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 -