@article{CsehFaenzaKavithaetal.2022, author = {Cseh, Agnes and Faenza, Yuri and Kavitha, Telikepalli and Powers, Vladlena}, title = {Understanding popular matchings via stable matchings}, series = {SIAM journal on discrete mathematics}, volume = {36}, journal = {SIAM journal on discrete mathematics}, number = {1}, publisher = {Society for Industrial and Applied Mathematics}, address = {Philadelphia}, issn = {0895-4801}, doi = {10.1137/19M124770X}, pages = {188 -- 213}, year = {2022}, abstract = {An instance of the marriage problem is given by a graph G = (A boolean OR B, E), together with, for each vertex of G, a strict preference order over its neighbors. A matching M of G is popular in the marriage instance if M does not lose a head-to-head election against any matching where vertices are voters. Every stable matching is a min-size popular matching; another subclass of popular matchings that always exists and can be easily computed is the set of dominant matchings. A popular matching M is dominant if M wins the head-to-head election against any larger matching. Thus, every dominant matching is a max-size popular matching, and it is known that the set of dominant matchings is the linear image of the set of stable matchings in an auxiliary graph. Results from the literature seem to suggest that stable and dominant matchings behave, from a complexity theory point of view, in a very similar manner within the class of popular matchings. The goal of this paper is to show that there are instead differences in the tractability of stable and dominant matchings and to investigate further their importance for popular matchings. First, we show that it is easy to check if all popular matchings are also stable; however, it is co-NP hard to check if all popular matchings are also dominant. Second, we show how some new and recent hardness results on popular matching problems can be deduced from the NP-hardness of certain problems on stable matchings, also studied in this paper, thus showing that stable matchings can be employed to show not only positive results on popular matchings (as is known) but also most negative ones. Problems for which we show new hardness results include finding a min-size (resp., max-size) popular matching that is not stable (resp., dominant). A known result for which we give a new and simple proof is the NP-hardness of finding a popular matching when G is nonbipartite.}, language = {en} } @article{PanchalKojdaSahooetal.2022, author = {Panchal, Gyanendra and Kojda, Sandrino Danny and Sahoo, Sophia and Bagri, Anita and Kunwar, Hemant Singh and Bocklage, Lars and Panchwanee, Anjali and Sathe, Vasant G. and Fritsch, Katharina and Habicht, Klaus and Choudhary, Ram Janay and Phase, Deodutta M.}, title = {Strain and electric field control of magnetic and electrical transport properties in a magnetoelastically coupled Fe3O4/BaTiO3 (001) heterostructure}, series = {Physical review : B, Condensed matter and materials physics}, volume = {105}, journal = {Physical review : B, Condensed matter and materials physics}, number = {22}, publisher = {The American Institute of Physics}, address = {Woodbury, NY}, issn = {2469-9950}, doi = {10.1103/PhysRevB.105.224419}, pages = {8}, year = {2022}, abstract = {We present a study of the control of electric field induced strain on the magnetic and electrical transport properties in a magnetoelastically coupled artificial multiferroic Fe3O4/BaTiO3 heterostructure. In this Fe3O4/BaTiO3 heterostructure, the Fe3O4 thin film is epitaxially grown in the form of bilateral domains, analogous to a-c stripe domains of the underlying BaTiO3(001) substrate. By in situ electric field dependent magnetization measurements, we demonstrate the extrinsic control of the magnetic anisotropy and the characteristic Verwey metal-insulator transition of the epitaxial Fe3O4 thin film in a wide temperature range between 20-300 K, via strain mediated converse magnetoelectric coupling. In addition, we observe strain induced modulations in the magnetic and electrical transport properties of the Fe3O4 thin film across the thermally driven intrinsic ferroelectric and structural phase transitions of the BaTiO3 substrate. In situ electric field dependent Raman measurements reveal that the electric field does not significantly modify the antiphase boundary defects in the Fe3O4 thin film once it is thermodynamically stable after deposition and that the modification of the magnetic properties is mainly caused by strain induced lattice distortions and magnetic anisotropy. These results provide a framework to realize electrical control of the magnetization in a classical highly correlated transition metal oxide.}, language = {en} } @article{HannemannEulenfeldKruegeretal.2021, author = {Hannemann, Katrin and Eulenfeld, Tom and Kr{\"u}ger, Frank and Dahm, Torsten}, title = {Seismic scattering and absorption of oceanic lithospheric S waves in the Eastern North Atlantic}, series = {Geophysical journal international}, volume = {229}, journal = {Geophysical journal international}, number = {2}, publisher = {Oxford Univ. Press}, address = {Oxford}, issn = {0956-540X}, doi = {10.1093/gji/ggab493}, pages = {948 -- 961}, year = {2021}, abstract = {The scattering and absorption of high-frequency seismic waves in the oceanic lithosphere is to date only poorly constrained by observations. Such estimates would not only improve our understanding of the propagation of seismic waves, but also unravel the small-scale nature of the lithosphere and its variability. Our study benefits from two exceptional situations: (1) we deployed over 10 months a mid-aperture seismological array in the central part of the Eastern North Atlantic in 5 km water depth and (2) we could observe in total 340 high-frequency (up to 30 Hz) Po and So arrivals with tens to hundreds of seconds long seismic coda from local and regional earthquakes in a wide range of backazimuths and epicentral distances up to 850 km with a travel path in the oceanic lithosphere. Moreover, the array was located about 100 km north of the Gloria fault, defining the plate boundary between the Eurasian and African plates at this location which also allows an investigation of the influence of an abrupt change in lithospheric age (20 Ma in this case) on seismic waves. The waves travel with velocities indicating upper-mantle material. We use So waves and their coda of pre-selected earthquakes to estimate frequency-dependent seismic scattering and intrinsic attenuation parameters. The estimated scattering attenuation coefficients are between 10(-4) and 4 x 10(-5) m(-1) and are typical for the lithosphere or the upper mantle. Furthermore, the total quality factors for So waves below 5 Hz are between 20 and 500 and are well below estimates from previous modelling for observations in the Pacific Ocean. This implies that the Atlantic Ocean is more attenuative for So waves compared to the Pacific Ocean, which is inline with the expected behaviour for the lithospheric structures resulting from the slower spreading rates in the Atlantic Ocean. The results for the analysed events indicate that for frequencies above 3 Hz, intrinsic attenuation is equal to or slightly stronger than scattering attenuation and that the So-wave coda is weakly influenced by the oceanic crust. Both observations are in agreement with the proposed propagation mechanism of scattering in the oceanic mantle lithosphere. Furthermore, we observe an age dependence which shows that an increase in lithospheric age is associated with a decrease in attenuation. However, we also observe a trade-off of this age-dependent effect with either a change in lithospheric thickness or thermal variations, for example due to small-scale upwellings in the upper mantle in the southeast close to Madeira and the Canaries. Moreover, the influence of the nearby Gloria fault is visible in a reduction of the intrinsic attenuation below 3 Hz for estimates across the fault. This is the first study to estimate seismic scattering and absorption parameters of So waves for an area with several hundreds of kilometres radius centred in the Eastern North Atlantic and using them to characterize the nature of the oceanic lithosphere.}, language = {en} } @article{BenNsirJomaaYildirimetal.2022, author = {Ben Nsir, Siwar and Jomaa, Seifeddine and Yildirim, Umit and Zhou, Xiangqian and D'Oria, Marco and Rode, Michael and Khlifi, Slaheddine}, title = {Assessment of climate change impact on discharge of the lakhmass catchment (Northwest Tunisia)}, series = {Water}, volume = {14}, journal = {Water}, number = {14}, publisher = {MDPI}, address = {Basel}, issn = {2073-4441}, doi = {10.3390/w14142242}, pages = {17}, year = {2022}, abstract = {The Mediterranean region is increasingly recognized as a climate change hotspot but is highly underrepresented in hydrological climate change studies. This study aims to investigate the climate change effects on the hydrology of Lakhmass catchment in Tunisia. Lakhmass catchment is a part of the Medium Valley of Medjerda in northwestern Tunisia that drains an area of 126 km(2). First, the Hydrologiska Byrans Vattenbalansavdelning light (HBV-light) model was calibrated and validated successfully at a daily time step to simulate discharge during the 1981-1986 period. The Nash Sutcliffe Efficiency and Percent bias (NSE, PBIAS) were (0.80, +2.0\%) and (0.53, -9.5\%) for calibration (September 1982-August 1984) and validation (September 1984-August 1986) periods, respectively. Second, HBV-light model was considered as a predictive tool to simulate discharge in a baseline period (1981-2009) and future projections using data (precipitation and temperature) from thirteen combinations of General Circulation Models (GCMs) and Regional Climatic Models (RCMs). We used two trajectories of Representative Concentration Pathways, RCP4.5 and RCP8.5, suggested by the Intergovernmental Panel on Climate Change (IPCC). Each RCP is divided into three projection periods: near-term (2010-2039), mid-term (2040-2069) and long-term (2070-2099). For both scenarios, a decrease in precipitation and discharge will be expected with an increase in air temperature and a reduction in precipitation with almost 5\% for every +1 degrees C of global warming. By long-term (2070-2099) projection period, results suggested an increase in temperature with about 2.7 degrees C and 4 degrees C, and a decrease in precipitation of approximately 7.5\% and 15\% under RCP4.5 and RCP8.5, respectively. This will likely result in a reduction of discharge of 12.5\% and 36.6\% under RCP4.5 and RCP8.5, respectively. This situation calls for early climate change adaptation measures under a participatory approach, including multiple stakeholders and water users.}, language = {en} } @article{McCoolCoddingVernonetal.2022, author = {McCool, Weston C. and Codding, Brian F. and Vernon, Kenneth B. and Wilson, Kurt M. and Yaworsky, Peter M. and Marwan, Norbert and Kennett, Douglas J.}, title = {Climate change-induced population pressure drives high rates of lethal violence in the Prehispanic central Andes}, series = {Proceedings of the National Academy of Sciences of the United States of America : PNAS}, volume = {119}, journal = {Proceedings of the National Academy of Sciences of the United States of America : PNAS}, number = {17}, publisher = {National Acad. of Sciences}, address = {Washington}, issn = {0027-8424}, doi = {10.1073/pnas.2117556119}, pages = {8}, year = {2022}, abstract = {Understanding the influence of climate change and population pressure on human conflict remains a critically important topic in the social sciences. Long-term records that evaluate these dynamics across multiple centuries and outside the range of modern climatic variation are especially capable of elucidating the relative effect of-and the interaction between-climate and demography. This is crucial given that climate change may structure population growth and carrying capacity, while both climate and population influence per capita resource availability. This study couples paleoclimatic and demographic data with osteological evaluations of lethal trauma from 149 directly accelerator mass spectrometry C-14-dated individuals from the Nasca highland region of Peru. Multiple local and supraregional precipitation proxies are combined with a summed probability distribution of 149 C-14 dates to estimate population dynamics during a 700-y study window. Counter to previous findings, our analysis reveals a precipitous increase in violent deaths associated with a period of productive and stable climate, but volatile population dynamics. We conclude that favorable local climate conditions fostered population growth that put pressure on the marginal and highly circumscribed resource base, resulting in violent resource competition that manifested in over 450 y of internecine warfare. These findings help support a general theory of intergroup violence, indicating that relative resource scarcity-whether driven by reduced resource abundance or increased competition-can lead to violence in subsistence societies when the outcome is lower per capita resource availability.}, language = {en} } @article{OhlertBoos2020, author = {Ohlert, Clemens and Boos, Pauline}, title = {Auswirkungen der Digitalisierung auf Geschlechterungleichheiten}, series = {Arbeit}, volume = {29}, journal = {Arbeit}, number = {3-4}, publisher = {De Gruyter Oldenbourg}, address = {Berlin}, issn = {0941-5025}, doi = {10.1515/arbeit-2020-0015}, pages = {195 -- 218}, year = {2020}, abstract = {Ausgehend von der Debatte um die Genderaspekte der Digitalisierung der Arbeit untersuchen wir den Zusammenhang zwischen der Nutzung digitaler Technologien und der Entwicklung von Geschlechterungleichheiten empirisch. Die Ergebnisse zeigen, dass Frauen in Branchen mit hohem Digitalisierungsgrad unterrepr{\"a}sentiert sind und dass sich diese Dimension der Geschlechtersegregation in den letzten Jahren verst{\"a}rkte. Die Unterrepr{\"a}sentation von Frauen in Branchen mit hohem Digitalisierungsgrad geht mit Nachteilen bei den Verdiensten einher. Die Ergebnisse zeigen zudem, dass der Gender Pay Gap in Branchen mit hohem Digitalisierungsgrad tendenziell gr{\"o}ßer ist und {\"u}ber die Zeit weniger zur{\"u}ckging als in Branchen, in denen weniger digitale Technologien genutzt werden.}, language = {de} } @incollection{BoosGeckilMuster2023, author = {Boos, Pauline and Geckil, Celine and Muster, Judith}, title = {Schneller, weiter, besser?}, series = {Die Digitalisierung des Politischen}, booktitle = {Die Digitalisierung des Politischen}, editor = {Wagener, Andreas and Stark, Carsten}, publisher = {Springer VS}, address = {Wiesbaden}, isbn = {978-3-658-38267-4}, doi = {10.1007/978-3-658-38268-1_6}, pages = {119 -- 140}, year = {2023}, abstract = {Der Beitrag nimmt die Kritik an der verz{\"o}gerten Umsetzung des Onlinezugangsgesetzes (OZG) zum Anlass, um die Digitalisierung der Verwaltung organisationssoziologisch zu diskutieren. Die verfolgte These ist, dass die Verz{\"o}gerungen der Umsetzung von Digitalisierungsprojekten ihren Ursprung im Umgang der Verwaltung mit einem Spannungsfeld haben: W{\"a}hrend politisch versucht wird, sich mithilfe einer Digitalisierung der Verfahren als bessere, schnellere und effizientere Verwaltung zu legitimieren, erzeugt eben diese Digitalisierung Probleme f{\"u}r die Legitimationsmechanismen der Verwaltung. Grundlegend f{\"u}r diese These ist die Figur der Legitimation durch Verfahren von Niklas Luhmann. Der Beitrag greift dementsprechend aktuelle Literatur zum Themengebiet auf, kategorisiert die gefundenen Erkenntnisse in zwei Problemfelder - Operationalisierungs- und Darstellungsprobleme - und begr{\"u}ndet das Entstehen dieser Problemfelder mithilfe der Theorie sozialer Systeme. Diese begreift Verfahren als Handlungssysteme, die einen zentralen Stellenwert f{\"u}r die Legitimation der Verwaltungsorganisationen haben. Zuletzt wird diskutiert ob und wie die Erkenntnisse aus der theoretischen Diskussion f{\"u}r die Praxis fruchtbar gemacht werden k{\"o}nnen.}, language = {de} } @article{Lettl2024, author = {Lettl, Tobias}, title = {Rechtsfolgen der Missbr{\"a}uchlichkeit einer Vertragsklausel nach Art. 6 Abs. 1 RL 93/13/EWG (Klausel-RL) und Art. 13 Abs. 1, 7 VO (EU) 2023/2854 (Datenverordnung oder Data-Act)}, series = {Wertpapier-Mitteilungen Teil 4, Zeitschrift f{\"u}r Wirtschafts- und Bankrecht}, volume = {78}, journal = {Wertpapier-Mitteilungen Teil 4, Zeitschrift f{\"u}r Wirtschafts- und Bankrecht}, number = {5}, publisher = {Herausgebergemeinschaft Wertpapiermitteilungen Keppler, Lehmann}, address = {Frankfurt am Main}, issn = {0342-6971}, pages = {185 -- 192}, year = {2024}, language = {de} } @article{Mitsch2023, author = {Mitsch, Wolfgang}, title = {Die „Vorpr{\"u}fung" beim Versuch in der Fallbearbeitung}, series = {Zeitschrift f{\"u}r das juristische Studium}, journal = {Zeitschrift f{\"u}r das juristische Studium}, number = {4}, publisher = {T. Rotsch}, address = {Gießen}, issn = {1865-6331}, pages = {729 -- 736}, year = {2023}, abstract = {Der Beitrag behandelt eine Marginalie der strafrechtlichen Fallbearbeitung, die "Vorpr{\"u}fung" bei der Er{\"o}rterung von Versuchsstrafbarkeit. Fehler sind hier selten, kommen aber in der Universit{\"a}ts- und Examensrealit{\"a}t vor. Zu ihrer Vermeidung gibt der vorliegende Beitrag einige Ratschl{\"a}ge und Hinweise.}, language = {de} } @article{YuanJiaoDupontNivetetal.2022, author = {Yuan, Xiaoping P. and Jiao, Ruohong and Dupont-Nivet, Guillaume and Shen, Xiaoming}, title = {Southeastern Tibetan Plateau growth revealed by inverse analysis of landscape evolution model}, series = {Geophysical research letters}, volume = {49}, journal = {Geophysical research letters}, number = {10}, publisher = {American Geophysical Union}, address = {Washington}, issn = {0094-8276}, doi = {10.1029/2021GL097623}, pages = {10}, year = {2022}, abstract = {The Cenozoic history of the Tibetan Plateau topography is critical for understanding the evolution of the Indian-Eurasian collision, climate, and biodiversity. However, the long-term growth and landscape evolution of the Tibetan Plateau remain ambiguous, it remains unclear if plateau uplift occurred soon after the India-Asia collision in the Paleogene (similar to 50-25 Ma) or later in the Neogene (similar to 20-5 Ma). Here, we reproduce the uplift history of the southeastern Tibetan Plateau using a 2D landscape evolution model, which simultaneously solves fluvial erosion and sediment transport processes in the drainage basins of the Three Rivers region (Yangtze, Mekong, and Salween Rivers). Our model was optimized through a formal inverse analysis with 20,000 forward simulations, which aims to reconcile the transient states of the present-day river profiles. The results, compared to existing paleoelevation and thermochronologic data, suggest initially low elevations (similar to 300-500 m) during the Paleogene, followed by a gradual southeastward propagation of topographic uplift of the plateau margin.}, language = {en} }