up, surface lowering, and overall increased ice-mass discharge. In this study, we investigate the temporal variation of these changes at the Dinsmoor-Bombardier-Edgeworth glacier system by analyzing dense time series from various spaceborne and airborne Earth observation missions. Precollapse ice shelf conditions and subsequent adjustments through 2014 were covered. Our results show a response of the glacier system some months after the breakup, reaching maximum surface velocities at the glacier front of up to 8.8 m/d in 1999 and a subsequent decrease to ~1.5 m/d in 2014. Using a dense time series of interferometrically derived TanDEM-X digital elevation models and photogrammetric data, an exponential function was fitted for the decrease in surface elevation. Elevation changes in areas below 1000 m a.s.l. amounted to at least 130±15 m130±15 m between 1995 and 2014, with change rates of ~3.15 m/a between 2003 and 2008. Current change rates (2010-2014) are in the range of 1.7 m/a. Mass imbalances were computed with different scenarios of boundary conditions. The most plausible results amount to -40.7±3.9 Gt-40.7±3.9 Gt. The contribution to sea level rise was estimated to be 18.8±1.8 Gt18.8±1.8 Gt, corresponding to a 0.052±0.005 mm0.052±0.005 mm sea level equivalent, for the period 1995-2014. Our analysis and scenario considerations revealed that major uncertainties still exist due to insufficiently accurate ice-thickness information. The second largest uncertainty in the computations was the glacier surface mass balance, which is still poorly known. Our time series analysis facilitates an improved comparison with GRACE data and as input to modeling of glacio-isostatic uplift in this region. The study contributed to a better understanding of how glacier systems adjust to ice shelf disintegration.

Ice furrow mapping in the Laptev Sea

During the "Polarstern"-expeditions ARK-IX/4 (1993) and ARK-XI/1 (1995), organised by the Alfred Wegener Institute (AWI), acoustic subbottom profiles (Parasound) have been collected in the Laptev Sea Shelf, Siberia. These data have been interpreted as an indicator of ice scours frequency and off-shore permafrost patterns. An additional acoustic profile data-base was available by the results of the expedition of the Federal Institute for Geosciences and Natural Resources (BGR) of the year 1994. The area of the expedition was located closer to the shelf, therefore supports a better understanding of ice scours frequency in shallower marine environments. The data-file consists of a 2930 km Parasound-traverse and has been subdivided into 586 working profiles. They are characterised by their location, number of ice scours, interpreted patterns of reflection and their extension and morphology. The data have been evaluated statistically and graphically and were presented in a map. Different patterns of sea floor reflection were established by different environments, outer influences (e.g. size of the icebergs, direction of the drift of icebergs) and the climatic history of the region. In the north-westerly region of the Laptev Sea at the continental slope of Severnaya Zemlya the sea floor in shallower depths has been ploughed intensely by recent icebergs. In some regions (40-60m), as an effect of intensely ploughing, the sea floor is hardly defined in acoustic profiles come along with relocation of marine deposits. Glacial diamiet deposits prevented the development of deep scours. Up to 355m deeper scours result from lower sea levels. The marginal north-easterly region of the Laptev Sea is characterised exclusively by this type of scour. Morphology and depth of these scours can be compared with those of the westerly Vilkitsky-Street so that similar conditions of development may be expected. Both, the north-easterly Laptev Sea and the Vilkitsky-Street, are not dominated by patterns ofrecent icebergs. In contrary the shelf-regions north-easterly ofthe Taimyr peninsula and north-westerly of the New Siberian Islands have been modified evidently by recent icebergs, which drifted with prevalent currents anticlockwise along the shelf edge of the Laptev Sea and cause the deepest scours of the whole region. The off-shore permafrost at the inner shelf regions has an important influence on the scours intensity. The permafrost layer can be recognised by the maximum depth of ice scours. It is represented by a Parasound reflector that can be made up for distances. The age of the ice scours cannot be determined absolutely by Parasound data but a relative order can be estimated whenever two scours are situated close to each other. When the Parasound-traverse ofthe expedition ARK-IX/4 (1993) (77°24'N 133°30'E-77°30'N 133°40'E) was repeated partially in expedition ARK-XI/l (1995) the ice scours of 1993 remained unchanged and uneroded and no new ice scours had been detected. It can be concluded that scours persist for a long time in the Laptev Sea, though after all with an average of 3 ice scours per kilometer there are not many at all in the Laptev Sea.

King George Island TanDEM-X DEM, link to GeoTIFF

We have generated a new digital elevation model for entire King George Island, Antarctica, using summer TanDEM-X bistatic SAR satellite data. The data was processed using differential SAR interferometry with an older DEM as reference. 4 TanDEM-X scenes from January 2012 were used as input. The new DEM was referenced to and validated against DGPS measurements. Height values are given in reference to ellipsoid (WGS84).

The Enlightening Supernatural: Ghost Stories in the Late Eighteenth-Century Germany

This dissertation explores the place of ghosts in late eighteenth-century German texts, where they appear with surprising frequency despite widespread disbelief in their ontological reality. These ghosts could simply be lingering remnants of superstition in an age where they no longer belong, but my project argues that they play a central role in the Enlightenment and its ideal of progress. The key texts analyzed in this context include three versions of the story of the Weiße Frau, as well as works by Immanuel Kant, Karl Philipp Moritz, Friedrich Schiller, and Johann Wolfgang von Goethe. In various ways, these texts demonstrate how the presentation of a ghost creates new possibilities in philosophy and aesthetics, as well as opportunities for critique. For some, the ghostly encounter produces an “Enlightening” suspense, disrupting the normal conditions of one’s understanding and creating a demand for resolution that propels one towards the future. Some recognized a dangerous manipulative potential in such suspense, and they used ghost stories to critique Enlightenment thought or imagine alternative aesthetic models. In all of these works, the ghost does not function simply as a relic of the past that needs to be left behind; it features prominently as a means of considering the present and imagining the future.

The relationship between the Enlightenment and superstitious beliefs has either been oversimplified as a basic opposition, or complicated by the recognition that the commitment to reason works as a new form of superstition. Prior scholarship has recognized the German ghost story as a primarily nineteenth-century phenomenon. This dissertation uncovers the roots of the German ghost story in unlikely texts from the eighteenth century and suggests that the relationship between ghostly apparitions and the Enlightenment was more complementary than oppositional. Ghosts do not only represent the persistence of the past, they also disrupt the normal conditions of the present in a way that enables progress towards new possibilities in aesthetics and thought.

Turandot in Schiller’s and Brecht’s Dramas

This paper aims to study the subject of Turandot in Friedrich Schiller’s Turandot, Prinzessin von China and Brecht’s Turandot oder Der Kongress der Weißwäscher. We will analyse both theatre adaptations, which have clearly influenced numerous authors through history, by addressing its intertextuality and originality.

Na 50 Nachlass Arthur Schopenhauer - 'Schopenhauer-Archiv', 582 - Promotionsurkunde und Urkunde zur Lehrerlaubnis an der Berliner Universität

u.a.: Ferdinand I.; August Boeckh; Friedrich Wilhelm III.; Johann Friedrich Ludwig Goeschen; Doktordiplom;