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Videos related to the maps
(2012)
Governments at central and sub-national levels are increasingly pursuing participatory mechanisms in a bid to improve governance and service delivery. This has been largely in the context of decentralization reforms in which central governments transfer (share) political, administrative, fiscal and economic powers and functions to sub-national units. Despite the great international support and advocacy for participatory governance where citizen’s voice plays a key role in decision making of decentralized service delivery, there is a notable dearth of empirical evidence as to the effect of such participation. This is the question this study sought to answer based on a case study of direct citizen participation in Local Authorities (LAs) in Kenya. This is as formally provided for by the Local Authority Service Delivery Action Plan (LASDAP) framework that was established to ensure citizens play a central role in planning and budgeting, implementation and monitoring of locally identified services towards improving livelihoods and reducing poverty. Influence of participation was assessed in terms of how it affected five key determinants of effective service delivery namely: efficient allocation of resources; equity in service delivery; accountability and reduction of corruption; quality of services; and, cost recovery. It finds that the participation of citizens is minimal and the resulting influence on the decentralized service delivery negligible. It concludes that despite the dismal performance of citizen participation, LASDAP has played a key role towards institutionalizing citizen participation that future structures will build on. It recommends that an effective framework of citizen participation should be one that is not directly linked to politicians; one that is founded on a legal framework and where citizens have a legal recourse opportunity; and, one that obliges LA officials both to implement what citizen’s proposals which meet the set criteria as well as to account for their actions in the management of public resources.
The Sun is surrounded by a 10^6 K hot atmosphere, the corona. The corona and the solar wind are fully ionized, and therefore in the plasma state. Magnetic fields play an important role in a plasma, since they bind electrically charged particles to their field lines. EUV spectroscopes, like the SUMER instrument on-board the SOHO spacecraft, reveal a preferred heating of coronal ions and strong temperature anisotropies. Velocity distributions of electrons can be measured directly in the solar wind, e.g. with the 3DPlasma instrument on-board the WIND satellite. They show a thermal core, an anisotropic suprathermal halo, and an anti-solar, magnetic-field-aligned, beam or "strahl". For an understanding of the physical processes in the corona, an adequate description of the plasma is needed. Magnetohydrodynamics (MHD) treats the plasma simply as an electrically conductive fluid. Multi-fluid models consider e.g. protons and electrons as separate fluids. They enable a description of many macroscopic plasma processes. However, fluid models are based on the assumption of a plasma near thermodynamic equilibrium. But the solar corona is far away from this. Furthermore, fluid models cannot describe processes like the interaction with electromagnetic waves on a microscopic scale. Kinetic models, which are based on particle velocity distributions, do not show these limitations, and are therefore well-suited for an explanation of the observations listed above. For the simplest kinetic models, the mirror force in the interplanetary magnetic field focuses solar wind electrons into an extremely narrow beam, which is contradicted by observations. Therefore, a scattering mechanism must exist that counteracts the mirror force. In this thesis, a kinetic model for electrons in the solar corona and wind is presented that provides electron scattering by resonant interaction with whistler waves. The kinetic model reproduces the observed components of solar wind electron distributions, i.e. core, halo, and a "strahl" with finite width. But the model is not only applicable on the quiet Sun. The propagation of energetic electrons from a solar flare is studied, and it is found that scattering in the direction of propagation and energy diffusion influence the arrival times of flare electrons at Earth approximately to the same degree. In the corona, the interaction of electrons with whistler waves does not only lead to scattering, but also to the formation of a suprathermal halo, as it is observed in interplanetary space. This effect is studied both for the solar wind as well as the closed volume of a coronal magnetic loop. The result is of fundamental importance for solar-stellar relations. The quiet solar corona always produces suprathermal electrons. This process is closely related to coronal heating, and can therefore be expected in any hot stellar corona. In the second part of this thesis it is detailed how to calculate growth or damping rates of plasma waves from electron velocity distributions. The emission and propagation of electron cyclotron waves in the quiet solar corona, and that of whistler waves during solar flares, is studied. The latter can be observed as so-called fiber bursts in dynamic radio spectra, and the results are in good agreement with observed bursts.
Aufstiege aus der Mittelschicht : soziale Aufstiegsmobilität von Haushalten zwischen 1984 und 2010
(2012)
Die Dissertation widmet sich den intragenerationalen Aufstiegsprozessen von Haushalten aus der Mittelschicht zu den Wohlhabenden. Intragenerationale Mobilitätsforschung wird bislang vor allem als arbeitsmarktbezogene Inidivualmobilität angesehen. Diese Dissertation erweitert den Ansatz auf die Ebene des Haushaltes. Dem liegt der Gedanke zugrunde, dass die soziale Position eines Individuums nicht allein durch sein Erwerbseinkommen determiniert wird. Ebenso entscheidend ist der Kontext des Haushaltes. Dieser bestimmt darüber, wie viele Personen zum Einkommen beitragen können und wie viele daran partizipieren. Weiterhin kommt der Haushaltsebene in Paar-Haushalten die Rolle des Aushandlungsortes zu. Hier wird über Familienplanung, Kinderwunsch und damit in Zusammenhang stehend auch über die Erwerbsbeteiligung der Partner entscheiden. Die vorliegende Dissertation untersucht diese Annahmen mithilfe von Daten des Sozioökonomischen Panels (SOEP) der Jahre 1984 bis 2010. Der Fokus liegt auf der Erwerbsbeteiligung und dem Bildungsniveau des Haushaltes, seiner Struktur, sowie dem Beruf des Haushaltsvorstandes. Es wird davon ausgegangen, dass dies die Hauptfaktoren sind, die über die finanziellen Möglichkeiten eines Haushaltes entscheiden. Ein weiterer Schwerpunkt der Arbeit liegt in der Berücksichtigung des historischen Kontextes, da anzunehmen ist, dass die oben benannten Faktoren sich und ihren Einfluss auf die Aufstiegsmöglichkeiten von Haushalten im historischen Verlauf verändert haben.
Climate is the principal driving force of hydrological extremes like floods and attributing generating mechanisms is an essential prerequisite for understanding past, present, and future flood variability. Successively enhanced radiative forcing under global warming enhances atmospheric water-holding capacity and is expected to increase the likelihood of strong floods. In addition, natural climate variability affects the frequency and magnitude of these events on annual to millennial time-scales. Particularly in the mid-latitudes of the Northern Hemisphere, correlations between meteorological variables and hydrological indices suggest significant effects of changing climate boundary conditions on floods. To date, however, understanding of flood responses to changing climate boundary conditions is limited due to the scarcity of hydrological data in space and time. Exploring paleoclimate archives like annually laminated (varved) lake sediments allows to fill this gap in knowledge offering precise dated time-series of flood variability for millennia. During river floods, detrital catchment material is eroded and transported in suspension by fluid turbulence into downstream lakes. In the water body the transport capacity of the inflowing turbidity current successively diminishes leading to the deposition of detrital layers on the lake floor. Intercalated into annual laminations these detrital layers can be dated down to seasonal resolution. Microfacies analyses and X-ray fluorescence scanning (µ-XRF) at 200 µm resolution were conducted on the varved Mid- to Late Holocene interval of two sediment profiles from pre-alpine Lake Ammersee (southern Germany) located in a proximal (AS10prox) and distal (AS10dist) position towards the main tributary River Ammer. To shed light on sediment distribution within the lake, particular emphasis was (1) the detection of intercalated detrital layers and their micro-sedimentological features, and (2) intra-basin correlation of these deposits. Detrital layers were dated down to the season by microscopic varve counting and determination of the microstratigraphic position within a varve. The resulting chronology is verified by accelerator mass spectrometry (AMS) 14C dating of 14 terrestrial plant macrofossils. Since ~5500 varve years before present (vyr BP), in total 1573 detrital layers were detected in either one or both of the investigated sediment profiles. Based on their microfacies, geochemistry, and proximal-distal deposition pattern, detrital layers were interpreted as River Ammer flood deposits. Calibration of the flood layer record using instrumental daily River Ammer runoff data from AD 1926 to 1999 proves the flood layer succession to represent a significant time-series of major River Ammer floods in spring and summer, the flood season in the Ammersee region. Flood layer frequency trends are in agreement with decadal variations of the East Atlantic-Western Russia (EA-WR) atmospheric pattern back to 200 yr BP (end of the used atmospheric data) and solar activity back to 5500 vyr BP. Enhanced flood frequency corresponds to the negative EA-WR phase and reduced solar activity. These common links point to a central role of varying large-scale atmospheric circulation over Europe for flood frequency in the Ammersee region and suggest that these atmospheric variations, in turn, are likely modified by solar variability during the past 5500 years. Furthermore, the flood layer record indicates three shifts in mean layer thickness and frequency of different manifestation in both sediment profiles at ~5500, ~2800, and ~500 vyr BP. Combining information from both sediment profiles enabled to interpret these shifts in terms of stepwise increases in mean flood intensity. Likely triggers of these shifts are gradual reduction of Northern Hemisphere orbital summer forcing and long-term solar activity minima. Hypothesized atmospheric response to this forcing is hemispheric cooling that enhances equator-to-pole temperature gradients and potential energy in the troposphere. This energy is transferred into stronger westerly cyclones, more extreme precipitation, and intensified floods at Lake Ammersee. Interpretation of flood layer frequency and thickness data in combination with reanalysis models and time-series analysis allowed to reconstruct the flood history and to decipher flood triggering climate mechanisms in the Ammersee region throughout the past 5500 years. Flood frequency and intensity are not stationary, but influenced by multi-causal climate forcing of large-scale atmospheric modes on time-scales from years to millennia. These results challenge future projections that propose an increase in floods when Earth warms based only on the assumption of an enhanced hydrological cycle.
A discrete analogue of the Witten Laplacian on the n-dimensional integer lattice is considered. After rescaling of the operator and the lattice size we analyze the tunnel effect between different wells, providing sharp asymptotics of the low-lying spectrum. Our proof, inspired by work of B. Helffer, M. Klein and F. Nier in continuous setting, is based on the construction of a discrete Witten complex and a semiclassical analysis of the corresponding discrete Witten Laplacian on 1-forms. The result can be reformulated in terms of metastable Markov processes on the lattice.
Sustainable management of semi-arid African savannas under environmental and political change
(2012)
Drylands cover about 40% of the earth’s land surface and provide the basis for the livelihoods of 38% of the global human population. Worldwide, these ecosystems are prone to heavy degradation. Increasing levels of dryland degradation result a strong decline of ecosystem services. In addition, in highly variable semi-arid environments changing future environmental conditions will potentially have severe consequences for productivity and ecosystem dynamics. Hence, global efforts have to be made to understand the particular causes and consequences of dryland degradation and to promote sustainable management options for semi-arid and arid ecosystems in a changing world. Here I particularly address the problem of semi-arid savanna degradation, which mostly occurs in form of woody plant encroachment. At this, I aim at finding viable sustainable management strategies and improving the general understanding of semi-arid savanna vegetation dynamics under conditions of extensive livestock production. Moreover, the influence of external forces, i.e. environmental change and land reform, on the use of savanna vegetation and on the ecosystem response to this land use is assessed. Based on this I identify conditions and strategies that facilitate a sustainable use of semi-arid savanna rangelands in a changing world. I extended an eco-hydrological model to simulate rangeland vegetation dynamics for a typical semi-arid savanna in eastern Namibia. In particular, I identified the response of semi-arid savanna vegetation to different land use strategies (including fire management) also with regard to different predicted precipitation, temperature and CO2 regimes. Not only environmental but also economic and political constraints like e.g. land reform programmes are shaping rangeland management strategies. Hence, I aimed at understanding the effects of the ongoing process of land reform in southern Africa on land use and the semi-arid savanna vegetation. Therefore, I developed and implemented an agent-based ecological-economic modelling tool for interactive role plays with land users. This tool was applied in an interdisciplinary empirical study to identify general patterns of management decisions and the between-farm cooperation of land reform beneficiaries in eastern Namibia. The eco-hydrological simulations revealed that the future dynamics of semi-arid savanna vegetation strongly depend on the respective climate change scenario. In particular, I found that the capacity of the system to sustain domestic livestock production will strongly depend on changes in the amount and temporal distribution of precipitation. In addition, my simulations revealed that shrub encroachment will become less likely under future climatic conditions although positive effects of CO2 on woody plant growth and transpiration have been considered. While earlier studies predicted a further increase in shrub encroachment due to increased levels of atmospheric CO2, my contrary finding is based on the negative impacts of temperature increase on the drought sensitive seedling germination and establishment of woody plant species. Further simulation experiments revealed that prescribed fires are an efficient tool for semi-arid rangeland management, since they suppress woody plant seedling establishment. The strategies tested have increased the long term productivity of the savanna in terms of livestock production and decreased the risk for shrub encroachment (i.e. savanna degradation). This finding refutes the views promoted by existing studies, which state that fires are of minor importance for the vegetation dynamics of semi-arid and arid savannas. Again, the difference in predictions is related to the bottleneck at the seedling establishment stage of woody plants, which has not been sufficiently considered in earlier studies. The ecological-economic role plays with Namibian land reform beneficiaries showed that the farmers made their decisions with regard to herd size adjustments according to economic but not according to environmental variables. Hence, they do not manage opportunistically by tracking grass biomass availability but rather apply conservative management strategies with low stocking rates. This implies that under the given circumstances the management of these farmers will not per se cause (or further worsen) the problem of savanna degradation and shrub encroachment due to overgrazing. However, as my results indicate that this management strategy is rather based on high financial pressure, it is not an indicator for successful rangeland management. Rather, farmers struggle hard to make any positive revenue from their farming business and the success of the Namibian land reform is currently disputable. The role-plays also revealed that cooperation between farmers is difficult even though obligatory due to the often small farm sizes. I thus propose that cooperation needs to be facilitated to improve the success of land reform beneficiaries.
The Indian summer monsoon (ISM) is one of the largest climate systems on earth and impacts the livelihood of nearly 40% of the world’s population. Despite dedicated efforts, a comprehensive picture of monsoon variability has proved elusive largely due to the absence of long term high resolution records, spatial inhomogeneity of the monsoon precipitation, and the complex forcing mechanisms (solar insolation, internal teleconnections for e.g., El Niño-Southern Oscillation, tropical-midlatitude interactions). My work aims to improve the understanding of monsoon variability through generation of long term high resolution palaeoclimate data from climatically sensitive regions in the ISM and westerlies domain. To achieve this aim I have (i) identified proxies (sedimentological, geochemical, isotopic, and mineralogical) that are sensitive to environmental changes; (ii) used the identified proxies to generate long term palaeoclimate data from two climatically sensitive regions, one in NW Himalayas (transitional westerlies and ISM domain in the Spiti valley and one in the core monsoon zone (Lonar lake) in central India); (iii) undertaken a regional overview to generate “snapshots” of selected time slices; and (iv) interpreted the spatial precipitation anomalies in terms of those caused by modern teleconnections. This approach must be considered only as the first step towards identifying the past teleconnections as the boundary conditions in the past were significantly different from today and would have impacted the precipitation anomalies. As the Spiti valley is located in the in the active tectonic orogen of Himalayas, it was essential to understand the role of regional tectonics to make valid interpretations of catchment erosion and detrital influx into the lake. My approach of using integrated structural/morphometric and geomorphic signatures provided clear evidence for active tectonics in this area and demonstrated the suitability of these lacustrine sediments as palaleoseismic archives. The investigations on the lacustrine outcrops in Spiti valley also provided information on changes in seasonality of precipitation and occurrence of frequent and intense periods (ca. 6.8-6.1 cal ka BP) of detrital influx indicating extreme hydrological events in the past. Regional comparison for this time slice indicates a possible extended “break-monsoon like” mode for the monsoon that favors enhanced precipitation over the Tibetan plateau, Himalayas and their foothills. My studies on surface sediments from Lonar lake helped to identify environmentally sensitive proxies which could also be used to interpret palaeodata obtained from a ca. 10m long core raised from the lake in 2008. The core encompasses the entire Holocene and is the first well dated (by 14C) archive from the core monsoon zone of central India. My identification of authigenic evaporite gaylussite crystals within the core sediments provided evidence of exceptionally drier conditions during 4.7-3.9 and 2.0-0.5 cal ka BP. Additionally, isotopic investigations on these crystals provided information on eutrophication, stratification, and carbon cycling processes in the lake.
Die Entwicklung neuer Verfahren für die Rückführung von Palladium aus Altmaterialien, wie gebrauchten Autoabgaskatalysatoren, in den Stoffstromkreislauf ist sowohl aus ökologischer als auch ökonomischer Sicht erstrebenswert. In dieser Arbeit wurden neue Flüssig-Flüssig- und Fest-Flüssig-Extraktionsmittel entwickelt, mit denen Palladium(II) aus einer oxidierenden, salzsauren Laugungslösung, die neben Palladium auch Platin und Rhodium sowie zahlreiche unedle Metalle enthält, zurückgewonnen werden kann. Die neuen Extraktionsmittel ungesättigte monomere 1,2-Dithioether und oligomere Ligandenmischungen mit vicinalen Dithioether-Einheiten – sind im Gegensatz zu vielen in der Literatur aufgeführten Extraktionsmitteln hochselektiv. Aufgrund ihrer geometrischen und elektronischen Präorganisation bilden sie mit Palladium(II) stabile quadratisch-planare Chelatkomplexe. Für die Entwicklung des Flüssig-Flüssig-Extraktionsmittels wurde eine Reihe von ungesättigten 1,2-Dithioetherliganden dargestellt, welche auf einer starren 1,2-Dithioethen-Einheit, die in ein variierendes elektronenziehendes Grundgerüst eingebettet ist, basieren und polare Seitenketten besitzen. Neben der Bestimmung der Kristallstrukturen der Liganden und ihrer Palladiumdichlorid-Komplexe wurden die elektro- und photochemischen Eigenschaften, die Komplexstabilität und das Verhalten in Lösung untersucht. In Flüssig-Flüssig-Extraktionsuntersuchungen konnte gezeigt werden, dass einige der neuen Liganden industriell genutzten Extraktionsmitteln durch eine schnellere Einstellung des Extraktionsgleichgewichts überlegen sind. Anhand von Kriterien, die für eine industrielle Nutzbarkeit entscheidend sind, wie: guter Oxidationsbeständigkeit, einer hohen Extraktionsausbeute (auch bei hohen Salzsäurekonzentrationen der Speiselösung), schneller Extraktionskinetik und einer hohen Selektivität für Palladium(II) wurde aus der Reihe der sechs Liganden ein geeignetes Flüssig-Flüssig-Extraktionsmittel ausgewählt: 1,2-Bis(2-methoxyethylthio)benzen. Mit diesem wurde ein praxisnahes Flüssig-Flüssig-Extraktionssystem entwickelt. Nach der schrittweisen Adaption der wässrigen Phase von einer Modelllösung hin zu der oxidierenden, salzsauren Laugungslösung erfolgte die Auswahl eines geeigneten großtechnisch, einsetzbaren Lösemittels (1,2-Dichlorbenzen) und eines effizienten Reextraktionsmittels (0,5 M Thioharnstoff in 0,1 M HCl). Die hohe Palladium(II)-Selektivität dieses Flüssig-Flüssig-Extraktionssystems konnte verifiziert und seine Wiederverwendbarkeit und Praxistauglichkeit unter Beweis gestellt werden. Weiterhin wurde gezeigt, dass sich beim Kontakt mit oxidierenden Medien aus dem Dithioether 1,2-Bis(2-methoxyethylthio)benzen geringe Mengen des Thioethersulfoxids 1-(2-Methoxyethylsulfinyl)-2-(2-methoxyethylthio)benzen bilden. Dieses wird im sauren Milieu protoniert und beschleunigt die Extraktion wie ein Phasentransferkatalysator, ohne jedoch die Palladium(II)-Selektivität herabzusetzen. Die Kristallstruktur des Palladiumdichlorid-Komplexes des Tioethersulfoxids zeigt, dass der unprotonierte Ligand Palladium(II), analog zum Dithioether, über die chelatisierenden Schwefelatome koordiniert. Verschiedene Mischungen von Oligo(dithioether)-Liganden und der monomere Ligand 1,2-Bis(2-methoxyethylthio)benzen dienten als Extraktionsmittel für Fest-Flüssig-Extraktionsversuche mit SIRs (solvent impregnated resins) und wurden zu diesem Zweck auf hydrophilem Kieselgel und organophilem Amberlite® XAD 2 adsorbiert. Die Oligo(dithioether)-Liganden basieren auf 1,2-Dithiobenzen oder 1,2-Dithiomaleonitril-Einheiten, welche über Tris(oxyethylen)ethylen- oder Trimethylen-Brücken miteinander verknüpft sind. Mit Hilfe von Batch-Versuchen konnte gezeigt werden, dass sich strukturelle Unterschiede - wie die Art der chelatisierenden Einheit, die Art der verbrückenden Ketten und das Trägermaterial - auf die Extraktionsausbeuten, die Extraktionskinetik und die Beladungskapazität auswirken. Die kieselgelhaltigen SIRs stellen das Extraktionsgleichgewicht viel schneller ein als die Amberlite® XAD 2-haltigen. Jedoch bleiben die Extraktionsmittel auf Amberlite® XAD 2, im Gegensatz zu Kieselgel, dauerhaft haften. Im salzsauren Milieu sind die 1,2-Dithiobenzen-derivate besser als Extraktionsmittel geeignet als die 1,2-Dithiomaleonitrilderivate. In Säulenversuchen mit der oxidierenden, salzsauren Laugungslösung und wiederverwendbaren, mit 1,2-Dithiobenzenderivaten imprägnierten, Amberlite® XAD 2-haltigen SIRs zeigte sich, dass für die Realisierung hoher Beladungskapazitäten sehr geringe Pumpraten benötigt werden. Trotzdem konnte die gute Palladium(II)-Selektivität dieser Festphasenmaterialien demonstriert werden. Allerdings wurden in den Eluaten im Gegensatz zu den Eluaten, die aus Flüssig-Flüssig-Extraktion resultierten neben dem Palladium auch geringe Mengen an Platin, Aluminium, Eisen und Blei gefunden.