TY - JOUR A1 - Zaupa, Alessandro A1 - Neffe, Axel T. A1 - Pierce, Benjamin F. A1 - Nöchel, Ulrich A1 - Lendlein, Andreas T1 - Influence of tyrosine-derived moieties and drying conditions on the formation of helices in gelatin JF - Biomacromolecules : an interdisciplinary journal focused at the interface of polymer science and the biological sciences N2 - The single and triple helical organization of protein chains strongly influences the mechanical properties of gelatin-based materials. A chemical method for obtaining different degrees of helical organization in gelatin is covalent functionalization, while a physical method for achieving the same goal is the variation of the drying conditions of gelatin solutions. Here we explored how the introduction of desaminotyrosine (DAT) and desaminotyrosyl tyrosine (DATT) linked to lysine residues of gelatin influenced the kinetics and thermodynamic equilibrium of the helicalization process of single and triple helices following different drying conditions. Drying at a temperature above. the helix-to-coil transition temperature of gelatin (T > T-c, called nu(short)) generally resulted in gelatins with relatively lower triple helical content (X-c,X-t = 1-2%) than lower temperature drying (T < T-c, called nu(long)) (X-c,X-t = 8-10%), where the DAT(T) functional groups generally disrupted helix formation. While different helical contents affected the thermal transition temperatures only slightly, the mechanical properties were strongly affected for swollen hydrogels (E = 4-13 kPa for samples treated by nu(long) and E = 120-700 kPa for samples treated by nu(short)). This study shows that side group functionalization and different drying conditions are viable options to control the helicalization and macroscopic properties of gelatin-based materials. Y1 - 2011 U6 - https://doi.org/10.1021/bm101029k SN - 1525-7797 VL - 12 IS - 1 SP - 75 EP - 81 PB - American Chemical Society CY - Washington ER - TY - JOUR A1 - Zaupa, Alessandro A1 - Neffe, Axel T. A1 - Pierce, Benjamin F. A1 - Lendlein, Andreas A1 - Hofmann, Dieter T1 - A molecular dynamic analysis of gelatin as an amorphous material Prediction of mechanical properties of gelatin systems JF - The international journal of artificial organs N2 - Biomaterials are used in regenerative medicine for induced autoregeneration and tissue engineering. This is often challenging, however, due to difficulties in tailoring and controlling the respective material properties. Since functionalization is expected to offer better control, in this study gelatin chains were modified with physically interacting groups based on tyrosine with the aim of causing the formation of physical crosslinks. This method permits application-specific properties like swelling and better tailoring of mechanical properties. The design of the crosslink strategy was supported by molecular dynamic (MD) simulations of amorphous bulk models for gelatin and functionalized gelatins at different water contents (0.8 and 25 wt.-%). The results permitted predictions to be formulated about the expected crosslink density and its influence on equilibrium swelling behavior and on elastic material properties. The models of pure gelatin were used to validate the strategy by comparison between simulated and experimental data such as density, backbone conformation angle distribution, and X-ray scattering spectra. A key result of the simulations was the prediction that increasing the number of aromatic functions attached to the gelatin chain leads to an increase in the number of physical netpoints observed in the simulated bulk packing models. By comparison with the Flory-Rehner model, this suggested reduced equilibrium swelling of the functionalized materials in water, a prediction that was subsequently confirmed by our experimental work. The reduction and control of the equilibrium degree of swelling in water is a key criterion for the applicability of functionalized gelatins when used, for example, as matrices for induced autoregeneration of tissues. KW - Physical Network KW - Biopolymer material KW - Molecular modeling KW - Gelatin Y1 - 2011 U6 - https://doi.org/10.5301/IJAO.2010.6083 SN - 0391-3988 VL - 34 IS - 2 SP - 139 EP - 151 PB - Wichtig CY - Milano ER - TY - JOUR A1 - Zakrevskyy, Yuriy A1 - Kopyshev, Alexey A1 - Lomadze, Nino A1 - Morozova, Elena A1 - Lysyakova, Liudmila A1 - Kasyanenko, Nina A1 - Santer, Svetlana T1 - DNA compaction by azobenzene-containing surfactant JF - Physical review : E, Statistical, nonlinear and soft matter physics N2 - We report on the interaction of cationic azobenzene-containing surfactant with DNA investigated by absorption and fluorescence spectroscopy, dynamic light scattering, and atomic force microscopy. The properties of the surfactant can be controlled with light by reversible switching of the azobenzene unit, incorporated into the surfactant tail, between a hydrophobic trans (visible irradiation) and a hydrophilic cis (UV irradiation) configuration. The influence of the trans-cis isomerization of the azobenzene on the compaction process of DNA molecules and the role of both isomers in the formation and colloidal stability of DNA-surfactant complexes is discussed. It is shown that the trans isomer plays a major role in the DNA compaction process. The influence of the cis isomer on the DNA coil configuration is rather small. The construction of a phase diagram of the DNA concentration versus surfactant/DNA charge ratio allows distancing between three major phases: colloidally stable and unstable compacted globules, and extended coil conformation. There is a critical concentration of DNA above which the compacted globules can be hindered from aggregation and precipitation by adding an appropriate amount of the surfactant in the trans configuration. This is because of the compensation of hydrophobicity of the globules with an increasing amount of the surfactant. Below the critical DNA concentration, the compacted globules are colloidally stable and can be reversibly transferred with light to an extended coil state. Y1 - 2011 U6 - https://doi.org/10.1103/PhysRevE.84.021909 SN - 1539-3755 VL - 84 IS - 2 PB - American Physical Society CY - College Park ER - TY - JOUR A1 - Zakharova, Anna A1 - Kurths, Jürgen A1 - Vadivasova, Tatyana A1 - Koseska, Aneta T1 - Analysing dynamical behavior of cellular networks via stochastic bifurcations JF - PLoS one N2 - The dynamical structure of genetic networks determines the occurrence of various biological mechanisms, such as cellular differentiation. However, the question of how cellular diversity evolves in relation to the inherent stochasticity and intercellular communication remains still to be understood. Here, we define a concept of stochastic bifurcations suitable to investigate the dynamical structure of genetic networks, and show that under stochastic influence, the expression of given proteins of interest is defined via the probability distribution of the phase variable, representing one of the genes constituting the system. Moreover, we show that under changing stochastic conditions, the probabilities of expressing certain concentration values are different, leading to different functionality of the cells, and thus to differentiation of the cells in the various types. Y1 - 2011 U6 - https://doi.org/10.1371/journal.pone.0019696 SN - 1932-6203 VL - 6 IS - 5 PB - PLoS CY - San Fransisco ER - TY - JOUR A1 - Zacke, Birgit T1 - Rhythm of the images narrative strategies in text and image products of the eleventh and thirteenth century JF - Zeitschrift für Germanistik Y1 - 2011 SN - 0323-7982 VL - 21 IS - 1 SP - 175 EP - 176 PB - Lang CY - Bern ER - TY - THES A1 - Yustus, Ekaterina T1 - Verfassungsgerichtsbarkeit in Russland und Deutschland T2 - Europäische Hochschulschriften : Reihe 2, Rechtswissenschaften Y1 - 2011 SN - 978-3-631-60741-1 SN - 0531-7312 VL - 5205 PB - Lang CY - Frankfurt am Main ER - TY - JOUR A1 - Yuan, Jiayin A1 - ten Brummelhuis, Niels A1 - Junginger, Mathias A1 - Xie, Zailai A1 - Lu, Yan A1 - Taubert, Andreas A1 - Schlaad, Helmut T1 - Diversified applications of chemically modified 1,2-Polybutadiene JF - Macromolecular rapid communications N2 - Commercially available 1,2-PB was transformed into a well-defined reactive intermediate by quantitative bromination. The brominated polymer was used as a polyfunctional macroinitiator for the cationic ring-opening polymerization of 2-ethyl-2-oxazoline to yield a water-soluble brush polymer. Nucleophilic substitution of bromide by 1-methyl imidazole resulted in the formation of polyelectrolyte copolymers consisting of mixed units of imidazolium, bromo, and double bond. These copolymers, which were soluble in water without forming aggregates, were used as stabilizers in the heterophase polymerization of styrene and were also studied for their ionic conducting properties. KW - emulsion polymerization KW - polybutadiene KW - polyelectrolytes KW - polymer modification KW - ring-opening polymerization Y1 - 2011 U6 - https://doi.org/10.1002/marc.201100254 SN - 1022-1336 VL - 32 IS - 15 SP - 1157 EP - 1162 PB - Wiley-Blackwell CY - Malden ER - TY - JOUR A1 - Yin, Jian A1 - Linker, Torsten T1 - Stereoselective diversity-oriented syntheses of functionalized saccharides from bicyclic carbohydrate 1,2-lactones JF - Tetrahedron N2 - Bicyclic carbohydrate 1,2-lactones have been synthesized in only two steps and high yields by saponification and subsequent cyclization from known malonate addition products to glycals. The gluco-configured lactone serves as an important precursor for diversity-oriented syntheses. Thus, stereoselective opening of the lactone ring was realized with various nucleophiles in the presence of Sc(OTf)(3). This enabled the introduction of different substituents at the anomeric position, to afford a broad variety of 1-functionalized carbohydrates. On the other hand, stereoselective alpha-substitution of the gluco-configured lactone with different electrophiles and subsequent ring opening gives a collection of 2-functionalized saccharides. More than 30 products have been isolated in analytically pure form, and their configurations were unequivocally established by various NMR methods. Thus, carbohydrate 1,2-lactones are attractive precursors for the stereoselective synthesis of diverse saccharides. KW - Carbohydrates KW - Lactones KW - Glycosides KW - Molecular diversity KW - Synthetic methods Y1 - 2011 U6 - https://doi.org/10.1016/j.tet.2011.01.069 SN - 0040-4020 VL - 67 IS - 13 SP - 2447 EP - 2461 PB - Elsevier CY - Oxford ER - TY - JOUR A1 - Yildirim, Cengiz A1 - Schildgen, Taylor F. A1 - Echtler, Helmut Peter A1 - Melnick, Daniel A1 - Strecker, Manfred T1 - Late Neogene and active orogenic uplift in the Central Pontides associated with the North Anatolian Fault implications for the northern margin of the Central Anatolian Plateau, Turkey JF - Tectonics N2 - Surface uplift at the northern margin of the Central Anatolian Plateau (CAP) is integrally tied to the evolution of the Central Pontides (CP), between the North Anatolian Fault (NAF) and the Black Sea. Our regional morphometric and plate kinematic analyses reveal topographic anomalies, steep channel gradients, and local high relief areas as indicators of ongoing differential surface uplift, which is higher in the western CP compared to the eastern CP and fault-normal components of geodetic slip vectors and the character of tectonic activity of the NAF suggest that stress is accumulated in its broad restraining bend. Seismic reflection and structural field data show evidence for a deep structural detachment horizon responsible for the formation of an actively northward growing orogenic wedge with a positive flower-structure geometry across the CP and the NAF. Taken together, the tectonic, plate kinematic, and geomorphic observations imply that the NAF is the main driving mechanism for wedge tectonics and uplift in the CP. In addition, the NAF Zone defines the boundary between the extensional CAP and the contractional CP. The syntectonic deposits within inverted intermontane basins and deeply incised gorges suggest that the formation of relief, changes in sedimentary dynamics, and > 1 km fluvial incision resulted from accelerated uplift starting in the early Pliocene. The Central Pontides thus provide an example of an accretionary wedge with surface-breaking faults that play a critical role in mountain building processes, sedimentary basin development, and ensuing lateral growth of a continental plateau since the end of the Miocene. Y1 - 2011 U6 - https://doi.org/10.1029/2010TC002756 SN - 0278-7407 VL - 30 PB - American Geophysical Union CY - Washington ER - TY - JOUR A1 - Yeung, Ching-man Au A1 - Noll, Michael G. A1 - Gibbins, Nicholas A1 - Meinel, Christoph A1 - Shadbolt, Nigel T1 - Spear spamming-resistant expertise analysis and ranking incollaborative tagging systems JF - Computational intelligence N2 - In this article, we discuss the notions of experts and expertise in resource discovery in the context of collaborative tagging systems. We propose that the level of expertise of a user with respect to a particular topic is mainly determined by two factors. First, an expert should possess a high-quality collection of resources, while the quality of a Web resource in turn depends on the expertise of the users who have assigned tags to it, forming a mutual reinforcement relationship. Second, an expert should be one who tends to identify interesting or useful resources before other users discover them, thus bringing these resources to the attention of the community of users. We propose a graph-based algorithm, SPEAR (spamming-resistant expertise analysis and ranking), which implements the above ideas for ranking users in a folksonomy. Our experiments show that our assumptions on expertise in resource discovery, and SPEAR as an implementation of these ideas, allow us to promote experts and demote spammers at the same time, with performance significantly better than the original hypertext-induced topic search algorithm and simple statistical measures currently used in most collaborative tagging systems. KW - collaborative tagging KW - expertise KW - folksonomy KW - HITS KW - ranking KW - spamming Y1 - 2011 U6 - https://doi.org/10.1111/j.1467-8640.2011.00384.x SN - 0824-7935 SN - 1467-8640 VL - 27 IS - 3 SP - 458 EP - 488 PB - Wiley-Blackwell CY - Hoboken ER - TY - JOUR A1 - Yarman, Aysu A1 - Nagel, Thomas A1 - Gajovic-Eichelmann, Nenad A1 - Fischer, Anna A1 - Wollenberger, Ursula A1 - Scheller, Frieder W. T1 - Bioelectrocatalysis by Microperoxidase-11 in a Multilayer Architecture of Chitosan Embedded Gold Nanoparticles JF - Electroanalysis : an international journal devoted to fundamental and practical aspects of electroanalysis N2 - We report on the redox behaviour of the microperoxidase-11 (MP-11) which has been electrostatically immobilized in a matrix of chitosan-embedded gold nanoparticles on the surface of a glassy carbon electrode. MP-11 contains a covalently bound heme c as the redox active group that exchanges electrons with the electrode via the gold nanoparticles. Electroactive surface concentration of MP-11 at high scan rate is between 350+/-50 pmol cm(-2), which reflects a multilayer process. The formal potential (E degrees') of MP-11 in the gold nanoparticles-chitosan film was estimated to be -(267.7+/-2.9) mV at pH 7.0. The heterogeneous electron transfer rate constant (k(s)) starts at 1.21 s(-1) and levels off at 6.45 s(-1) in the scan rate range from 0.1 to 2.0 V s(-1). Oxidation and reduction of MP-11 by hydrogen peroxide and superoxide, respectively have been coupled to the direct electron transfer of MP-11. KW - Microperoxidase KW - Direct electron transfer KW - Nanoparticles KW - Hydrogen peroxide KW - Superoxide KW - Bioelectrocatalysis Y1 - 2011 U6 - https://doi.org/10.1002/elan.201000535 SN - 1040-0397 VL - 23 IS - 3 SP - 611 EP - 618 PB - Wiley-Blackwell CY - Malden ER - TY - JOUR A1 - Yarman, Aysu A1 - Badalyan, Artavazd A1 - Gajovic-Eichelmann, Nenad A1 - Wollenberger, Ursula A1 - Scheller, Frieder W. T1 - Enzyme electrode for aromatic compounds exploiting the catalytic activities of microperoxidase-11 JF - Biosensors and bioelectronics : the principal international journal devoted to research, design development and application of biosensors and bioelectronics N2 - Microperoxidase-11 (MR-11) which has been immobilised in a matrix of chitosan-embedded gold nanoparticles on the surface of a glassy carbon electrode catalyzes the conversion of aromatic substances. This peroxide-dependent catalysis of microperoxidase has been applied in an enzyme electrode for the first time to indicate aromatic compounds such as aniline. 4-fluoroaniline, catechol and p-aminophenol. The electrode signal is generated by the cathodic reduction of the quinone or quinoneimine which is formed in the presence of both MP-II and peroxide from the substrate. The same sensor principle will be extended to aromatic drugs. KW - Microperoxidase-11 KW - Nanoparticles KW - p-Aminophenol KW - Aniline KW - Catechol KW - 4-Fluoroaniline KW - Biosensors Y1 - 2011 U6 - https://doi.org/10.1016/j.bios.2011.09.004 SN - 0956-5663 VL - 30 IS - 1 SP - 320 EP - 323 PB - Elsevier CY - Oxford ER - TY - JOUR A1 - Xie, Zai-Lai A1 - White, Robin J. A1 - Weber, Jens A1 - Taubert, Andreas A1 - Titirici, Magdalena M. T1 - Hierarchical porous carbonaceous materials via ionothermal carbonization of carbohydrates JF - Journal of materials chemistry N2 - We report on the ionothermal synthesis of porous carbon materials from a variety of carbohydrate precursors (i.e. D-glucose, D-fructose, D-xylose, and starch) using 1-butyl-3-methylimidazolium tetrachloroferrate(III), [Bmim][FeCl(4)] as a reusable solvent and catalyst. The carbon materials derived from these different carbohydrates are similar in terms of particle size and chemical composition, possessing relatively high surface areas from 44 to 155 m(2) g(-1) after ionothermal processing, which can be significantly increased to > 350 m(2) g(-1) by further thermal treatment (e. g. post-carbonization at 750 degrees C). CO(2) and N(2) sorption analysis, combined with Hg intrusion porosimetry, reveals a promising hierarchical pore structuring to these carbon materials. The ionic liquid [Bmim][FeCl(4)] has a triple role: it acts as both a soft template to generate the characterized pore structuring, solvent and as a catalyst resulting in enhanced ionothermal carbon yields. Importantly from a process point of view, the ionic liquid can be successfully recovered and reused. The current work shows that ionothermal synthesis has the potential to be an effective, low cost, and green reusable synthetic route towards sustainable porous carbon materials. Y1 - 2011 U6 - https://doi.org/10.1039/c1jm00013f SN - 0959-9428 VL - 21 IS - 20 SP - 7434 EP - 7442 PB - Royal Society of Chemistry CY - Cambridge ER - TY - JOUR A1 - Xie, Zai-Lai A1 - Taubert, Andreas T1 - Thermomorphic behavior of the ionic liquids [C(4)mim][FeCl4] and [C(12)mim][FeCl4] JF - ChemPhysChem : a European journal of chemical physics and physical chemistry N2 - The iron-containing ionic liquids 1-butyl-3-methylimidazolium tetrachloroferrate(III) [C(4)mim][FeCl4] and 1-dodecyl-3-methylimidazolium tetrachloroferrate(III) [C(12)mim][FeCl4] exhibit a thermally induced demixing with water (thermomorphism). The phase separation temperature varies with IL weight fraction in water and can be tuned between 100 degrees C and room temperature. The reversible lower critical solution temperature (LCST) is only observed at IL weight fractions below ca. 35% in water. UV/Vis, IR, and Raman spectroscopy along with elemental analysis prove that the yellow-brown liquid phase recovered after phase separation is the starting IL [C(4)mim][FeCl4] and [C(12)mim][FeCl4], respectively. Photometry and ICP-OES show that about 40% of iron remains in the water phase upon phase separation. Although the process is thus not very efficient at the moment, the current approach is the first example of an LCST behavior of a metal-containing IL and therefore, although still inefficient, a prototype for catalyst removal or metal extraction. KW - imidazolium KW - ionic liquids KW - phase transitions KW - Raman spectroscopy KW - thermomorphism Y1 - 2011 U6 - https://doi.org/10.1002/cphc.201000808 SN - 1439-4235 VL - 12 IS - 2 SP - 364 EP - 368 PB - Wiley-VCH CY - Weinheim ER - TY - JOUR A1 - Wüstenhagen, Axel T1 - Die neue Struktur der UN-Informationsarbeit in Europa JF - Die Vereinten Nationen vor globalen Herausforderungen : Referate der Potsdamer UNO-Konferenzen 2000–2008 Y1 - 2011 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:kobv:517-opus-61169 SP - 311 EP - 318 PB - Universitätsverlag Potsdam CY - Potsdam ER - TY - THES A1 - Wyschkon, Anne T1 - Repräsentativität und Umfang von Normstrichproben für Leistungstests : Auswirkungen auf die Diagnostik von schwachen Leistungen und Umschriebenen Entwicklungsstörungen im Grundschulalter T2 - Psychologische Forschungsergebnisse Y1 - 2011 SN - 978-3-8300-5924-0 SN - 1435-666X VL - 162 PB - Kova? CY - Hamburg ER - TY - THES A1 - Wurster, Simone T1 - Born global standard establishers : Einfluss- und Erfolgsfaktoren für die internationale Standardsetzung und -erhaltung Y1 - 2011 SN - 978-3-8349-2975-4 U6 - https://doi.org/10.1007/978-3-8349-6795-4 PB - Gabler Verlag / Springer Fachmedien Wiesbaden GmbH Wiesbaden CY - Wiesbaden ER - TY - JOUR A1 - Wulf, Monika A1 - Rujner, Hendrik T1 - A GIS-based method for the reconstruction of the late eighteenth century forest vegetation in the Prignitz region (NE Germany) JF - Landscape ecology N2 - Our goal was to reconstruct the late eighteenth century forest vegetation of the Prignitz region (NE Germany) at a scale of 1:50,000. We also wanted to relate the historical forest vegetation to the actual and potential natural vegetation. For these purposes, we selected 15 woody species and transferred relevant data found in historical records from various sources together with the recent localities of (very) old individuals belonging to these woody species into ArcView GIS. Following multi-step data processing including the generation of a point density layer using a moving window with kernel estimation and derivation of vegetation units applying Boolean algebra rules together with information on site conditions, we derived 17 forest communities corresponding to the potential natural vegetation. We were able to reconstruct the historical forest vegetation for 90% of the forest area ca. 1780. Only two of the 17 forest communities covered large parts of the forested area. The oak forest with Agrostis capillaris covered about 44% of the total forest area, and alder forests on fenland made up about 37%. Oak-hornbeam forests with Stellaria holostea comprised slightly less than 6% of the forest area, while all other forest communities comprised less than 1%. The historical forest vegetation is more similar to the potential forest vegetation and quite different from the actual forest vegetation because coniferous tree species currently cover approximately two-thirds of the actual forest area. The most beneficial result of this study is the map of high-resolution historical vegetation units that may serve as the basis for various further studies, e.g., modelling long-term changes in biodiversity at the landscape scale. KW - Boolean algebra KW - Historical ecology KW - Kernel estimation KW - Moving window KW - Point density KW - Potential natural vegetation KW - Schmettau map KW - Toponymy KW - Vegetation map Y1 - 2011 U6 - https://doi.org/10.1007/s10980-010-9555-1 SN - 0921-2973 VL - 26 IS - 2 SP - 153 EP - 168 PB - Springer CY - Dordrecht ER - TY - THES A1 - Wulf, Hendrik T1 - Seasonal precipitation, river discharge, and sediment flux in the western Himalaya T1 - Saisonaler Niederschlag, Wasserabfluss und Sedimentationsfluss im westlichen Himalaya N2 - Rainfall, snow-, and glacial melt throughout the Himalaya control river discharge, which is vital for maintaining agriculture, drinking water and hydropower generation. However, the spatiotemporal contribution of these discharge components to Himalayan rivers is not well understood, mainly because of the scarcity of ground-based observations. Consequently, there is also little known about the triggers and sources of peak sediment flux events, which account for extensive hydropower reservoir filling and turbine abrasion. We therefore lack basic information on the distribution of water resources and controls of erosion processes. In this thesis, I employ various methods to assess and quantify general characteristics of and links between precipitation, river discharge, and sediment flux in the Sutlej Valley. First, I analyze daily precipitation data (1998-2007) from 80 weather stations in the western Himalaya, to decipher the distribution of rain- and snowfall. Rainfall magnitude frequency analyses indicate that 40% of the summer rainfall budget is attributed to monsoonal rainstorms, which show higher variability in the orogenic interior than in frontal regions. Combined analysis of rainstorms and sediment flux data of a major Sutlej River tributary indicate that monsoonal rainfall has a first order control on erosion processes in the orogenic interior, despite the dominance of snowfall in this region. Second, I examine the contribution of rainfall, snow and glacial melt to river discharge in the Sutlej Valley (s55,000 km2), based on a distributed hydrological model, which covers the period 2000-2008. To achieve high spatial and daily resolution despite limited ground-based observations the hydrological model is forced by daily remote sensing data, which I adjusted and calibrated with ground station data. The calibration shows that the Tropical Rainfall Measuring Mission (TRMM) 3B42 rainfall product systematically overestimates rainfall in semi-arid and arid regions, increasing with aridity. The model results indicate that snowmelt-derived discharge (74%) is most important during the pre-monsoon season (April to June) whereas rainfall (56%) and glacial melt (17%) dominate the monsoon season (July-September). Therefore, climate change most likely causes a reduction in river discharge during the pre-monsoon season, which especially affects the orogenic interior. Third, I investigate the controls on suspended sediment flux in different parts of the Sutlej catchments, based on daily gauging data from the past decade. In conjunction with meteorological data, earthquake records, and rock strength measurements I find that rainstorms are the most frequent trigger of high-discharge events with peaks in suspended sediment concentrations (SSC) that account for the bulk of the suspended sediment flux. The suspended sediment flux increases downstream, mainly due to increases in runoff. Pronounced erosion along the Himalayan Front occurs throughout the monsoon season, whereas efficient erosion of the orogenic interior is confined to single extreme events. The results of this thesis highlight the importance of snow and glacially derived melt waters in the western Himalaya, where extensive regions receive only limited amounts of monsoonal rainfall. These regions are therefore particularly susceptible to global warming with major implications on the hydrological cycle. However, the sediment discharge data show that infrequent monsoonal rainstorms that pass the orographic barrier of the Higher Himalaya are still the primary trigger of the highest-impact erosion events, despite being subordinate to snow and glacially–derived discharge. These findings may help to predict peak sediment flux events and could underpin the strategic development of preventative measures for hydropower infrastructures. N2 - Regen, Schnee- und Gletscherschmelze speisen die Flüsse des Himalajas, die eine große Bedeutung für die Landwirtschaft, Trinkwasserversorgung und Wasserkraftnutzung in Südasien aufweisen. Welchen Anteil die einzelnen Abflusskomponenten am Gesamtabfluss in Raum und Zeit besitzen, ist jedoch kaum quantifiziert, da es in der entlegenen Region an Bodenmessstationen mangelt. Aus diesem Grund ist auch wenig über die Auslöser und Herkunftsgebiete von hohen Sedimentaustragsereignissen bekannt, die im erheblichen Maße dazu beitragen, dass die Kapazität vonWasserkraftreservoiren abnimmt undWasserkraftturbinen abradieren. Daher fehlen bisher grundlegende Informationen zur räumlichen Verteilung von Wasserressourcen und zu den Ursachen von Erosionsprozessen. In dieser Arbeit benutze ich verschiedene Methoden um die Eigenschaften von und die Beziehungen zwischen Niederschlag, Abflussmenge und Sedimentaustrag im Sutlej-Tal zu untersuchen. In einer ersten Studie analysiere ich Tagesniederschläge (1998-2007) von 80 Wetterstationen aus dem westlichen Himalaja, um die räumliche Verteilung von Regen- und Schneeniederschlägen zu charakterisieren. Die weitere Analyse der Magnituden-Häufigkeitsverteilung von Regenfällen zeigt, dass 40% der sommerlichen Niederschläge auf monsunale Starkregenereignisse zurückgehen, die eine höhere Variabilität im Gebirgsinneren aufweisen als an der Gebirgsfront. Die Kombination von Niederschlagsdaten mit Sedimentaustragsdaten für einen der größten Zuflüsse des Sutlejs zeigt, dass monsunaler Niederschlag der primäre Auslöser von Erosionsprozessen im Gebirgsinneren ist, ungeachtet größerer Abflussmengen durch Schnee- und Gletscherschmelze. In einer zweiten Studie untersuche ich den Beitrag von Regen, Schnee- und Gletscherschmelze zur Abflussmenge im Sutlej-Tal (s55.000 km2) mit Hilfe eines hydrologischen Modells für den Jahreszeitraum 2000-2008. Um trotz der begrenzten Bodenmessungen eine hohe räumliche und zeitliche Auflösung zu erzielen, basiert das Modell auf täglichen Fernerkundungsdaten, die ich mit allen verfügbaren Bodenstationsdaten kalibriert und an diese angepasst habe. Die Kalibrierung zeigt, dass das Regenniederschlagsprodukt 3B42 der „Tropical Rainfall Measuring Mission“ (TRMM) den Bodenniederschlag in den semi-ariden bis ariden Gebirgsregionen mit zunehmender Trockenheit systematisch überschätzt. Die Modellierungsergebnisse verdeutlichen, dass die Schneeschmelze den bedeutendsten Beitrag zur Abflussmenge (74 %) zwischen April und Juni aufbringt, während Regen (56%) und Gletscherschmelze (17%) die Monsunsaison (Juli-September) prägen. Daher ist anzunehmen, dass der Klimawandel zu einer Verringerung der Abflussmenge zwischen April und Juni führen wird, was sich besonders auf das Gebirgsinnere auswirkt. In einer dritten Studie untersuche ich mit Hilfe von täglichen Messdaten der letzten Dekade die Ursachen und Eigenschaften des Sedimentaustrags in verschiedenen Bereichen des Sutlej-Einzugsgebietes. Auf der Grundlage von meteorologischen Daten, Erdbebenaufzeichnungen und Gesteinsfestigkeitsmessungen identifiziere ich Starkregenereignisse als häufigste Ursache für extreme Erosionsereignisse, die einen Großteil des gesamten Sedimentaustrags ausmachen. Großräumig betrachtet nimmt der Sedimentaustrag flussabwärts zu, was hauptsächlich auf den Anstieg der Abflussmenge zurückzuführen ist. Zur Monsunzeit treten Erosionsprozesse entlang der Himalajafront besonders häufig auf, während im Gebirgsinneren die Erosion auf einzelne Extremereignisse beschränkt ist. Die Ergebnisse dieser Arbeit untersteichen die Bedeutung von Schnee- und Gletscherschmelze im westlichen Himalaja, in dem große Gebiete nur vereinzelt von monsunalen Niederschlägen erreicht werden. Diese Gebiete sind daher besonders anfällig für den Klimawandel mit weitreichenden Konsequenzen für den Wasserhaushalt in der Region. Die Analyse von Sedimentaustragsdaten zeigt jedoch, dass vereinzelte monsunale Regenstürme, welche die topographische Barriere des Himalaja überqueren, die primäre Ursache von extremen Erosionsereignissen sind, trotz der größeren Abflussmengen von Schnee- und Gletscherschmelze im Gebirgsinneren. Diese Ergebnisse können dazu beitragen, große Erosionsereignisse vorherzusagen und vorbeugende Maßnahmen zum Schutz von Wasserkraftanlagen zu entwickeln. KW - Klimawandel KW - Erosion KW - Monsun KW - Regensturm KW - Suspendsionsfracht KW - climate change KW - erosion KW - monsoon KW - rainstorm KW - suspended sediment Y1 - 2011 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:kobv:517-opus-57905 ER - TY - JOUR A1 - Wu, Yunhua A1 - Wollenberger, Ursula A1 - Hofrichter, Martin A1 - Ullrich, Rene A1 - Scheibner, Katrin A1 - Scheller, Frieder W. T1 - Direct electron transfer of Agrocybe aegerita peroxygenase at electrodes modified with chitosan-capped Au nanoparticles and its bioelectrocatalysis to aniline JF - Sensors and actuators : B, Chemical N2 - Three different sizes of chitosan-capped Au nanoparticles were synthesized and were used to incorporate Agrocybe aegerita peroxygenase (AaeAPO) onto the surface of glassy carbon electrode. The direct electron transfer of AaeAPO was achieved in all films. The highest amount of electroactive enzyme and highest electron transfer rate constant k(s) of AaeAPO were obtained in the film with the smallest size of chitosan-capped Au nanoparticles. In anaerobic solutions, quasi-reversible oxidation and reduction are obtained with a formal potential of -0.280V vs. Ag/AgCl 1 M KCl in 100 mM (pH 7.0) PBS at scan rate of 1 V s(-1). Bioelectrocatalytic reduction currents can be obtained with the AaeAPO-modified electrode on addition of hydrogen peroxide. This reaction was suppressed when sodium azide, an inhibitor of AaeAPO, was present. Furthermore, the peroxide-dependent conversion of aniline was characterized and it was found that a polymer product via p-aminophenol is formed. And the AaeAPO biosensor was applied to determine aniline and p-aminophenol. KW - Agrocybe aegerita peroxygenase KW - Au nanoparticles KW - Direct electron transfer KW - Aniline biosensor KW - Bioelectrocatalysis Y1 - 2011 U6 - https://doi.org/10.1016/j.snb.2011.09.090 SN - 0925-4005 VL - 160 IS - 1 SP - 1419 EP - 1426 PB - Elsevier CY - Lausanne ER - TY - JOUR A1 - Worseck, Gabor A1 - Prochaska, J. Xavier A1 - McQuinn, Matthew A1 - Dall'Aglio, Aldo A1 - Fechner, Cora A1 - Hennawi, Joseph F. A1 - Reimers, Dieter A1 - Richter, Philipp A1 - Wisotzki, Lutz T1 - The end of Helium Reionization at z similar or equal to 2.7 Inferred from cosmic variance in HST/COS He II Ly alpha Absorption spectra JF - The astrophysical journal : an international review of spectroscopy and astronomical physics ; Part 2, Letters N2 - We report on the detection of strongly varying intergalactic He II absorption in HST/COS spectra of two z(em) similar or equal to 3 quasars. From our homogeneous analysis of the He II absorption in these and three archival sightlines, we find a marked increase in the mean He II effective optical depth from similar or equal to 1 at z similar or equal to 2.3 to greater than or similar to 5 at z similar or equal to 3.2, but with a large scatter of 2 less than or similar to tau(eff, He II) less than or similar to 5 at 2.7 < z < 3 on scales of similar to 10 proper Mpc. This scatter is primarily due to fluctuations in the He II fraction and the He II-ionizing background, rather than density variations that are probed by the coeval Hi forest. Semianalytic models of He II absorption require a strong decrease in the He II-ionizing background to explain the strong increase of the absorption at z greater than or similar to 2.7, probably indicating He II reionization was incomplete at z(reion) greater than or similar to 2.7. Likewise, recent three-dimensional numerical simulations of He II reionization qualitatively agree with the observed trend only if He II reionization completes at z(reion) similar or equal to 2.7 or even below, as suggested by a large tau(eff, He II) greater than or similar to 3 in two of our five sightlines at z < 2.8. By doubling the sample size at 2.7 less than or similar to z less than or similar to 3, our newly discovered He II sightlines for the first time probe the diversity of the second epoch of reionization when helium became fully ionized. KW - dark ages, reionization, first stars KW - diffuse radiation KW - intergalactic medium KW - quasars: absorption lines KW - quasars: individual (SDSS J092447.36+485242.8, SDSS J110155.74+105302.3) Y1 - 2011 U6 - https://doi.org/10.1088/2041-8205/733/2/L24 SN - 2041-8205 VL - 733 IS - 2 PB - IOP Publ. Ltd. CY - Bristol ER - TY - JOUR A1 - Wolff, Christian Michael A1 - Haug, Gerald H. A1 - Timmermann, Axel A1 - Damste, Jaap S. Sinninghe A1 - Brauer, Achim A1 - Sigman, Daniel M. A1 - Cane, Mark A. A1 - Verschuren, Dirk T1 - Reduced interannual rainfall variability in East Africa during the last Ice Age JF - Science N2 - Interannual rainfall variations in equatorial East Africa are tightly linked to the El Nino Southern Oscillation (ENSO), with more rain and flooding during El Nino and droughts in La Nina years, both having severe impacts on human habitation and food security. Here we report evidence from an annually laminated lake sediment record from southeastern Kenya for interannual to centennial-scale changes in ENSO-related rainfall variability during the last three millennia and for reductions in both the mean rate and the variability of rainfall in East Africa during the Last Glacial period. Climate model simulations support forward extrapolation from these lake sediment data that future warming will intensify the interannual variability of East Africa's rainfall. Y1 - 2011 U6 - https://doi.org/10.1126/science.1203724 SN - 0036-8075 VL - 333 IS - 6043 SP - 743 EP - 747 PB - American Assoc. for the Advancement of Science CY - Washington ER - TY - THES A1 - Wolff, Christian Michael T1 - East African monsoon variability since the last glacial T1 - Ostafrikanische Monsunvariabilität seit dem letztem Glazial N2 - The impact of global warming on human water resources is attracting increasing attention. No other region in this world is so strongly affected by changes in water supply than the tropics. Especially in Africa, the availability and access to water is more crucial to existence (basic livelihoods and economic growth) than anywhere else on Earth. In East Africa, rainfall is mainly influenced by the migration of the Inter-Tropical Convergence Zone (ITCZ) and by the El Niño Southern Oscillation (ENSO) with more rain and floods during El Niño and severe droughts during La Niña. The forecasting of East African rainfall in a warming world requires a better understanding of the response of ENSO-driven variability to mean climate. Unfortunately, existing meteorological data sets are too short or incomplete to establish a precise evaluation of future climate. From Lake Challa near Mount Kilimanjaro, we report records from a laminated lake sediment core spanning the last 25,000 years. Analyzing a monthly cleared sediment trap confirms the annual origin of the laminations and demonstrates that the varve-thicknesses are strongly linked to the duration and strength of the windy season. Given the modern control of seasonal ITCZ location on wind and rain in this region and the inverse relation between the two, thicker varves represent windier and thus drier years. El Niño (La Niña) events are associated with wetter (drier) conditions in east Africa and decreased (increased) surface wind speeds. Based on this fact, the thickness of the varves can be used as a tool to reconstruct a) annual rainfall b) wind season strength, and c) ENSO variability. Within this thesis, I found evidence for centennialscale changes in ENSO-related rainfall variability during the last three millennia, abrupt changes in variability during the Medieval Climate Anomaly and the Little Ice Age, and an overall reduction in East African rainfall and its variability during the Last Glacial period. Climate model simulations support forward extrapolation from these lake-sediment data, indicating that a future Indian Ocean warming will enhance East Africa’s hydrological cycle and its interannual variability in rainfall. Furthermore, I compared geochemical analyses from the sediment trap samples with a broad range of limnological, meteorological, and geological parameters to characterize the impact of sedimentation processes from the in-situ rocks to the deposited sediments. As a result an excellent calibration for existing μXRF data from Lake Challa over the entire 25,000 year long profile was provided. The climate development during the last 25,000 years as reconstructed from the Lake Challa sediments is in good agreement with other studies and highlights the complex interactions between long-term orbital forcing, atmosphere, ocean and land surface conditions. My findings help to understand how abrupt climate changes occur and how these changes correlate with climate changes elsewhere on Earth. N2 - Änderungen des Klimas in einer sich erwärmenden Erde haben große Auswirkungen auf den globalen und lokalen Wasserhaushalt und rücken anhand starker Extremereignisse immer häufiger in den Fokus der Öffentlichkeit. Besonders die Regionen der Tropen sind von derartigen Einschnitten stark gefährdet. Der jährliche Niederschlag in Ostafrika ist stark mit der saisonalen Wanderung der ITCZ (Innertropischen Konvergenzzone) sowie mit dem El Niño/Southern Oscillation (ENSO) Phänomen verbunden. Extreme Regenfälle und Überschwemmungen während El Niño Jahren stehen Trockenheit und Dürren in La Niña Jahren gegenüber. Prognosen über zukünftige Veränderungen der ostafrikanischen Niederschläge erfordern ein verbessertes Verständnis der ENSO antreibenden Faktoren. Unglücklicherweise sind die vorhandenen meteorologischen Datenreihen nicht lang genug oder besitzen nicht die benötigte Homogenität. Einen hilfreichen Beitrag können jährlich geschichtete Seesedimente des am Fuße des Kilimandscharo gelegenen Lake Challa leisten. Anhand einer monatlich aufgelösten Sedimentfalle konnte ich nachweisen, dass die rund 25.000 Jahre zurückreichenden Sedimente eine jährliche Struktur besitzen sowie die Dicke dieser jährlichen Schichtung (Warve) stark mit der Dauer und Intensität der saisonal windreichen/trockenen Jahreszeit verbunden ist. Dickere Warven repräsentieren windige/trockene Jahre, wohingegen dünnere Warven für windschwache und feuchte Jahre stehen. Stärkere Winde und kaum Niederschläge treten oft im Zusammenhang mit einem La Niña Ereignis in Ostafrika auf, wohingegen während eines El Niño Ereignisses häufig extreme Niederschläge mit wenig Wind zu beobachten sind. Anhand der Vermessung der Warven kann man verschiedene Klimaparameter rekonstruieren: a) den jährlichen Niederschlag b) jährliche Windgeschwindigkeiten und ihre Intensitäten sowie c) ENSO Variabilitäten. Die in meiner Arbeit gewonnenen klimatischen Informationen zeigen starke Änderungen der ENSO Variabilität innerhalb der letzten 3.000 Jahre mit starken Unterschieden während der Kleinen Eiszeit und während der Mittelalterlichen Warmzeit sowie deutlich trockene und windige Bedingungen mit sehr geringen ENSO Aktivitäten im glazialem Zeitraum (18.500 und 21.000 Jahren). Modellberechnungen unterstützen diese Ergebnisse einer Zunahme von Extremereignissen und feuchteren Bedingungen im Zuge einer Erwärmung des Indischen Ozeans. Mittels geochemischer Analysen der Sedimentfallenproben sowie die daraus resultierende Verknüpfung mit limnologischen und meteorologischen Parametern, konnte ich einen entscheidenden Beitrag zur erfolgreichen Interpretation der existierenden 25.000 Jahre langen μXRF Datensätze leisten. Der Anteil an allochthonem und autochthonem Eintrag kann so genau klassifiziert werden. Das dadurch gewonnene Bild der Klimaentwicklung der letzten 25.000 Jahre deckt sich hervorragend mit anderen Studien und ermöglicht Einblicke in das komplexe Zusammenspiel zwischen Ozean-Atmosphäre und Umwelt auf dem afrikanischen Kontinent. Besonders die für die Ostafrikaforschung extrem hohe Auflösung der Daten wird helfen, die abrupten Klimawechsel und Interaktionen besser verstehen zu können. KW - Lake Challa KW - Sedimentfalle KW - Warve KW - ENSO KW - Monsun KW - Lake Challa KW - sediment trap KW - varve KW - ENSO KW - monsoon Y1 - 2011 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:kobv:517-opus-58079 ER - TY - JOUR A1 - Wolf, Mark J. P. T1 - Theorizing navigable space in video games JF - DIGAREC Series N2 - Space is understood best through movement, and complex spaces require not only movement but navigation. The theorization of navigable space requires a conceptual representation of space which is adaptable to the great malleability of video game spaces, a malleability which allows for designs which combine spaces with differing dimensionality and even involve non-Euclidean configurations with contingent connectivity. This essay attempts to describe the structural elements of video game space and to define them in such a way so as to make them applicable to all video game spaces, including potential ones still undiscovered, and to provide analytical tools for their comparison and examination. Along with the consideration of space, there will be a brief discussion of navigational logic, which arises from detectable regularities in a spatial structure that allow players to understand and form expectations regarding a game’s spaces. Y1 - 2011 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:kobv:517-opus-49809 SN - 1867-6219 SN - 1867-6227 IS - 6 SP - 18 EP - 49 ER - TY - BOOK A1 - Wolf, Hans-Georg A1 - Cummings, Patrick T1 - A dictionary of Hong Kong English : words from the fragrant harbor Y1 - 2011 SN - 988-808330-9 PB - Univ. of Hong Kong CY - Hong Kong ER - TY - JOUR A1 - Wobbe, Theresa A1 - Kestler, Annegret A1 - Kauffenstein, Evelyn T1 - Statistische Klassifizierung und geschlechtliche Kategorisierung : die Unterscheidung von Haushalt und Betrieb im Medium der deutschen Berufsstatistik um 1900 Y1 - 2011 SN - 978-3-593-39526-5 ER - TY - JOUR A1 - Wobbe, Theresa A1 - Berrebi-Hoffmann, Isabelle A1 - Lallement, Michel T1 - Einleitung Y1 - 2011 SN - 978-3-593-39526-5 ER - TY - JOUR A1 - Wobbe, Theresa T1 - Max Weber : eine Soziologie ohne Geschlecht? Y1 - 2011 SN - 978-3-593-39526-5 ER - TY - CHAP A1 - Wittenberg, Eva A1 - Paczynski, Martin A1 - Wiese, Heike A1 - Jackendoff, Ray A1 - Kuperberg, Gina T1 - Light verbs make heavy work T2 - Psychophysiology : journal of the Society for Psychophysiological Research KW - sustained negativity KW - argument structure KW - language erp Y1 - 2011 SN - 0048-5772 VL - 48 IS - 3 SP - S105 EP - S105 PB - Wiley-Blackwell CY - Malden ER - TY - JOUR A1 - Witt, Stephanie H. A1 - Buchmann, Arlette F. A1 - Blomeyer, Dorothea A1 - Nieratschker, Vanessa A1 - Treutlein, Jens A1 - Esser, Günter A1 - Schmidt, Martin H. A1 - Bidlingmaier, Martin A1 - Wiedemann, Klaus A1 - Rietschel, Marcella A1 - Laucht, Manfred A1 - Wuest, Stefan A1 - Zimmermann, Ulrich S. T1 - An interaction between a neuropeptide Y gene polymorphism and early adversity modulates endocrine stress responses JF - Psychoneuroendocrinology N2 - Interindividual variability in the regulation of the human stress system accounts for a part of the individual's liability to stress-related diseases. These differences are influenced by environmental and genetic factors. Early childhood adversity is a well-studied environmental factor affecting an individual's stress response which has been shown to be modulated by gene environment interaction (GxE). Neuropeptide Y (NPY) plays a role in stress regulation and genetic variation in NPY may influence stress responses. In this study, we analyzed the association of a common variant in the NPY gene promoter, rs16147, with cortisol and ACTH responses to acute psychosocial stress in young adults from the Mannheim Study of Children at Risk (MARS), an ongoing epidemiological cohort study following the outcome of early adversity from birth into adulthood. We found evidence of a GxE interaction between rs16147 and early adversity significantly affecting HPA axis responses to acute psychosocial stress. These findings suggest that the neurobiological mechanisms linking early adverse experience and later neuroendocrine stress regulation are modulated by a gene variant whose functional relevance is documented by increasing convergent evidence from in vitro, animal and human studies. KW - GxE interaction KW - Stress KW - HPA KW - Neuropeptide Y KW - Early adversity Y1 - 2011 U6 - https://doi.org/10.1016/j.psyneuen.2010.12.015 SN - 0306-4530 VL - 36 IS - 7 SP - 1010 EP - 1020 PB - Elsevier CY - Oxford ER - TY - JOUR A1 - Wist, Dominic A1 - Schaefer, Mark A1 - Vogler, Walter A1 - Wollowski, Ralf T1 - Signal transition graph decomposition internal communication for speed independent circuit implementation JF - IET Computers and digital techniques N2 - Logic synthesis of speed independent circuits based on signal transition graph (STG) decomposition is a promising approach to tackle complexity problems like state-space explosion. Unfortunately, decomposition can result in components that in isolation have irreducible complete state coding conflicts. In earlier work, the authors showed how to resolve such conflicts by introducing internal communication between components, but only for very restricted specification structures. Here, they improve their former work by presenting algorithms for identifying delay transitions and inserting gyroscopes for specifications having a much more general structure. Thus, the authors are now able to synthesise controllers from real-life specifications. For all algorithms, they present correctness proofs and show their successful application to benchmarks, including very complex STGs arising in the context of control resynthesis. Y1 - 2011 U6 - https://doi.org/10.1049/iet-cdt.2010.0162 SN - 1751-8601 VL - 5 IS - 6 SP - 440 EP - 451 PB - Institution of Engineering and Technology CY - Hertford ER - TY - THES A1 - Wist, Dominic T1 - Attacking complexity in logic synthesis of asynchronous circuits T1 - Komplexitätsbewältigung in der Logiksynthese asynchroner Schaltungen N2 - Most of the microelectronic circuits fabricated today are synchronous, i.e. they are driven by one or several clock signals. Synchronous circuit design faces several fundamental challenges such as high-speed clock distribution, integration of multiple cores operating at different clock rates, reduction of power consumption and dealing with voltage, temperature, manufacturing and runtime variations. Asynchronous or clockless design plays a key role in alleviating these challenges, however the design and test of asynchronous circuits is much more difficult in comparison to their synchronous counterparts. A driving force for a widespread use of asynchronous technology is the availability of mature EDA (Electronic Design Automation) tools which provide an entire automated design flow starting from an HDL (Hardware Description Language) specification yielding the final circuit layout. Even though there was much progress in developing such EDA tools for asynchronous circuit design during the last two decades, the maturity level as well as the acceptance of them is still not comparable with tools for synchronous circuit design. In particular, logic synthesis (which implies the application of Boolean minimisation techniques) for the entire system's control path can significantly improve the efficiency of the resulting asynchronous implementation, e.g. in terms of chip area and performance. However, logic synthesis, in particular for asynchronous circuits, suffers from complexity problems. Signal Transitions Graphs (STGs) are labelled Petri nets which are a widely used to specify the interface behaviour of speed independent (SI) circuits - a robust subclass of asynchronous circuits. STG decomposition is a promising approach to tackle complexity problems like state space explosion in logic synthesis of SI circuits. The (structural) decomposition of STGs is guided by a partition of the output signals and generates a usually much smaller component STG for each partition member, i.e. a component STG with a much smaller state space than the initial specification. However, decomposition can result in component STGs that in isolation have so-called irreducible CSC conflicts (i.e. these components are not SI synthesisable anymore) even if the specification has none of them. A new approach is presented to avoid such conflicts by introducing internal communication between the components. So far, STG decompositions are guided by the finest output partitions, i.e. one output per component. However, this might not yield optimal circuit implementations. Efficient heuristics are presented to determine coarser partitions leading to improved circuits in terms of chip area. For the new algorithms correctness proofs are given and their implementations are incorporated into the decomposition tool DESIJ. The presented techniques are successfully applied to some benchmarks - including 'real-life' specifications arising in the context of control resynthesis - which delivered promising results. N2 - Moderner Schaltungsentwurf fokussiert hauptsächlich synchrone Schaltungstechnik mit allen inhärenten Problemen. Asynchone (d.h. ungetaktete) Schaltungen zeichnen sich jedoch nicht nur durch das Fehlen der Taktversatzproblematik gegenüber ihren synchronen Pendents aus, sondern auch insbesondere durch geringeren Energieverbrauch, günstigere EMV-Eigenschaften, hohe Performance, Modularität und Robustheit gegenüber Schwankungen in der Spannungsversorgung, im Herstellungsprozess sowie Temperaturunterschieden. Diese Vorteile werden mit höherer Integration sowie höheren Taktraten signifikanter. Jedoch ist der Entwurf und auch der Test asynchroner Schaltungen erheblich schwieriger verglichen mit synchronen Schaltungen. Entwurfswerkzeuge zur Synthese asynchroner Schaltungen aus Hochsprachen-Spezifikationen sind zwar inzwischen verfügbar, sie sind jedoch noch nicht so ausgereift und bei weitem noch nicht so akzeptiert in der Industrie, wie ihre Äquivalente für den synchronen Schaltungsentwurf. Insbesondere fehlt es an Werkzeugunterstützung im Bereich der Logiksynthese komplexer Steuerungen („Controller“), welche kritisch für die Effizienz – z.B. in Bezug auf Chipfläche und Geschwindigkeit – der resultierenden Schaltungen oder Systeme ist. Zur Spezifikation von Steuerungen haben sich Signalflankengraphen („signal transition graphs“, STGs) bewährt, die auch als Entwurfseinstieg für eine Logiksynthese von SI-Schaltungen („speed independent“) verwendet werden. (SI-Schaltungen gelten als sehr robuste asynchrone Schaltungen.) Aus den STGs werden zwecks Logiksynthese Automaten abgeleitet werden, deren Zustandszahl aber oft prohibitiv groß werden kann. Durch sogenannte STG-Dekomposition wird die Logiksynthese einer komplexen Schaltung ermöglicht, was bislang aufgrund von Zustandsexplosion oft nicht möglich war. Dabei wird der Spezifikations-STG laut einer gegebenen Partition von Ausgangssignalen in viele kleinere Teilnetze dekomponiert, wobei zu jedem Partitionsblock ein Teilnetz – mit normalerweise signifikant kleinerem Zustandsraum im Vergleich zur Spezifikation – erzeugt wird. Zu jedem Teilnetz wird dann eine Teilschaltung (Komponente) mittels Logiksynthese generiert. Durch die Anwendung von STG-Dekomposition können jedoch Teilnetze erzeugt werden, die sogenannte irreduzible CSC-Konflikte aufweisen (d.h. zu diesen Teilnetzen kann keine SI-Schaltung erzeugt werden), obwohl die Spezifikation keine solchen Konflikte hatte. Diese Arbeit präsentiert einen neuen Ansatz, welcher die Entstehung solcher irreduziblen Konflikte vermeidet, und zwar durch die Einführung interner Kommunikation zwischen den (zu den Teilnetzen gehörenden) Schaltungskomponenten. Bisher werden STG-Dekompositionen total durchgeführt, d.h. pro resultierender Komponente wird ein Ausgangssignal erzeugt. Das führt gewöhnlich nicht zu optimalen Schaltungsimplementierungen. In dieser Arbeit werden Heuristiken zur Bestimmung gröberer Ausgabepartitionen (d.h. Partitionsblöcke mit mehreren Ausgangssignalen) vorgestellt, die zu kleineren Schaltungen führen. Die vorgestellten Algorithmen werden formal abgesichert und wurden in das bereits vorhandene Dekompositionswerkzeug DESIJ integriert. An praxisrelevanten Beispielen konnten die vorgestellten Verfahren erfolgreich erprobt werden. KW - Asynchrone Schaltung KW - Logiksynthese KW - Komplexitätsbewältigung KW - STG-Dekomposition KW - CSC KW - asynchronous circuit KW - logic synthesis KW - speed independence KW - STG decomposition KW - CSC Y1 - 2011 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:kobv:517-opus-59706 ER - TY - JOUR A1 - Wischnewski, Juliane A1 - Mischke, Steffen A1 - Wang, Yongbo A1 - Herzschuh, Ulrike T1 - Reconstructing climate variability on the northeastern Tibetan Plateau since the last Lateglacial - a multi-proxy, dual-site approach comparing terrestrial and aquatic signals JF - Quaternary science reviews : the international multidisciplinary research and review journal N2 - A sediment core from a closed basin lake (Lake Kuhai) from the semi-arid northeastern Tibetan Plateau was analysed for its pollen record to infer Lateglacial and post glacial vegetation and climatic change. At Lake Kuhai five major vegetation and climate shifts could be identified: (1) a change from cold and dry to relatively warmer and more moist conditions at 14.8 cal ka BP: (2) a shift to conditions of higher effective moisture and a stepwise warmer climate at 13.6 cal ka BP; (3) a further shift with increased moisture but colder conditions at 7.0 cal ka BP; (4) a return to a significantly colder and drier phase at 6.3 cal ka BP; (5) and a change back to relatively moist conditions at 2.2 cal ka BP. To investigate the response of lake ecosystems to climatic changes, statistical comparisons were made between the lake Kuhai pollen record and a formerly published ostracod and sedimentary record from the same sediment core. Furthermore, the pollen and lacustrine proxies from lake Kuhai were compared to a previously published pollen and lacustrine record from the nearby Lake Koucha. Statistical comparisons were done using non-metric multidimensional scaling and Procrustes rotation. Differences between lacustrine and pollen responses within one site could be identified, suggesting that lacustrine proxies are partly influenced by in-lake or local catchment processes, whereas the terrestrial (pollen) proxy shows a regional climate signal. Furthermore, we found regional differences in proxy response between lake Kuhai and Lake Koucha. Both pollen records reacted in similar ways to major environmental changes, with minor differences in the timing and magnitude of these changes. The lacustrine records were very similar in their timing and magnitude of response to environmental changes; however, the nature of change was at times very distinct. To place the current study in the context of Holocene moisture evolution across the Tibetan Plateau, we applied a five-scale moisture index and average link clustering to all available continuous palaeo-climate records from the Tibetan Plateau to possibly find general patterns of moisture evolution on the Plateau. However, no common regional pattern of moisture evolution during the Holocene could be detected. We assign this to complex responses of different proxies to environmental and atmospheric changes in an already very heterogeneous mountain landscape where minor differences in elevation can cause strong variation in microenvironments. Y1 - 2011 U6 - https://doi.org/10.1016/j.quascirev.2010.10.001 SN - 0277-3791 VL - 30 IS - 1-2 SP - 82 EP - 97 PB - Elsevier CY - Oxford ER - TY - JOUR A1 - Wischnewski, Juliane A1 - Mackay, Anson W. A1 - Appleby, Peter G. A1 - Mischke, Steffen A1 - Herzschuh, Ulrike T1 - Modest diatom responses to regional warming on the southeast Tibetan Plateau during the last two centuries JF - Journal of paleolimnolog N2 - A general mean annual temperature increase accompanied with substantial glacial retreat has been noted on the Tibetan Plateau during the last two centuries but most significantly since the mid 1950s. These climate trends are particularly apparent on the southeastern Tibetan Plateau. However, the Tibetan Plateau (due to its heterogeneous mountain landscape) has very complex and spatially differing temperature and precipitations patterns. As a result, intensive palaeolimnological investigations are necessary to decipher these climatic patterns and to understand ecological responses to recent environmental change. Here we present palaeolimnological results from a (210)Pb/(137)Cs-dated sediment core spanning approximately the last 200 years from a remote high-mountain lake (LC6 Lake, working name) on the southeastern Tibetan Plateau. Sediment profiles of diatoms, organic variables (TOC, C:N) and grain size were investigated. The (210)Pb record suggests a period of rapid sedimentation, which might be linked to major tectonic events in the region ca. 1950. Furthermore, unusually high (210)Pb supply rates over the last 50 years suggest that the lake has possibly been subjected to increasing precipitation rates, sediment focussing and/or increased spring thaw. The majority of diatom taxa encountered in the core are typical of slightly acidic to circumneutral, oligotrophic, electrolyte-poor lakes. Diatom species assemblages were rich, and dominated by Cyclotella sp., Achnanthes sp., Aulacoseira sp. and fragilarioid taxa. Diatom compositional change was minimal over the 200-year period (DCCA = 0.85 SD, p = 0.59); only a slightly more diverse but unstable diatom assemblage was recorded during the past 50 years. The results indicate that large-scale environmental changes recorded in the twentieth century (i.e. increased precipitation and temperatures) are likely having an affect on the LC6 Lake, but so far these impacts are more apparent on the lake geochemistry than on the diatom flora. Local and/or regional peculiarities, such as increasing precipitation and cloud cover, or localized climatic phenomena, such as negative climate feedbacks, might have offset the effects of increasing mean surface temperatures. KW - Diatoms KW - Tibetan Plateau KW - Mountain lake KW - Climate change KW - Lake sediments KW - Palaeolimnology Y1 - 2011 U6 - https://doi.org/10.1007/s10933-011-9533-x SN - 0921-2728 VL - 46 IS - 2 SP - 215 EP - 227 PB - Springer CY - Dordrecht ER - TY - JOUR A1 - Wischnewski, Juliane A1 - Kramer, Annette A1 - Kong, Zhaochen A1 - Mackay, Anson W. A1 - Simpson, Gavin L. A1 - Mischke, Steffen A1 - Herzschuh, Ulrike T1 - Terrestrial and aquatic responses to climate change and human impact on the southeastern Tibetan Plateau during the past two centuries JF - Global change biology N2 - Rapid population growth and economic development have led to increased anthropogenic pressures on the Tibetan Plateau, causing significant land cover changes with potentially severe ecological consequences. To assess whether or not these pressures are also affecting the remote montane-boreal lakes on the SE Tibetan Plateau, fossil pollen and diatom data from two lakes were synthesized. The interplay of aquatic and terrestrial ecosystem response was explored in respect to climate variability and human activity over the past 200 years. Nonmetric multidimensional scaling and Procrustes rotation analysis were undertaken to determine whether pollen and diatom responses in each lake were similar and synchronous. Detrended canonical correspondence analysis was used to develop quantitative estimates of compositional species turnover. Despite instrumental evidence of significant climatic warming on the southeastern Plateau, the pollen and diatom records indicate very stable species composition throughout their profiles and show only very subtle responses to environmental changes over the past 200 years. The compositional species turnover (0.36-0.94 SD) is relatively low in comparison to the species reorganizations known from the periods during the mid-and early-Holocene (0.64-1.61 SD) on the SE Plateau, and also in comparison to turnover rates of sediment records from climate-sensitive regions in the circum arctic. Our results indicate that climatically induced ecological thresholds are not yet crossed, but that human activity has an increasing influence, particularly on the terrestrial ecosystem in our study area. Synergistic processes of post-Little Ice Age warming, 20th century climate warming and extensive reforestations since the 19th century have initiated a change from natural oak-pine forests to seminatural, likely less resilient pine-oak forests. Further warming and anthropogenic disturbances would possibly exceed the ecological threshold of these ecosystems and lead to severe ecological consequences. KW - climate change KW - compositional species turnover KW - diatoms KW - human impact KW - pollen KW - Procrustes rotation KW - Tibetan Plateau Y1 - 2011 U6 - https://doi.org/10.1111/j.1365-2486.2011.02474.x SN - 1354-1013 VL - 17 IS - 11 SP - 3376 EP - 3391 PB - Wiley-Blackwell CY - Malden ER - TY - THES A1 - Wischnewski, Juliane T1 - Reconstructing climate variability on the Tibetan Plateau : comparing aquatic and terrestrial signals T1 - Klimarekonstruktionen auf dem Tibet Plateau : aquatische und terrestrische Signale im Vergleich N2 - Spatial and temporal temperature and moisture patterns across the Tibetan Plateau are very complex. The onset and magnitude of the Holocene climate optimum in the Asian monsoon realm, in particular, is a subject of considerable debate as this time period is often used as an analogue for recent global warming. In the light of contradictory inferences regarding past climate and environmental change on the Tibetan Plateau, I have attempted to explain mismatches in the timing and magnitude of change. Therefore, I analysed the temporal variation of fossil pollen and diatom spectra and the geochemical record from palaeo-ecological records covering different time scales (late Quaternary and the last 200 years) from two core regions in the NE and SE Tibetan Plateau. For interpretation purposes I combined my data with other available palaeo-ecological data to set up corresponding aquatic and terrestrial proxy data sets of two lake pairs and two sets of sites. I focused on the direct comparison of proxies representing lacustrine response to climate signals (e.g., diatoms, ostracods, geochemical record) and proxies representing changes in the terrestrial environment (i.e., terrestrial pollen), in order to asses whether the lake and its catchments respond at similar times and magnitudes to environmental changes. Therefore, I introduced the established numerical technique procrustes rotation as a new approach in palaeoecology to quantitatively compare raw data of any two sedimentary records of interest in order to assess their degree of concordance. Focusing on the late Quaternary, sediment cores from two lakes (Kuhai Lake 35.3°N; 99.2°E; 4150 m asl; and Koucha Lake 34.0°N; 97.2°E; 4540 m asl) on the semi-arid northeastern Tibetan Plateau were analysed to identify post-glacial vegetation and environmental changes, and to investigate the responses of lake ecosystems to such changes. Based on the pollen record, five major vegetation and climate changes could be identified: (1) A shift from alpine desert to alpine steppe indicates a change from cold, dry conditions to warmer and more moist conditions at 14.8 cal. ka BP, (2) alpine steppe with tundra elements points to conditions of higher effective moisture and a stepwise warming climate at 13.6 cal. ka BP, (3) the appearance of high-alpine meadow vegetation indicates a further change towards increased moisture, but with colder temperatures, at 7.0 cal. ka BP, (4) the reoccurrence of alpine steppe with desert elements suggests a return to a significantly colder and drier phase at 6.3 cal. ka BP, and (5) the establishment of alpine steppe-meadow vegetation indicates a change back to relatively moist conditions at 2.2 cal. ka BP. To place the reconstructed climate inferences from the NE Tibetan Plateau into the context of Holocene moisture evolution across the Tibetan Plateau, I applied a five-scale moisture index and average link clustering to all available continuous pollen and non-pollen palaeoclimate records from the Tibetan Plateau, in an attempt to detect coherent regional and temporal patterns of moisture evolution on the Plateau. However, no common temporal or spatial pattern of moisture evolution during the Holocene could be detected, which can be assigned to the complex responses of different proxies to environmental changes in an already very heterogeneous mountain landscape, where minor differences in elevation can result in marked variations in microenvironments. Focusing on the past 200 years, I analysed the sedimentary records (LC6 Lake 29.5°N, 94.3°E, 4132 m asl; and Wuxu Lake 29.9°N, 101.1°E, 3705 m asl) from the southeastern Tibetan Plateau. I found that despite presumed significant temperature increases over that period, pollen and diatom records from the SE Tibetan Plateau reveal only very subtle changes throughout their profiles. The compositional species turnover investigated over the last 200 years appears relatively low in comparison to the species reorganisations during the Holocene. The results indicate that climatically induced ecological thresholds are not yet crossed, but that human activity has an increasing influence, particularly on the terrestrial ecosystem. Forest clearances and reforestation have not caused forest decline in our study area, but a conversion of natural forests to semi-natural secondary forests. The results from the numerical proxy comparison of the two sets of two pairs of Tibetan lakes indicate that the use of different proxies and the work with palaeo-ecological records from different lake types can cause deviant stories of inferred change. Irrespective of the timescale (Holocene or last 200 years) or region (SE or NE Tibetan Plateau) analysed, the agreement in terms of the direction, timing, and magnitude of change between the corresponding terrestrial data sets is generally better than the match between the corresponding lacustrine data sets, suggesting that lacustrine proxies may partly be influenced by in-lake or local catchment processes whereas the terrestrial proxy reflects a more regional climatic signal. The current disaccord on coherent temporal and spatial climate patterns on the Tibetan Plateau can partly be ascribed to the complexity of proxy response and lake systems on the Tibetan Plateau. Therefore, a multi-proxy, multi-site approach is important in order to gain a reliable climate interpretation for the complex mountain landscape of the Tibetan Plateau. N2 - Die räumlichen und zeitlichen Temperatur- und Feuchtigkeitsmuster auf dem Tibet-Plateau sind sehr komplex. Im Einzugsbereich der asiatischen Monsune sind insbesondere der Beginn und das Ausmaß des Klimaoptimums während des Holozäns von wissenschaftlichem Interesse, da diese Periode oft als Analogie für die derzeitige globale Klimaerwärmung herangezogen wird. In Hinblick auf sich teilweise widersprechende Paläoklima- und Umweltrekonstruktionen für das Tibet-Plateau, ist es mein Ziel, die bestehenden Unstimmigkeiten bezüglich des Zeitpunktes und des Ausmaßes des Umweltwandels zu erklären. Dafür wurden von mir zeitliche Variationen fossiler Pollen- und Diatomeenspektren und geochemische Untersuchungen an Seesedimenten unterschiedlicher Zeitskalen (Spätquartär und die letzten 200 Jahre) aus zwei Kernregionen auf dem NO und SO Tibet-Plateau analysiert. Zur Unterstützung der Interpretation wurden die hier erhobenen Daten mit bereits vorhandenen paläoökologischen Aufzeichnungen der Lokalitäten kombiniert, um Datensätze der entsprechenden aquatischen und terrestrischen Proxy-Daten (Stellvertreterdaten) zweier Seenpaare aus den beiden Regionen gegenüberstellen zu können. Hierbei konzentrierte ich mich auf den direkten Vergleich von Proxies, die die Seenentwicklung reflektieren (z.B. Diatomeen, Ostracoden, geochemische Eigenschaften), mit Proxies, die Veränderungen der terrestrischen Umgebung des Sees beschreiben (terrestrische Pollen). Durch diesen Vergleich lässt sich beurteilen, ob Veränderungen im See selbst mit Umweltveränderungen in dem jeweiligen Einzugsgebiet zeitlich übereinstimmen. Dafür habe ich die bereits etablierte numerische Methode Procrustes-Rotation als neuen Ansatz in der Paläoökologie eingeführt. Damit ist ein quantitativer Vergleich von Rohdaten zweier beliebiger sedimentärer Datensätze möglich, um den Grad der Übereinstimmung zu prüfen. Um die in dieser Arbeit rekonstruierten Umwelt- und Klimaereignisse des nordöstlichen Tibet-Plateaus in einen größeren Zusammenhang hinsichtlich holozäner Klimaentwicklung des gesamten Plateaus setzen zu können, und um schlüssige zeitliche und räumliche Klimatrends auf dem Plateau erkennen zu können, habe ich auf alle vorhandenen Paläoklimadatensätze einen Fünf-Skalen Feuchtigkeitsindex und eine Clusteranalyse angewandt. Es konnten jedoch keine einheitlichen zeitlichen und räumlichen Trends der holozänen Klimaentwicklung nachgewiesen werden, was meiner Analyse entsprechend, auf die komplexen Reaktionen verschiedener Proxies auf Umweltveränderungen in einer ohnehin sehr heterogen Berglandschaft, zurückgeführt werden kann. Die Ergebnisse des numerischen Proxy-Vergleichs beider Seenpaare zeigen, dass die Verwendung von verschiedenen Proxies und die Arbeit mit paläo-ökologischen Datensätzen unterschiedlicher See-Typen zu abweichenden Klimaableitungen führen können. Unabhängig vom untersuchten Zeitraum (Holozän oder die letzten 200 Jahren) oder der Region (SO oder NO Tibet-Plateau), ist die Übereinstimmung zweier Datensätze hinsichtlich der Richtung, des Zeitpunktes und des Ausmaßes der abgeleiteten Paläo-Umweltverhältnisse in der Regel zwischen den entsprechenden terrestrischen Datensätzen besser als zwischen den entsprechenden lakustrinen Datensätzen. Die derzeitige Uneinigkeit über stimmige zeitliche und räumliche Klimatrends auf dem Tibet-Plateau kann daher teilweise der Komplexität der verschieden Proxies und ihrer individuellen Empfindlichkeiten gegenüber Umweltveränderungen sowie der unterschiedlichen Reaktionsweise verschiedenartiger See-Systeme auf dem Plateau zugeschrieben werden. Meine Ergebnisse zeigen, dass ein „Multi-Proxy-Multi-Site-Ansatz“ für zuverlässige Paläoklimaableitungen für das Tibet-Plateau von zentraler Bedeutung ist. KW - Tibet Plateau KW - Holozän KW - Pollen KW - Diatomeen KW - Prokrustes Analyse KW - Tibetan Plateau KW - Holocene KW - Pollen KW - Diatoms KW - Procrustes rotation analysis Y1 - 2011 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:kobv:517-opus-52453 ER - TY - JOUR A1 - Wischerhoff, Erik A1 - Badi, Nezha A1 - Laschewsky, André A1 - Lutz, Jean-Francois ED - Börner, Hans Gerhard ED - Lutz, JF T1 - Smart polymer surfaces concepts and applications in biosciences JF - Advances in polymer science = Fortschritte der Hochpolymeren-Forschung JF - Advances in Polymer Science N2 - Stimuli-responsive macromolecules (i.e., pH-, thermo-, photo-, chemo-, and bioresponsive polymers) have gained exponential importance in materials science, nanotechnology, and biotechnology during the last two decades. This chapter describes the usefulness of this class of polymer for preparing smart surfaces (e.g., modified planar surfaces, particles surfaces, and surfaces of three-dimensional scaffolds). Some efficient pathways for connecting these macromolecules to inorganic, polymer, or biological substrates are described. In addition, some emerging bioapplications of smart polymer surfaces (e.g., antifouling surfaces, cell engineering, protein chromatography, tissue engineering, biochips, and bioassays) are critically discussed. KW - Antifouling surfaces KW - Bioactive surfaces KW - Biocompatible polymers KW - Bioseparation KW - Cell engineering KW - Polymer-modified surfaces KW - Stimuli-responsive polymers Y1 - 2011 SN - 978-3-642-20154-7 U6 - https://doi.org/10.1007/12_2010_88 SN - 0065-3195 VL - 240 IS - 1 SP - 1 EP - 33 PB - Springer CY - Berlin ER - TY - JOUR A1 - Wischer, Ilse T1 - Lexicalization of paraphrasal verb constructions with have and take Y1 - 2011 SN - 978-3-8233-6601-0 ER - TY - JOUR A1 - Wischer, Ilse T1 - Grammaticalization and Word Formation Y1 - 2011 SN - 978-0-19-958678-3 ER - TY - JOUR A1 - Wischer, Ilse T1 - Aspects of grammaticalization : current resources and future prospects Y1 - 2011 ER - TY - JOUR A1 - Wirth, Jonas A1 - Monturet, Serge A1 - Klamroth, Tillmann A1 - Saalfrank, Peter T1 - Adsorption and (photo-) electrochemical splitting of water on rutile ruthenium dioxide JF - epl : a letters journal exploring the frontiers of physics N2 - In this work, the adsorption and splitting of the water molecule by light and/or an external potential is investigated in the frame of (photo-) electrochemical cells using a rutile ruthenium dioxide anode. With the help of periodic density functional calculations, the adsorbed structures of H(2)O and some radicals involved in the splitting process (O, OH, OOH) are obtained and compared with the available experimental results. On the basis of these electronic-structure calculations, we use a method to calculate the stability of the reaction intermediates and conclude on the thermodynamical possibility of the water splitting reaction at the surface. We demonstrate that a moderate overpotential of 0.64 V is required for the reaction to take place at the RuO(2)(110) surface. Y1 - 2011 U6 - https://doi.org/10.1209/0295-5075/93/68001 SN - 0295-5075 VL - 93 IS - 6 PB - EDP Sciences CY - Mulhouse ER - TY - BOOK A1 - Wipper, Alexander T1 - Flugverkehr und Risikodiskurs BT - dargestellt am Ausbruch des Eyjafjallajökull 2010 N2 - Für den Flugverkehr als Teil eines regional und global verdichteten Infrastruktursystems sind Naturgefahren wie Vulkanausbrüche gleichbedeutend mit Risiken. Die Kommunikation von Risiken verläuft im Spannungsfeld von wirtschaftlichen und staatlichen Akteuren einerseits und Medien und Zivilgesellschaft andererseits. Demgegenüber stehen Modelle diskursiver Risikoregulierung als Instrumente öffentlicher Aushandlungsprozesse. Diskutiert werden Einflussfaktoren auf Entscheidungen im Kontext von Risikodiskursen. Dabei wird insbesondere die Funktionslogik der Medien untersucht. Am Beispiel der Aschewolke des Eyjafjallajökull 2010 wird die Phänomenkonstellation von Akteuren und Diskurspositionen illustriert und der Verlauf einer medialen Risikoentwicklung nachgezeichnet. T3 - Praxis Kultur- und Sozialgeographie | PKS - 52 KW - Risiko KW - Diskurs KW - Kommunikation KW - Medien KW - Flugverkehr KW - Vulkanasche KW - risk KW - discourse KW - communication KW - media KW - aviation KW - volcanic ash Y1 - 2011 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:kobv:517-opus-49533 SN - 978-3-86956-136-3 SN - 0934-716X SN - 1868-2499 PB - Universitätsverlag Potsdam CY - Potsdam ER - TY - JOUR A1 - Wintle, Brendan A. A1 - Bekessy, Sarah A. A1 - Keith, David A. A1 - van Wilgen, Brian W. A1 - Cabeza, Mar A1 - Schröder-Esselbach, Boris A1 - Carvalho, Silvia B. A1 - Falcucci, Alessandra A1 - Maiorano, Luigi A1 - Regan, Tracey J. A1 - Rondinini, Carlo A1 - Boitani, Luigi A1 - Possingham, Hugh P. T1 - Ecological-economic optimization of biodiversity conservation under climate change JF - Nature climate change N2 - Substantial investment in climate change research has led to dire predictions of the impacts and risks to biodiversity. The Intergovernmental Panel on Climate Change fourth assessment report(1) cites 28,586 studies demonstrating significant biological changes in terrestrial systems(2). Already high extinction rates, driven primarily by habitat loss, are predicted to increase under climate change(3-6). Yet there is little specific advice or precedent in the literature to guide climate adaptation investment for conserving biodiversity within realistic economic constraints(7). Here we present a systematic ecological and economic analysis of a climate adaptation problem in one of the world's most species-rich and threatened ecosystems: the South African fynbos. We discover a counterintuitive optimal investment strategy that switches twice between options as the available adaptation budget increases. We demonstrate that optimal investment is nonlinearly dependent on available resources, making the choice of how much to invest as important as determining where to invest and what actions to take. Our study emphasizes the importance of a sound analytical framework for prioritizing adaptation investments(4). Integrating ecological predictions in an economic decision framework will help support complex choices between adaptation options under severe uncertainty. Our prioritization method can be applied at any scale to minimize species loss and to evaluate the robustness of decisions to uncertainty about key assumptions. Y1 - 2011 U6 - https://doi.org/10.1038/NCLIMATE1227 SN - 1758-678X VL - 1 IS - 7 SP - 355 EP - 359 PB - Nature Publ. Group CY - London ER - TY - JOUR A1 - Winter, Martin T1 - Praxis des Studierens und Praxisbezug im Studium BT - Ausgewählte Befunde der Hochschulforschung zum „neuen“ und „alten“ Studieren JF - Potsdamer Beiträge zur Hochschulforschung Y1 - 2011 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:kobv:517-opus-52664 SN - 2192-1075 SN - 2192-1083 IS - 1 SP - 7 EP - 43 ER - TY - THES A1 - Winkler, Michael T1 - Thinning and turbulence in aqueous films N2 - This thesis covers the topic ”Thinning and Turbulence in Aqueous Films”. Experimental studies in two-dimensional systems gained an increasing amount of attention during the last decade. Thin liquid films serve as paradigms of atmospheric convection, thermal convection in the Earth’s mantle or turbulence in magnetohydrodynamics. Recent research on colloids, interfaces and nanofluids lead to advances in the developtment of micro-mixers (lab-on-a-chip devices). In this project a detailed description of a thin film experiment with focus on the particular surface forces is presented. The impact of turbulence on the thinning of liquid films which are oriented parallel to the gravitational force is studied. An experimental setup was developed which permits the capturing of thin film interference patterns under controlled surface and atmospheric conditions. The measurement setup also serves as a prototype of a mixer on the basis of thermally induced turbulence in liquid thin films with thicknesses in the nanometer range. The convection is realized by placing a cooled copper rod in the center of the film. The temperature gradient between the rod and the atmosphere results in a density gradient in the liquid film, so that different buoyancies generate turbulence. In the work at hand the thermally driven convection is characterized by a newly developed algorithm, named Cluster Imaging Velocimetry (CIV). This routine determines the flow relevant vector fields (velocity and deformation). On the basis of these insights the flow in the experiment was investigated with respect to its mixing properties. The mixing characteristics were compared to theoretical models and mixing efficiency of the flow scheme calculated. The gravitationally driven thinning of the liquid film was analyzed under the influence of turbulence. Strong shear forces lead to the generation of ultra-thin domains which consist of Newton black film. Due to the exponential expansion of the thin areas and the efficient mixing, this two-phase flow rapidly turns into the convection of only ultra-thin film. This turbulence driven transition was observed and quantified for the first time. The existence of stable convection in liquid nanofilms was proven for the first time in the context of this work. N2 - Diese Diplomarbeit behandelt das Thema ”Dünnung und Turbulenz in wässrigen Filmen”. Experimente in zweidimensionalen Systemen erfuhren in den vergangenen Jahren zunehmend an Aufmerksamkeit. Dünne Flüssigkeitsschichten dienen als Modell für atmosphärische Konvektion, thermische Konvektion im Erdmantel oder Turbulenz in der Magnetohydrodynamik. Aktuelle Forschung im Bereich der Kolloide, Grenzflächen und Nanofluidik führt zu Fortschritten in der Entwicklung von Mikromixern (”lab-on-a-chip”). In diesem Projekt wird eine detaillierte Beschreibung eines Dünnfilmexperiments mit Fokus auf die besonderen Oberflächenkräfte vorgestellt. Die Auswirkung der Turbulenz auf die Dünnung von parallel zur Gravitationskraft orientierten Flüssigkeitsschichten wurde untersucht. Es wurde ein Experiment entwickelt, welches die Aufnahme von Dünnschichtinterferenzmustern unter kontrollierten Oberflächenbedingungen und Atmosphäre erlaubt. Der Messaufbau dient auch als Prototyp eines Mixers auf Basis von thermisch induzierter Turbulenz in Flüssigkeitsfilmen mit Dicken im Nanometerbereich. Die Konvektion wird durch das Platzieren eines gekühlten Kupferstabs in der Mitte des Films realisiert. Der Temperaturgradient zwischen Stab und äußerer Atmosphäre resultiert in einem Dichtegradienten in dem flüssigen Film, sodass durch unterschiedliche Auftriebskräfte Turbulenz erzeugt wird. In der vorliegenden Arbeit ist die thermisch getriebenen Konvektion an Hand eines neu entwickelten Verfahrens (Cluster Imaging Velocimetry - CIV) zur Ermittlung des strömungsrelevanten Vektorfelder (Geschwindigkeit und Deformation) charakterisiert worden. Auf Basis dieser Erkenntnisse wurde die im Experiment vorherrschende Strömung in Hinsicht auf ihre Mischungseigenschaften im Vergleich zu theoretischen Modellen untersucht und die Mischungseffizienz berechnet. Die gravitationsgetriebene Ausdünnung der Flüssigkeitsschicht unter Einfluss der Turbulenz wurde analysiert. Durch starke Scherkräfte kommt es lokal zur Bildung ultradünner Domänen bestehend aus ”Newton black film”. Diese Zweiphasenströmung geht durch das exponentielle Ausdehnen der dünnen Bereiche und die effiziente Mischung sehr schnell in eine Konvektion von ausschließlich ultradünnem Film im Gleichgewichtszustand über. Dieser turbulenzgetriebene Übergang wurde zum ersten Mal beobachtet und quantifiziert. Die Existenz stabiler Konvektion in flüssigen Nanofilmen ist zum ersten Mal im Rahmen dieser Arbeit belegt worden. KW - wässrige Filme KW - Nanofluid KW - Mischung KW - Konvektion KW - Dünnung KW - Thin Film KW - Nanofluid KW - Mixing KW - Convection KW - Rapid thinning Y1 - 2011 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:kobv:517-opus-53107 ER - TY - JOUR A1 - Winkelmann, Ricarda A1 - Martin, Maria A. A1 - Haseloff, Monika A1 - Albrecht, Torsten A1 - Bueler, Ed A1 - Khroulev, C. A1 - Levermann, Anders T1 - The Potsdam parallel ice sheet model (PISM-PIK) - Part 1: Model description JF - The Cryosphere : TC ; an interactive open access journal of the European Geosciences Union N2 - We present the Potsdam Parallel Ice Sheet Model (PISM-PIK), developed at the Potsdam Institute for Climate Impact Research to be used for simulations of large-scale ice sheet-shelf systems. It is derived from the Parallel Ice Sheet Model (Bueler and Brown, 2009). Velocities are calculated by superposition of two shallow stress balance approximations within the entire ice covered region: the shallow ice approximation (SIA) is dominant in grounded regions and accounts for shear deformation parallel to the geoid. The plug-flow type shallow shelf approximation (SSA) dominates the velocity field in ice shelf regions and serves as a basal sliding velocity in grounded regions. Ice streams can be identified diagnostically as regions with a significant contribution of membrane stresses to the local momentum balance. All lateral boundaries in PISM-PIK are free to evolve, including the grounding line and ice fronts. Ice shelf margins in particular are modeled using Neumann boundary conditions for the SSA equations, reflecting a hydrostatic stress imbalance along the vertical calving face. The ice front position is modeled using a subgrid-scale representation of calving front motion (Albrecht et al., 2011) and a physically-motivated calving law based on horizontal spreading rates. The model is tested in experiments from the Marine Ice Sheet Model Intercomparison Project (MISMIP). A dynamic equilibrium simulation of Antarctica under present-day conditions is presented in Martin et al. (2011). Y1 - 2011 U6 - https://doi.org/10.5194/tc-5-715-2011 SN - 1994-0416 VL - 5 IS - 3 SP - 715 EP - 726 PB - Copernicus CY - Göttingen ER - TY - THES A1 - Winkelmann, Jan T1 - Die Mark Brandenburg des 14. Jahrhunderts : markgräfliche Herrschaft zwischen räumlicher "Ferne" und politischer "Krise" T2 - Studien zur brandenburgischen und vergleichenden Landesgeschichte Y1 - 2011 SN - 978-3-86732-112-9 VL - 5 PB - Lukas-Verl. CY - Berlin ER - TY - JOUR A1 - Winkelmann, Ingo T1 - GASP der Europäischen Union in den Vereinten Nationen am Beispiel der Reform des Sicherheitsrats der Vereinten Nationen JF - Die Vereinten Nationen vor globalen Herausforderungen : Referate der Potsdamer UNO-Konferenzen 2000–2008 N2 - Inhalt: - 1. Die Nichtwahrnehmung von Reformchancen durch die EU-Mitgliedstaaten - 2. Das Reformraster: der Razali-Vorschlag - 3. Hürden für eine einheitliche EU-Vertretung im UN-Sicherheitsrat Y1 - 2011 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:kobv:517-opus-61219 SP - 371 EP - 377 PB - Universitätsverlag Potsdam CY - Potsdam ER - TY - JOUR A1 - Winkelmann, Ingo T1 - Die Vereinten Nationen, das Seerecht und die Polarregionen JF - Die Vereinten Nationen zehn Jahre nach dem Millenniumsgipfel 2000 - eine Bilanz N2 - I. Die Vereinten Nationen als Seerechtsrahmen II. Die arktische Polarregion III. Die antarktische Polarregion IV. Abschließende Bemerkungen Y1 - 2011 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:kobv:517-opus4-101555 VL - 2011 IS - 9 SP - 27 EP - 37 PB - Universitätsverlag Potsdam CY - Potsdam ER - TY - JOUR A1 - Winkel, B. A1 - Ben Bekhti, Nadya A1 - Darmstaedter, V. A1 - Floeer, L. A1 - Kerp, J. A1 - Richter, Philipp T1 - The high-velocity cloud complex Galactic center negative as seen by EBHIS and GASS I. Cloud catalog and global properties JF - Astronomy and astrophysics : an international weekly journal N2 - Using Milky Way data of the new Effelsberg-Bonn HI Survey (EBHIS) and the Galactic All-Sky Survey (GASS), we present a revised picture of the high-velocity cloud (HVC) complex Galactic center negative (GCN). Owing to the higher angular resolution of these surveys compared to previous studies (e.g., the Leiden Dwingeloo Survey), we resolve complex GCN into lots of individual tiny clumps, that mostly have relatively broad line widths of more than 15 km s(-1). We do not detect a diffuse extended counterpart, which is unusual for an HVC complex. In total 243 clumps were identified and parameterized which allows us to statistically analyze the data. Cold-line components (i.e.,Delta upsilon(fwhm) < 7.5 km s(-1)) are found in about 5% only of the identified cloudlets. Our analysis reveals that complex GCN is likely built up of several subpopulations that do not share a common origin. Furthermore, complex GCN might be a prime example for warm-gas accretion onto the Milky Way, where neutral HI clouds are not stable against interaction with the Milky Way gas halo and become ionized prior to accretion. KW - ISM: clouds KW - Galaxy: halo Y1 - 2011 U6 - https://doi.org/10.1051/0004-6361/201117357 SN - 0004-6361 VL - 533 IS - 18 PB - EDP Sciences CY - Les Ulis ER -