TY - BOOK A1 - Ungelenk, Johannes T1 - Touching at a Distance BT - Shakespeare's Theatre T3 - Edinburgh Critical Studies in Shakespeare and Philosophy : ECSSP N2 - Studies the capacity of Shakespeare’s plays to touch and think about touchBased on plays from all major genres: Hamlet, The Tempest, Richard III, Much Ado About Nothing and Troilus and CressidaCentres on creative, close readings of Shakespeare’s plays, which aim to generate critical impulses for the 21st century readerBrings Shakespeare Studies into touch with philosophers and theoreticians from a range of disciplinary areas – continental philosophy, literary criticism, psychoanalysis, sociology, phenomenology, law, linguistics: Friedrich Nietzsche, Maurice Blanchot, Jacques Lacan, Luce Irigaray, Jacques Derrida, Roland Barthes, Niklas Luhmann, Hans Blumenberg, Carl Schmitt, J. L. AustinTheatre has a remarkable capacity: it touches from a distance. The audience is affected, despite their physical separation from the stage. The spectators are moved, even though the fictional world presented to them will never come into direct touch with their real lives. Shakespeare is clearly one of the master practitioners of theatrical touch. As the study shows, his exceptional dramaturgic talent is intrinsically connected with being one of the great thinkers of touch. His plays fathom the complexity and power of a fascinating notion – touch as a productive proximity that is characterised by unbridgeable distance – which philosophers like Friedrich Nietzsche, Maurice Blanchot, Jacques Derrida, Luce Irigaray and Jean-Luc Nancy have written about, centuries later. By playing with touch and its metatheatrical implications, Shakespeare raises questions that make his theatrical art point towards modernity: how are communities to form when traditional institutions begin to crumble? What happens to selfhood when time speeds up, when oneness and timeless truth can no longer serve as reliable foundations? What is the role and the capacity of language in a world that has lost its seemingly unshakeable belief and trust in meaning? How are we to conceive of the unthinkable extremes of human existence – birth and death – when the religious orthodoxy slowly ceases to give satisfactory explanations? Shakespeare’s theatre not only prompts these questions, but provides us with answers. They are all related to touch, and they are all theatrical at their core: they are argued and performed by the striking experience of theatre’s capacities to touch – at a distance Y1 - 2023 SN - 978-1-4744-9784-8 SN - 978-1-4744-9785-5 SN - 978-1-4744-9782-4 U6 - https://doi.org/10.1515/9781474497848 PB - Edinburgh University Press CY - Edinburgh ER - TY - JOUR A1 - Fischer, Caroline A1 - Heuberger, Moritz A1 - Heine, Moreen T1 - The impact of digitalization in the public sector BT - a systematic literature review JF - Der moderne Staat N2 - The digitalization of public administration is increasingly moving forward. This systematic literature review analyzes empirical studies that explore the impacts of digitalization projects (n=93) in the public sector. Bibliometrically, only a few authors have published several times on this topic so far. Most studies focusing on impact come from the US or China, and are related to Computer Science. In terms of content, the majority of examined articles studies services to citizens, and therefore consider them when measuring impact. A classification of the investigated effects by dimensions of public value shows that the analysis of utilitarian-instrumental values, such as efficiency or performance, is prevalent. More interdisciplinary cooperation is needed to research the impact of digitalization in the public sector. The different dimensions of impact should be linked more closely. In addition, research should focus more on the effects of digitalization within administration. KW - digital transformation KW - e-government KW - impact evaluation KW - public value KW - public values Y1 - 2021 U6 - https://doi.org/10.3224/dms.v14i1.13 SN - 1865-7192 SN - 2196-1395 VL - 14 IS - 1 SP - 3 EP - 23 PB - Barbara Budrich CY - Leverkusen-Opladen ER - TY - CHAP A1 - Heuberger, Moritz A1 - Schwab, Christian ED - Bergström, Tomas ED - Franzke, Jochen ED - Kuhlmann, Sabine ED - Wayenberg, Ellen T1 - Challenges of digital service provision for local governments from the citizens’ view BT - comparing citizens’ expectations and their experiences of digital service provision T2 - The future of local self-government Y1 - 2021 SN - 978-3-030-56058-4 SN - 978-3-030-56059-1 U6 - https://doi.org/10.1007/978-3-030-56059-1_9 SP - 115 EP - 130 PB - Palgrave Macmillan CY - Cham ER - TY - THES A1 - Aue, Lars T1 - Cyclone impacts on sea ice in the Atlantic Arctic Ocean T1 - Auswirkungen von Zyklonen auf das Meereis im Atlantischen Arktischen Ozean N2 - The Arctic is the hot spot of the ongoing, global climate change. Over the last decades, near-surface temperatures in the Arctic have been rising almost four times faster than on global average. This amplified warming of the Arctic and the associated rapid changes of its environment are largely influenced by interactions between individual components of the Arctic climate system. On daily to weekly time scales, storms can have major impacts on the Arctic sea-ice cover and are thus an important part of these interactions within the Arctic climate. The sea-ice impacts of storms are related to high wind speeds, which enhance the drift and deformation of sea ice, as well as to changes in the surface energy budget in association with air mass advection, which impact the seasonal sea-ice growth and melt. The occurrence of storms in the Arctic is typically associated with the passage of transient cyclones. Even though the above described mechanisms how storms/cyclones impact the Arctic sea ice are in principal known, there is a lack of statistical quantification of these effects. In accordance with that, the overarching objective of this thesis is to statistically quantify cyclone impacts on sea-ice concentration (SIC) in the Atlantic Arctic Ocean over the last four decades. In order to further advance the understanding of the related mechanisms, an additional objective is to separate dynamic and thermodynamic cyclone impacts on sea ice and assess their relative importance. Finally, this thesis aims to quantify recent changes in cyclone impacts on SIC. These research objectives are tackled utilizing various data sets, including atmospheric and oceanic reanalysis data as well as a coupled model simulation and a cyclone tracking algorithm. Results from this thesis demonstrate that cyclones are significantly impacting SIC in the Atlantic Arctic Ocean from autumn to spring, while there are mostly no significant impacts in summer. The strength and the sign (SIC decreasing or SIC increasing) of the cyclone impacts strongly depends on the considered daily time scale and the region of the Atlantic Arctic Ocean. Specifically, an initial decrease in SIC (day -3 to day 0 relative to the cyclone) is found in the Greenland, Barents and Kara Seas, while SIC increases following cyclones (day 0 to day 5 relative to the cyclone) are mostly limited to the Barents and Kara Seas. For the cold season, this results in a pronounced regional difference between overall (day -3 to day 5 relative to the cyclone) SIC-decreasing cyclone impacts in the Greenland Sea and overall SIC-increasing cyclone impacts in the Barents and Kara Seas. A cyclone case study based on a coupled model simulation indicates that both dynamic and thermodynamic mechanisms contribute to cyclone impacts on sea ice in winter. A typical pattern consisting of an initial dominance of dynamic sea-ice changes followed by enhanced thermodynamic ice growth after the cyclone passage was found. This enhanced ice growth after the cyclone passage most likely also explains the (statistical) overall SIC-increasing effects of cyclones in the Barents and Kara Seas in the cold season. Significant changes in cyclone impacts on SIC over the last four decades have emerged throughout the year. These recent changes are strongly varying from region to region and month to month. The strongest trends in cyclone impacts on SIC are found in autumn in the Barents and Kara Seas. Here, the magnitude of destructive cyclone impacts on SIC has approximately doubled over the last four decades. The SIC-increasing effects following the cyclone passage have particularly weakened in the Barents Sea in autumn. As a consequence, previously existing overall SIC-increasing cyclone impacts in this region in autumn have recently disappeared. Generally, results from this thesis show that changes in the state of the sea-ice cover (decrease in mean sea-ice concentration and thickness) and near-surface air temperature are most important for changed cyclone impacts on SIC, while changes in cyclone properties (i.e. intensity) do not play a significant role. N2 - Die Arktis ist der Hotspot des globalen Klimawandels. In den letzten Jahrzehnten sind die oberflächennahen Temperaturen in der Arktis fast viermal so schnell gestiegen wie im globalen Durchschnitt. Diese verstärkte Erwärmung der Arktis und die damit verbundenen raschen Umweltveränderungen werden u.a. durch Wechselwirkungen zwischen den einzelnen Komponenten des arktischen Klimasystems angetrieben. Auf täglichen bis wöchentlichen Zeitskalen können Stürme große Einflüsse auf das arktische Meereis haben und sind somit ein wichtiger Teil dieser Wechselwirkungen innerhalb des arktischen Klimas. Der Einfluss der Stürme auf das Meereis resultiert aus den hohen Windgeschwindigkeiten, welche die Drift und Verformung des Meereises verstärken, sowie aus Änderungen in der Oberflächenenergiebilanz im Zusammenhang mit der Advektion von Luftmassen, was das Wachstum und Schmelzen des Meereises beeinflusst. Das Auftreten von Stürmen in der Arktis ist oft mit dem Durchzug von Zyklonen verbunden. Obwohl die oben beschriebenen Mechanismen, wie sich Stürme/Zyklone auf das arktische Meereis auswirken, im Prinzip bekannt sind, fehlt es an einer statistischen Quantifizierung dieser Effekte. Dementsprechend ist das übergeordnete Ziel dieser Arbeit eine statistische Quantifizierung der Auswirkungen von Zyklonen auf die Meereiskonzentration (engl. Sea Ice Concentration, SIC) im atlantischen Arktischen Ozeans über die letzten vier Jahrzehnte. Um ein Verständnis für die zugrunde liegenden Mechanismen zu erlangen, besteht ein weiteres Ziel darin, die dynamischen und thermodynamischen Auswirkungen von Zyklonen auf das Meereis zu trennen und ihre relative Bedeutung zu analysieren. Zuletzt zielt diese Arbeit darauf ab, aktuelle Veränderungen der Zykloneneinflüsse auf das Meereis zu quantifizieren. Zum Erreichen dieser Forschungsziele werden verschiedene Datensätze genutzt, darunter atmosphärische und ozeanische Reanalysedaten sowie eine gekoppelte Modellsimulation und ein Algorithmus zur automatischen Identifikation von Zyklonen. Die Ergebnisse dieser Arbeit zeigen, dass Zyklone die SIC im atlantischen Arktischen Ozean von Herbst bis Frühjahr signifikant beeinflussen, während es im Sommer meist keine signifikanten Auswirkungen gibt. Die Stärke und das Vorzeichen (abnehmende oder zunehmende SIC) der Auswirkungen der Zyklone hängt stark von der betrachteten täglichen Zeitskala und der Region des Arktischen Ozeans ab. So ist ein anfänglicher Rückgang der SIC (Tag -3 bis Tag 0 relativ zum Zyklonendurchgang) in der Grönland-, der Barents- und der Karasee festzustellen, während ein SIC-Anstieg nach dem Zyklonendurchgang (Tag 0 bis Tag 5 relativ zum Zyklonendurchgang) hauptsächlich auf die Barents- und die Karasee beschränkt ist. Für die kalte Jahreszeit ergibt sich daraus ein ausgeprägter regionaler Unterschied zwischen insgesamt (Tag -3 bis Tag 5 relativ zum Zyklon) SIC-verringernden Zyklonenauswirkungen in der Grönlandsee und insgesamt SIC-erhöhenden Zyklonenauswirkungen in der Barents- und Karasee. Die Analyse spezifischer Zyklonenfälle basierend auf einer gekoppelten Modellsimulation zeigt, dass sowohl dynamische als auch thermodynamische Mechanismen zu den Auswirkungen von Zyklonen auf das Meereis im Winter beitragen. Hierbei wurde ein typisches Muster bestehend aus einer anfänglichen Dominanz dynamischer Meereisveränderungen gefolgt von verstärktem thermodynamischem Eiswachstum nach der Zyklonenpassage gefunden. Dieses verstärkte Eiswachstum nach der Zyklonenpassage erklärt u.a. auch die (statistischen) insgesamt SIC-erhöhenden Effekte von Zyklonen in der Barents- und Karasee im Winter. Signifikante Änderungen in den Auswirkungen von Zyklonen auf die SIC über die letzten vier Dekaden sind das ganze Jahr über zu finden. Diese Veränderungen variieren stark von Region zu Region und von Monat zu Monat. Die stärksten Trends in den Auswirkungen von Zyklonen auf die SIC sind im Herbst in der Barents- und Karasee zu beobachten. Hier hat sich die Stärke der zerstörerischen Auswirkungen von Zyklonen auf die SIC in den letzten vier Jahrzehnten ungefähr verdoppelt. Die SIC-erhöhenden Effekte nach der Zyklonenpassage haben sich in der Barentssee im Herbst besonders abgeschwächt. Dadurch sind zuvor existierende, insgesamt SIC-erhöhende Zyklonenauswirkungen in dieser Region und Jahreszeit zuletzt verschwunden. Generell zeigen die Ergebnisse dieser Arbeit, dass Änderungen im Zustand des Meereises (Abnahme der mittleren Meereiskonzentration und -dicke) sowie in der Lufttemperatur die veränderten Auswirkungen der Zyklonen auf die SIC antreiben, während Veränderungen in den Eigenschaften der Zyklonen (z.B. ihre Intensität) keine wesentliche Rolle spielen. KW - Arctic KW - atmosphere KW - sea ice KW - cyclones KW - meteorology KW - Arktis KW - Atmosphäre KW - Meereis KW - Zyklone KW - Meteorologie Y1 - 2024 U6 - http://nbn-resolving.de/urn/resolver.pl?urn:nbn:de:kobv:517-opus4-634458 SP - VIII, 131 ER - TY - JOUR A1 - Wolf, Sebastian G. A1 - Huismans, Ritske S. A1 - Braun, Jean A1 - Yuan, Xiaoping T1 - Topography of mountain belts controlled by rheology and surface processes JF - Nature : the international weekly journal of science N2 - It is widely recognized that collisional mountain belt topography is generated by crustal thickening and lowered by river bedrock erosion, linking climate and tectonics(1-4). However, whether surface processes or lithospheric strength control mountain belt height, shape and longevity remains uncertain. Additionally, how to reconcile high erosion rates in some active orogens with long-term survival of mountain belts for hundreds of millions of years remains enigmatic. Here we investigate mountain belt growth and decay using a new coupled surface process(5,6) and mantle-scale tectonic model(7). End-member models and the new non-dimensional Beaumont number, Bm, quantify how surface processes and tectonics control the topographic evolution of mountain belts, and enable the definition of three end-member types of growing orogens: type 1, non-steady state, strength controlled (Bm > 0.5); type 2, flux steady state(8), strength controlled (Bm approximate to 0.4-0.5); and type 3, flux steady state, erosion controlled (Bm < 0.4). Our results indicate that tectonics dominate in Himalaya-Tibet and the Central Andes (both type 1), efficient surface processes balance high convergence rates in Taiwan (probably type 2) and surface processes dominate in the Southern Alps of New Zealand (type 3). Orogenic decay is determined by erosional efficiency and can be subdivided into two phases with variable isostatic rebound characteristics and associated timescales. The results presented here provide a unified framework explaining how surface processes and lithospheric strength control the height, shape, and longevity of mountain belts. Y1 - 2022 U6 - https://doi.org/10.1038/s41586-022-04700-6 SN - 0028-0836 SN - 1476-4687 VL - 606 IS - 7914 SP - 516 EP - 521 PB - Nature portfolio CY - Berlin ER - TY - JOUR A1 - Hänel, Hilkje C. T1 - Potentially disabled? JF - Inquiry N2 - Ten years ago, I was diagnosed with a rare illness called Myasthenia Gravis. Myasthenia Gravis is a long-term neuromuscular autoimmune disease where antibodies block or destroy specific receptors at the junction between nerve and muscle; hence, nerve impulses fail to trigger muscle contractions. The disease leads to varying degrees of muscle weakness. Currently, I have only minor symptoms, I am not seriously impaired, and I do not suffer from any social disadvantage because of my illness. Yet, my life and my body since my diagnosis feel different than before. In this paper I aim to make this feeling intelligible and propose that it is a state of what I call ‘latent impairment’. Latent impairment is a state of being ‘in between’, different from being actually impaired and also different from being abled-bodied. The theory takes its cues both from social constructionist theories of disability as well as theories of (chronic) illness and their focus on the importance of subjectivity. Furthermore, I suggest that a phenomenological understanding of latent impairment can show possible ways of becoming an ally to the DRM. KW - disability KW - chronic illness KW - latent impairment KW - social construction Y1 - 2022 U6 - https://doi.org/10.1080/0020174X.2022.2136753 SN - 0020-174X SN - 1502-3923 SP - 1 EP - 26 PB - Routledge, Taylor & Francis CY - London ER - TY - JOUR A1 - Weaver, Catherine A1 - Heinzel, Mirko A1 - Jorgensen, Samantha A1 - Flores, Joseph T1 - Bureaucratic representation in the IMF and the World Bank JF - Global perspectives N2 - The legitimacy and effectiveness of international organizations are often linked directly to issues of representation—not only on their high-level governing boards and in top leadership but also within their staff. This article explores two key questions of bureaucratic representation in the critical cases of the International Monetary Fund and World Bank. First, we seek to unpack three essential dimensions of staff representation—nationality, education, and gender—to explain how representation may matter for international organizations. Second, we aim to describe the multiple dimensions of representation in the International Monetary Fund and the World Bank over the past twenty years by deploying a novel dataset on staff demographics, focusing on ranks with decision-making authority within the institutions. Our descriptive analysis reveals that the International Monetary Fund and the World Bank have made considerable efforts to diversify their bureaucracies. Nonetheless, representation remains uneven; for example, nationals from middle- and low-income countries, women, and staff without economics degrees from prominent US- or UK-based universities are less present in key leadership positions. These results may be well explained by the particular needs of the institutions’ technical mandates and limits in the supply of qualified staff and, as such, need not be seen as suboptimal. Nonetheless, perceived imbalances in representation may continue to pose external legitimation and operational challenges to the International Monetary Fund and the World Bank in a complex political environment where such multidimensional representation is important to sustaining the buy-in of donor and borrower countries alike. To this end, we recommend that the International Monetary Fund and the World Bank enhance their diversity and inclusion efforts by increasing transparency via reporting disaggregated data on workforce composition and introducing annual requirements to publish progress reports with management feedback to strengthen internal and external accountability. KW - representation KW - international bureaucracy KW - multilateralism KW - World Bank KW - IMF Y1 - 2022 U6 - https://doi.org/10.1525/gp.2022.39684 SN - 2575-7350 VL - 3 IS - 1 PB - University of California Press CY - Oakland, CA ER - TY - JOUR A1 - Pena-Camargo, Francisco A1 - Thiesbrummel, Jarla A1 - Hempel, Hannes A1 - Musiienko, Artem A1 - Le Corre, Vincent M. A1 - Diekmann, Jonas A1 - Warby, Jonathan A1 - Unold, Thomas A1 - Lang, Felix A1 - Neher, Dieter A1 - Stolterfoht, Martin T1 - Revealing the doping density in perovskite solar cells and its impact on device performance JF - Applied physics reviews N2 - Traditional inorganic semiconductors can be electronically doped with high precision. Conversely, there is still conjecture regarding the assessment of the electronic doping density in metal-halide perovskites, not to mention of a control thereof. This paper presents a multifaceted approach to determine the electronic doping density for a range of different lead-halide perovskite systems. Optical and electrical characterization techniques, comprising intensity-dependent and transient photoluminescence, AC Hall effect, transfer-length-methods, and charge extraction measurements were instrumental in quantifying an upper limit for the doping density. The obtained values are subsequently compared to the electrode charge per cell volume under short-circuit conditions ( CUbi/eV), which amounts to roughly 10(16) cm(-3). This figure of merit represents the critical limit below which doping-induced charges do not influence the device performance. The experimental results consistently demonstrate that the doping density is below this critical threshold 10(12) cm(-3), which means << CUbi / e V) for all common lead-based metal-halide perovskites. Nevertheless, although the density of doping-induced charges is too low to redistribute the built-in voltage in the perovskite active layer, mobile ions are present in sufficient quantities to create space-charge-regions in the active layer, reminiscent of doped pn-junctions. These results are well supported by drift-diffusion simulations, which confirm that the device performance is not affected by such low doping densities. Y1 - 2022 U6 - https://doi.org/10.1063/5.0085286 SN - 1931-9401 VL - 9 IS - 2 PB - AIP Publishing CY - Melville ER - TY - JOUR A1 - Brunner, Martin A1 - Keller, Lena A1 - Stallasch, Sophie E. A1 - Kretschmann, Julia A1 - Hasl, Andrea A1 - Preckel, Franzis A1 - Luedtke, Oliver A1 - Hedges, Larry T1 - Meta-analyzing individual participant data from studies with complex survey designs BT - a tutorial on using the two-stage approach for data from educational large-scale assessments JF - Research synthesis methods N2 - Descriptive analyses of socially important or theoretically interesting phenomena and trends are a vital component of research in the behavioral, social, economic, and health sciences. Such analyses yield reliable results when using representative individual participant data (IPD) from studies with complex survey designs, including educational large-scale assessments (ELSAs) or social, health, and economic survey and panel studies. The meta-analytic integration of these results offers unique and novel research opportunities to provide strong empirical evidence of the consistency and generalizability of important phenomena and trends. Using ELSAs as an example, this tutorial offers methodological guidance on how to use the two-stage approach to IPD meta-analysis to account for the statistical challenges of complex survey designs (e.g., sampling weights, clustered and missing IPD), first, to conduct descriptive analyses (Stage 1), and second, to integrate results with three-level meta-analytic and meta-regression models to take into account dependencies among effect sizes (Stage 2). The two-stage approach is illustrated with IPD on reading achievement from the Programme for International Student Assessment (PISA). We demonstrate how to analyze and integrate standardized mean differences (e.g., gender differences), correlations (e.g., with students' socioeconomic status [SES]), and interactions between individual characteristics at the participant level (e.g., the interaction between gender and SES) across several PISA cycles. All the datafiles and R scripts we used are available online. Because complex social, health, or economic survey and panel studies share many methodological features with ELSAs, the guidance offered in this tutorial is also helpful for synthesizing research evidence from these studies. KW - complex survey designs KW - educational large-scale assessments KW - individual KW - participant data KW - meta-analysis KW - Programme for International Student KW - Assessment Y1 - 2022 U6 - https://doi.org/10.1002/jrsm.1584 SN - 1759-2879 SN - 1759-2887 VL - 14 IS - 1 SP - 5 EP - 35 PB - Wiley CY - Hoboken ER - TY - JOUR A1 - Dudi, Reetika A1 - Dietrich, Tim A1 - Rashti, Alireza A1 - Brügmann, Bernd A1 - Steinhoff, Jan A1 - Tichy, Wolfgang T1 - High-accuracy simulations of highly spinning binary neutron star systems JF - Physical review : D, Particles, fields, gravitation, and cosmology N2 - With an increasing number of expected gravitational-wave detections of binary neutron star mergers, it is essential that gravitational-wave models employed for the analysis of observational data are able to describe generic compact binary systems. This includes systems in which the individual neutron stars are millisecond pulsars for which spin effects become essential. In this work, we perform numerical-relativity simulations of binary neutron stars with aligned and antialigned spins within a range of dimensionless spins of chi similar to [-0.28, 0.58]. The simulations are performed with multiple resolutions, show a clear convergence order and, consequently, can be used to test existing waveform approximants. We find that for very high spins gravitational-wave models that have been employed for the interpretation of GW170817 and GW190425 arc not capable of describing our numerical-relativity dataset. We verify through a full parameter estimation study in which clear biases in the estimate of the tidal deformability and effective spin are present. We hope that in preparation of the next gravitational-wave observing run of the Advanced LIGO and Advanced Virgo detectors our new set of numerical-relativity data can be used to support future developments of new gravitational-wave models. Y1 - 2022 U6 - https://doi.org/10.1103/PhysRevD.105.064050 SN - 2470-0010 SN - 2470-0029 VL - 105 IS - 6 PB - American Physical Society CY - College Park ER -