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- Afrika (17) (remove)
Afrika hat seinen berechtigten Platz auf der Weltbühne noch nicht gefunden. Ein wichtiger Grund dafür besteht darin, dass afrikanische Regierungen – im Gegensatz zu denen Chinas, Indiens, Brasiliens oder Indonesiens – nicht jene Maßnahmen ergriffen haben, die für das Entstehen eines Mittelstandes aus dem Gemenge von Millionen Armen wichtig sind.
Agriculture is one of the most important human activities providing food and more agricultural goods for seven billion people around the world and is of special importance in sub-Saharan Africa. The majority of people depends on the agricultural sector for their livelihoods and will suffer from negative climate change impacts on agriculture until the middle and end of the 21st century, even more if weak governments, economic crises or violent conflicts endanger the countries’ food security. The impact of temperature increases and changing precipitation patterns on agricultural vegetation motivated this thesis in the first place. Analyzing the potentials of reducing negative climate change impacts by adapting crop management to changing climate is a second objective of the thesis. As a precondition for simulating climate change impacts on agricultural crops with a global crop model first the timing of sowing in the tropics was improved and validated as this is an important factor determining the length and timing of the crops´ development phases, the occurrence of water stress and final crop yield. Crop yields are projected to decline in most regions which is evident from the results of this thesis, but the uncertainties that exist in climate projections and in the efficiency of adaptation options because of political, economical or institutional obstacles have to be considered. The effect of temperature increases and changing precipitation patterns on crop yields can be analyzed separately and varies in space across the continent. Southern Africa is clearly the region most susceptible to climate change, especially to precipitation changes. The Sahel north of 13° N and parts of Eastern Africa with short growing seasons below 120 days and limited wet season precipitation of less than 500 mm are also vulnerable to precipitation changes while in most other part of East and Central Africa, in contrast, the effect of temperature increase on crops overbalances the precipitation effect and is most pronounced in a band stretching from Angola to Ethiopia in the 2060s. The results of this thesis confirm the findings from previous studies on the magnitude of climate change impact on crops in sub-Saharan Africa but beyond that helps to understand the drivers of these changes and the potential of certain management strategies for adaptation in more detail. Crop yield changes depend on the initial growing conditions, on the magnitude of climate change, and on the crop, cropping system and adaptive capacity of African farmers which is only now evident from this comprehensive study for sub-Saharan Africa. Furthermore this study improves the representation of tropical cropping systems in a global crop model and considers the major food crops cultivated in sub-Saharan Africa and climate change impacts throughout the continent.
Kenia erlangt Anfang der 1960er seine Unabhängigkeit und wird in der Folge von den Präsidenten Kenyatta und später Moi autoritär regiert. Als Konsequenz des internationalen und nationalen Druckes werden 1991 wieder Mehrparteienwahlen zugelassen. Die Hoffnungen auf einen Trendwechsel werden zunächst aber nicht erfüllt. Präsident Moi bleibt bei den Wahlen 1992 und 1997 siegreich und versucht jeden möglichen Reformprozess aufzuhalten bzw. zu verlangsamen. Mit dem neu gewählten Präsidenten Kibaki entsteht 2002 die Hoffnung auf Veränderung. Aber als alter Wegbegleiter Mois erfüllt Kibaki nicht die internationalen und nationalen Erwartungen. Moi und Kibaki organisieren jeweils kontra-demokratische Eliten hinter sich und nutzen das mächtige Präsidentenamt, die stärkste Institution im politischen System Kenias, um den Status quo so lange wie möglich zu erhalten. Die Parteien werden weder durch die Regierung noch durch die Opposition zu starken Institutionen transformiert und das unstete Verhalten der Geberländer vermag den Einfluss der autoritären Führung nicht dauerhaft einzuschränken.
This diploma thesis deals with the process of political and administrative decentralisation in the Kingdom of Lesotho. Although decentralization in itself does not automatically lead to development it became an integral part of reform processes in many developing countries. Governments and international donors consider efficient decentralized political and administrative structures as essential elements of “good governance” and a prerequisite for structural poverty alleviation. This paper seeks to analyse how the given decentralization strategy and its implementation is affecting different features of good governance in the case of Lesotho. The results of the analysis confirm that the decentralisation process significantly improved political participation of the local population. However, the second objective of enhancing efficiency through decentralisation was not achieved. To the contrary, in the institutional design of the newly created local authorities and in the civil service recruitment policy efficiency considerations did not matter. Additionally, the created mechanisms for political participation generate relevant costs. Thus it is impossible to judge unambiguously on the contribution of decentralisation to the achievement of good governance. Different subtargets of good governance are influenced contrarily. Consequently, the adequacy of the concept of good governance as a guiding concept for decentralisation policies can be questioned. The assessment of the success of decentralisation policies requires a normative framework that takes into account the relations between both participation and efficiency. Despite the partly reduced administrative efficiency the author’s overall impression of the decentralisation process in Lesotho is positive. The establishment of democratically legitimised and participatory local governments justifies certain additional expenditure. However, mistakes in the design and the implementation of the decentralisation strategy would have been avoidable.
In der vorliegenden Arbeit analysiert Yann Wernert die Rolle der Afrikanischen Union im Rahmen von Regionalkonflikten in Afrika. Dabei wird insbesondere Wert auf die konkrete Vorgehensweise der Afrikanischen Union in den jeweiligen Konflikten gelegt. Untersucht wird der Bürgerkrieg in Somalia sowie die Versuche seitens der internationalen Gemeinschaft, eine stabile politische Ordnung wieder aufzubauen. Ebenfalls analysiert wird der Darfur-Konflikt im Sudan und die Möglichkeiten, den regelmäßig stattfindenden Massakern Einhalt zu gebieten. Der Untersuchungszeitraum erstreckt sich von 2003 bis 2007.
Ende 2013 begannen massive militärische Auseinandersetzungen in der Hauptstadt Juba. Hintergrund sind Machtkämpfe zwischen dem Präsidenten und seinem Stellvertreter. Dadurch sind die ethnischen Differenzen zwischen den Dinka und den Nuer wieder aufgebrochen. Innerhalb weniger Tage starben mehrere Hundert Menschen, Tausende flohen, internationale Helfer wurden ausgeflogen. Die Kämpfe griffen schnell auf andere Regionen des Landes über. Südsudan droht ein neuer Bürgerkrieg.
Indien inside
(2013)
Die Bilder vom heutigen Indien faszinieren, aber mehr noch erschrecken sie. Der gnadenlose Kontrast, der mehr ist als „soziale Ungleichheit“, die grausame Armut, die trotz Wachstum in den vergangenen Jahren dramatisch angestiegen ist. 42 Prozent der Inder leben heute unter der Armutsgrenze. Das sind 500 Millionen Menschen! Dazu kommen die sich über das ganze Land ausbreitende, oft tödliche Gewalt, nicht nur, aber vor allem gegen „Indiens Töchter“, ein fortdauerndes archaisches Kastenwesen, ein immer stärker werdender Separatismus, der die nationale Einheit ernsthaft infrage stellt, bürgerkriegsartige Zustände in einigen Bundesstaaten und eine massive Zerstörung der Umwelt.
This thesis presents investigations on sediments from two African lakes which have been recording changes in their surrounding environmental and climate conditions since more than 200,000 years. Focus of this work is the time of the last Glacial and the Holocene (the last ~100,000 years before present [in the following 100 kyr BP]). One important precondition for this kind of research is a good understanding of the present ecosystems in and around the lakes and of the sediment formation under modern climate conditions. Both studies therefore include investigations on the modern environment (including organisms, soils, rocks, lake water and sediments). A 90 m long sediment sequence was investigated from Lake Tswaing (north-eastern South Africa) using geochemical analyses. These investigations document alternating periods of high detrital input and low (especially autochthonous) organic matter content and periods of low detrital input, carbonatic or evaporitic sedimentation and high autochthonous organic matter content. These alternations are interpreted as changes between relatively humid and arid conditions, respectively. Before c. 75 kyr BP, they seem to follow changes in local insolation whereas afterwards they appear to be acyclic and are probably caused by changes in ocean circulation and/or in the mean position of the Inter-Tropical Convergence Zone (ITCZ). Today, these factors have main influence on precipitation in this area where rainfall occurs almost exclusively during austral summer. All modern organisms were analysed for their biomarker and bulk organic and compound-specific stable carbon isotope composition. The same investigations on sediments from the modern lake floor document the mixed input of the investigated individual organisms and reveal additional influences by methanotrophic bacteria. A comparison of modern sediment characteristics with those of sediments covering the time 14 to 2 kyr BP shows changes in the productivity of the lake and the surrounding vegetation which are best explained by changes in hydrology. More humid conditions are indicated for times older than 10 kyr BP and younger than 7.5 kyr BP, whereas arid conditions prevailed in between. These observations agree with the results from sediment composition and indications from other climate archives nearby. The second lake study deals with Lake Challa, a small, deep crater lake on the foot of Mount Kilimanjaro. In this lake form mm-scale laminated sediments which were analyses with micro-XRF scanning for changes in the element composition. By comparing these results with investigations on thin sections, results from ongoing sediment trap studies, meteorological data, and investigations on the surrounding rocks and soils, I develop a model for seasonal variability in the limnology and sedimentation of Lake Challa. The lake appears to be stratified during the warm rain seasons (October – December and March – May) during which detrital material is delivered to the lake and carbonates precipitate. On the lake floor forms a dark lamina with high contents of Fe and Ti and high Ca/Al and low Mn/Fe ratios. Diatoms bloom during the cool and windy season (June – September) when mixing down to c. 60 m depth provides easily bio-available nutrients. Contemporaneously, Fe and Mn-oxides are precipitating which cause high Mn/Fe ratios in the light diatom-rich laminae of the sediments. Trends in the Mn/Fe ratio of the sediments are interpreted to reflect changes in the intensity or duration of seasonal mixing in Lake Challa. This interpretation is supported by parallel changes in the organic matter and biogenic silica content observed in the 22 m long profile recovered from Lake Challa. This covers the time of the last 25 kyr BP. It documents a transition around 16 kyr BP from relatively well-mixed conditions with high detrital input during glacial times to stronger stratified conditions which are probably related to increasing lake levels in Challa and generally more humid conditions in East Africa. Intensified mixing is recorded for the time of the Younger Dryas and the period between 11.4 and 10.7 kyr BP. For these periods, reduced intensity of the SW monsoon and intensified NE monsoon are reported from archives of the Indian-Asian Monsoon region, arguing for the latter as a probable source for wind mixing in Lake Challa. This connection is probably also responsible for contemporaneous events in the Mn/Fe ratios of the Lake Challa sediments and in other records of northern hemisphere monsoon intensity during the Holocene and underlines the close interaction of global low latitude atmospheric circulation.
In this work, an approach of paleoclimate reconstruction for tropical East Africa is presented. After giving a short summary of modern climate conditions in the tropics and the East African climate peculiarity, the potential of reconstructing climate from paleolake sediments is discussed. As demonstrated, the hydrologic sensitivity of high-elevated closed-basin lakes in the Central Kenya Rift yields valuable guaranties for the establishment of long-term climate records. Temporal fluctuations of the limnological characteristics saved in the lake sediments are used to define variations in the Quaternary climate history. Based on diatom analyses in radiocarbon- and 40Ar/39Ar-dated sediments, a chronology of paleoecologic fluctuations is developed for the Central Kenya Rift -lakes Nakuru, Elmenteita and Naivasha. At least during the penultimate interglacial (around 140 to 60 kyr BP) and during the last interglacial (around 12 to 4 kyr BP), these lakes experienced several transgression-regression cycles on time intervals of about 11,000 years. Additionally, a long-term trend of lake evolution is found suggesting the general succession from deep freshwater lakes towards more saline waters during the last million years. Using ecologic transfer functions and a simple lake-balance model, the observed paleohydrologic fluctuations are linked to potential precipitation-evaporation changes in the lake basins. Though also tectonic influences on the drainage pattern and the effect of varied seepage are investigated, it can be shown that already a small increase in precipitation of about 30±10 % may have affected the hydrologic budget of the intra-rift lakes within the reconstructed range. The findings of this study help to assess the natural climate variability of East Africa. They furthermore reflect the sensitivity of the Central Kenya Rift -lakes to fluctuations of large-scale climate parameters, such as solar radiation and sea-surface temperatures of the Indian Ocean.
Menschenrechte auch in Afrika! : WT-Interview mit dem ugandischen Richter George W. Kanyeihamba
(2009)
Im Rahmen der alljährlichen Potsdamer Frühjahrsgespräche, die die Stiftung Entwicklung und Frieden in Kooperation mit WeltTrends durchführt, hatten wir Gelegenheit zu einem Gespräch mit dem ehemaligen Richter am Afrikanischen Gerichtshof für Menschenrechte und die Rechte der Völker, George W. Kanyeihamba aus Uganda.