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The spiritual weakness of Western Missionary Founded Churches as the cause of the rise of Africa Independent Churches in Zimbabwe with special reference to theUniting Presbyterian Church in Southern AfricaMushayavanhu, David January 2013 (has links)
This dissertation is an attempt to analyse and investigate ways of responding to the poor UPCSA missional approach to Zimbabwean society. The desire to write this dissertation was born out of the experience of working for the past six years as an ordained minister of this denomination in the Presbytery of Zimbabwe, there are six congregations with the right to call a minister, thirty grant receiving and fifteen preaching stations in the whole country which is serviced by thirteen ministers, including probationers. The UPCSA has a total of four thousand five hundred and ninety seven members not counting Sunday school children. The dissertation seeks to survey the history of how the people in the Presbytery of Zimbabwe came to be some of fewer memberships as compared to other denominations in the country. It will focus on colonial and post –colonial events, which led to evangelizing the nation.
The spiritual weakness which the people of Presbytery of Zimbabwe (POZ) experience is a product of the evangelism mode of missional approach to society and the failure to contextualize the Good-News. This dissertation considers the possibility of how to correct this state of affairs.
Spiritually weak people have been destroyed precisely because they have reduced them to products. How to understand the context and achieve that change is the central issue which the writer addresses in this dissertation. / Dissertation (MA Theol)--University of Pretoria, 2013. / gm2014 / Church History and Church Policy / unrestricted
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The COMESA, EAC and SADC Tri-partite Free Trade Agreement: Prospects and Challenges for the Regions and AfricaMathys, Reagan January 2012 (has links)
Masters administration (M. Admin) / The tri-partite initiative in and for Africa has been accompanied by high levels of optimism since its political endorsement in 2008. It provides for an opportunity to resolve a host of problems with regards to regional integration in Eastern and Southern Africa. The overall aim of this study is to explore the prospects and challenges towards realising the Tri-partite Free Trade Area (T-FTA) in and for Africa. This study is pragmatic and implicitly seeks to uncover how the T-FTA could contribute to the African Regional Integration Project (ARIP), given the challenges that regional integration face in Africa. Regional integration has a long and rich history in Africa, which started at thehave been weak since the start and persist in its superficial nature with littledevelopmental impact. The reasons for the lack of meaningful integration in Africa are wide-ranging and span national, regional and system level analytical viewpoints. They encompass areas such as developmental levels, political will, respect for regional architecture, overlapping membership and the Economic Partnership Agreements (EPAs). These factors impact on the integration process in Africa and explain in varied ways why there has been little comprehensive economic integration. The starting point was to define the complex concept of regional integration. The dominant factors that define and affect regional integration in this study are that it is a state-based exercise, driven by economic integration, and influenced by the global political economy of the day. It was determined that Africa has adapted its regional integration strategies according to the shifts and influences in the global political economy on states, emanating from the post WWII period to the present day. The mpact of the global economy on Africa since independence was great and is viewed impact on the integration process. Regional integration is essentially a state to state pursuit for integration. Essentially, regional integration is being pursued by states that are still struggling to consolidate statehood, and this leaves little space to move towards a regional approach. However, given the dynamics of a globalised world, regional integration as a strategy is no longer questioned in Africa and is an important component of its developmental agenda. Clarifying the T-FTA was important, and this was done in order to highlight what the tri-partite initiative is and is not. This provided for an opportunity to investigate what the dominant areas are that have informed the emergence of the tri-partite process. The former was found to be largely economic in nature, focusing on harmonising the trade regimes of COMESA, EAC and SADC as a primary motivation. The tri-partite initiative will facilitate and encourage the harmonisation of trade regimes by stressing market integration, infrastructure development and industrialisation, coupled by a developmental approach. This is promising, as the tri-partite initiative seeks to simultaneously deal with many issues that have been commonly associated with the problems that regional integration face in Africa. When viewing the negotiating context, as well as the principles upon which it is to be based, indicate though, that Africa still favours individual state interest that will be hard to reconcile given that the tri-partite region currently has 26 participant states. In terms of economic integration, the T-FTA seeks to put new generation trade issues on the agenda by including services, movement of persons as well as trade facilitation, all of which have been found to be important in realising a trade in goods agenda that is the focus of regional integration in Africa. Analysing the grassroots realities of the market integration pillar offered some valuable insights towards the purposes of this study. The market integration pillar is inundated with challenges, with Rules of Origin (RoO) being the primary challenge towards consolidating the trade in goods agenda on a tri-partite level. New generation trade issues are going to be equally difficult to realise, given that they have no implementation record in the individual Regional Economic Communities (RECs). Promising though is that trade facilitation has already seen positive results by resolving non tariff barriers in the regions.Infrastructure development is equally challenging, although it provides a significant opportunity to create better connectivity (physical integration) between states. In lot of pan-African goals that directly feed into initiatives of the African Union (AU) pillar has not as yet created any concrete tri-partite plans, so it remains to be seen what can be achieved. Ideally, industrialisation is viewed as the pillar that will solve the supply-side constraints of African economies hence, strengthening the trade in goods agenda in the regions. Even though the T-FTA has practical challenges to implementation, there are at least two underlying factors that indirectly affect the prospects of realising the tripartite initiative. The EPAs are an emergent threat in that they run parallel to tripartite negotiations; and respect for a rules based integration process, are issues that warrant consideration. Fundamentally, in order to achieve a successful T-FTA will require a shift in the way business is done in African integration. African states need to realise that their national interests are best served through cooperation, in meaningful ways. Inevitably this requires good faith as well as ceding some sovereignty towards regional goals. Thus, there is a risk that the T-FTA not realised. The fundamentals of political will, economic polarisation and instability have to be resolved. This will lay an appropriate foundation for the tripartite initiative to be sustainable, with developmental impact. / South Africa
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The concept of economic integration with specific reference to financial integration in southern AfricaNokaneng, Shima Henock 28 March 2009 (has links)
The objective of the study is to establish how original financial integration could be attained in southern Africa in order to attract more foreign investment and develop a financially robust and stable region in the southern part of Africa; also to deal with the challenges, risks and remedies of prospective future financial crises. Financial markets are rapidly integrating into a single global market. Developing countries of various regions are drawn into the process with little choice, and without having sound financial infrastructure and policies in place. It is against this background that countries and regions of global integration choose policies that would benefit their regional economy and avert potential economic shock. The challenges posed to countries and regions by the progressive global integration of financial markets are becoming more urgent by the day. These challenges need to be addressed more effectively, either nationally or regionally, as demonstrated by the 1998 financial turmoil in Asia. Private capital flows are becoming intra regionally concentrated, particularly in the USA, Europe, Asia and Latin America. Be that as it may, failure in one market is likely to have immediate and large regional repercussions. Globalisation also marginalises Africa and other Least Developed Countries (LDC), leaving them more impoverished and with greater disparities in terms of income, GDP and FDI. Regional financial integration has to be efficient and sound in order to prevent or contain currency and capital market crises in the southern African region. This study identifies macro economic challenges and risks associated with financial integration. Recommendations are made about methodologies of addressing these issues in order to realise the benefits of regional financial integration in southern Africa, which could be a building block in realising the dream of an African Monetary Union. The study contributes greatly to the debate around the most appropriate criteria that are to be met by the SADC countries, before monetary integration can become a reality. A comparison of the benchmark macro economic convergence criteria of the EU and of the African Monetary Union is done and the performance of SADC countries is assessed in terms of both sets of benchmarks. Southern African states are found to not even be at a comparable level with regard to the EU targets of 1997. The thesis is also critical to the impact of the political instability in the SADC region on prospective monetary integration. Most importantly, SADC would be at a permanent disadvantage and face a long-run depreciation of its common currency, should it continue to integrate financially at macro economic benchmark levels inferior to those of its major trading partner, the EU. / Thesis (PhD)--University of Pretoria, 2009. / Economics / unrestricted
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The mechanisms of politico-security regionalism in Southeast Asia and Southern Africa : a comparative case study of ASEAN and SADCHwang, Kyu Deug 27 September 2006 (has links)
The central question addressed by this thesis is whether and to what extent ASEAN and SADC provide a regional response to security challenges from within and without the region respectively. In the examination of a regional response to security challenges in Southeast Asia and Southern Africa, this study investigates each regional organisation’s efforts and methods of how to approach and deal with regional security problems. In examining the processes and patterns of ASEAN and SADC regionalism in terms of the security dimension, the focus is on political security in its regional context. In doing so, the mechanisms of both ASEAN and SADC politico-security regionalisms are explored. This study also aims to compare SADC and ASEAN to find similarities and differences in terms of the way in which ‘politico-security regionalism’ as a regional project is used to respond to global challenges, as well as to internal needs. Moreover, this study seeks to explore what can be learnt from the experiences of both ASEAN and SADC with regard to regionalism and regionalisation in response to political security threats. This will, as a result, be conducive to understanding the character, nature and type of contemporary regionalism and regional security in the South, including Southeast Asia and Southern Africa. Furthermore, in discussing the question of whether and how ASEAN and SADC attempt to shape and modify or change the process of globalisation and regionalisation in politico-security terms, this study emphasises a multi-dimensionality of contemporary regionalism – so called ‘new regionalism’ – which would normally be based on constructivism. Therefore, this study argues that the theoretical problem relates to the insufficiency of neo-realist and neo-liberal institutionalist accounts that call for a much needed attempt to bring ASEAN and SADC into contemporary discussions about the mechanisms of politico-security regionalisms within the context of a (social) constructivism of international relations (IR) theory. / Thesis (DPhil (International Relations))--University of Pretoria, 2007. / Political Sciences / unrestricted
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Simulation of tropical cyclone-like vortices over the southwestern Indian OceanMbedzi, Maluta Pennington 25 October 2010 (has links)
Tropical cyclones claim a huge number of lives and cause substantial damage to property and crops in many regions each year. Southern Africa is no exception. This makes the process of forecasting tropical cyclones of great importance to the region’s economy and to public safety. Skillful seasonal forecasts of tropical cyclone activity could be used to warn the communities affected by tropical cyclones of the likely occurrence of such systems ahead of the cyclone season. This could result in reduced damage and fatalities associated with such systems. Both statistical and dynamical techniques have been employed in an attempt to predict tropical cyclone activity on a seasonal time scale over a number of ocean basins. The skills of such techniques vary from one technique to another and from one basin to another. This study investigates the predictability of tropical cyclone activity on a seasonal time scale over the southwestern Indian Ocean (SWIO) by nesting a regional climate model (RCM), the RegCM3 within a coarse-resolution atmospheric general circulation model (AGCM), the ECHAM4.5. The national meteorological centres of most southern African countries do not have the required dedicated computational resources to run the high-resolution GCMs that are suitable to predict these systems operationally. However, these systems can be very devastating on the southern African region and need to be predicted on various time scales, including the seasonal time scale. Therefore, it is instructive that research be done to better our understanding of these systems and their predictability using physical models. This study examines the simulations of the genesis locations and the number of tropical cyclones produced in RCM integrations nested within an AGCM forced by observed sea-surface temperatures (SSTs). The season of interest is the mid-summer period of December to February. Four members of the AGCM generated at the International Research Institute for Climate and Society (IRI) are used to force the RCM. Four-month integrations over a 10-year period (1991/92-2000/01) are performed. An objective procedure for detecting model-generated tropical cyclones is applied to this ensemble. Some characteristics of the simulated cyclones are compared with the observations. In addition, some statistical techniques are employed to evaluate the capability of the RCM to reproduce some aspects of the observed tropical cyclones during the aforementioned period. The results show that there is a good agreement between two of the simulated and observed environmental variables that influence tropical cyclone formation, viz. vertical wind shear and relative vorticity. In particular, the simulated and observed vertical wind shear show a similar pattern in most parts of the model domain. With regards to the relative vorticity, the highest agreement is found in the Mozambique Channel and in the region east of Madagascar. In addition, there is an appreciable agreement between the simulated and observed tropical cyclone characteristics such as tropical cyclone genesis locations and frequency. The model also simulated the interannual variability in the tropical cyclone frequency skillfully. AFRIKAANS : Tropiese siklone is verantwoordelik vir ‘n goot aantal sterftes en veroorsaak beduidende skade aan eindom asook oeste oor etlike areas elke jaar. Suidelike Afrika is nie ‘n uitsondering nie. Hierdie verliese maak die voorspelling van tropiese siklone van groot belang vir die gebied se ekonomie asook vir publieke veiligheid. Vaardige seisoenale voorspelling van tropiese sikloon aktiwiteit kan gebruik word om gemeenskappe wat onderhewig is aan die invloed van tropiese siklone te waarsku oor die kans vir sulke sisteme om voor te kom voordat die tropiese sikloon seisoen ‘n aanvang neem. Vroegtydige waarskuwings kan tot gevolg hê dat daar minder verwant skade en laer sterftes is. Beide statistiese en dinamiese tegnieke is al in die verlede gebruik om tropiese sikloon aktiwiteit oor verskeie oseaankomme op ‘n seisoenale tydskaal te probeer voorspel. Die vaardigheid van hierdie tegnieke hang af van die tipe tegniek wat gebruik word asook watter oseaankom beskou word. Hierdie studie ondersoek die voorspelbaarheid van tropies sikloon aktiwiteit op ‘n seisoenale tydskaal oor die suid-westelike Indiese Oseaan deur gebruik te maak van ‘n streeksmodel, die RegCM3, genes in ‘n growwe-resolusie algemene sirkulasie model van die atmosfeer, die ECHAM4.5. Die nasionale weerdienste van die meerderheid Suider-Afrikaanse lande beskik nie oor die nodige rekenaars om geskikte hoë-resolusie algemene sirkulasie modelle te loop om sodanige sisteme mee operasioneel te voorspel nie. Desnieteenstaande kan hierdie tropiese sisteme verwoestend wees en daarom behoort hulle voorspel te word op verskeie tydskale, insluitende seisoenale tydskale. Dit sal dus insiggewend wees om navorsing te doen om sodoende ons begrip oor hierdie sisteme en hul voorspelbaarheid te verbeter deur gebruik te maak van fisiese modelle. Hierdie studie gaan ondersoek instel oor die simulasie van tropiese siklone oor hul ontwikkelingsgebiede en die aantal tropiese siklone wat ‘n streeksmodel, genes in ‘n algemen sirkulasie model van die atmosfeer wat geforseer word deur waargeneemde see-oppervlak temperature, kan produseer. Die seisoen van belang is die mid-somer periode van Desember tot Februarie. Vier ensemble lede afkomstig vanaf die algemene sirkulasie model wat geloop is by die International Research Institute for Climate and Society word gebruik om die streeksmodel mee te forseer. Model integrasies word oor ‘n 4-maand periode gedoen en vir ‘n 10-jaar tydperk (1991/92-2000/01). ‘n Objektiewe vorteks opsporingsprosedure word dan toegepas op die 4-lid ensemble om model-geskepte tropiese siklone te identifiseer. Sommige van die karakteristieke van die gesimuleerde siklone word dan vergelyk met die waargeneemde tropiese stelsels. Hiermee saam word statisiese tegnieke ingespan vir die genoemde tydperk om die vermoë van die streeksmodel te ondersoek om sekere aspekte van waargeneemde storms te herproduseer. Die resultate wys dat daar ‘n goeie ooreenkoms is tussen twee van die gesimuleerde en waargeneemde omgewingsveranderlikes wat tropiese sikloon ontwikkeling beinvloed, nl, vertikale windskuiwing en relatiewe vortisiteit. In besonder het die gesimuleerde en waargeneemde vertikale windskuiwing ooreenstemmende patrone gelewer oor die grootste gedeelte van die streeks model-area. Wat relatiewe vortisiteit betref, is die beste ooreenkoms oor die Mosambiek kanaal en in die gebied oos van Madagaskar gevind. Verder is daar ‘n sterk ooreenkoms tussen die gesimuleerde en waargeneemde tropiese sikloon karakteristieke soos by die tropiese siklone se ontwikkelingsgebiede asook hul frekwensie. Die model he took daarin geslaag om die inter-jaarlikse veranderlikheid van tropiese sikloon frekwensie suksesvol te simuleer. / Dissertation (MSc)--University of Pretoria, 2010. / Geography, Geoinformatics and Meteorology / MSc / Unrestricted
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Environmental history in southern Mozambique : Reconstruction of flooding events, hydroclimate and sea-level dynamics since mid-HoloceneRaúl Sitoe, Sandra January 2017 (has links)
The aim of this thesis has been to reconstruct paleoenvironment, paleohydrology and paleoclimate in coastal southern Mozambique, with emphasis on tracing past flooding events on the lower Limpopo River floodplain. In order to extend flood chronologies beyond periods covered by instrumental data, sediments from lakes on the floodplain were studied (Lake Lungué, Coassane Oxbow, Lake Magandane and Lake Soane). Past sea-level variations and climate changes were deduced by analyzing sediments from coastal sites north of the floodplain area (Lake Chilau, Lake Nhauhache and Macassa Bay). To achieve the established objectives, a multi-proxy approach was applied on most of the retrieved sediment cores, involving analysis of mineral magnetic parameters, grain-size and organic carbon in combination with analysis of microfossils such as diatoms and/or phytoliths. Chronologies for the constructed time-series analysis were obtained by radiocarbon dating and age-depth modelling. The synthesized data from the sampled sites on the Limpopo River floodplain suggest that the area was affected by at least 16 flooding events of variable magnitudes during the studied period. These are dated to c. AD 940, 980, 1040, 1100, 1250, 1300, 1370, 1580, 1665, 1730, 1755, 1855, 1920, 1945, 1970 and 2000. In calibrated years BP these ages correspond to 1010, 970, 910, 850, 700, 650, 580, 370, 285, 220, 195, 95, 30, and 5 cal yrs BP. The two youngest are dated to 20 and 50 years AP (After Present being 1950). Proxy data further suggest that southern Africa was subject to two periods of sea-level highstands, at c. 5000–4200 BC (6950–6150 cal yrs BP) and AD 300–950 (1650–1000 cal yrs BP). The former represents the middle part of the postglacial climatic optimum. The wettest period in the Limpopo River floodplain was reported between AD 1360 and 1560 (590 and 390 cal yrs BP) in the Lake Lungué record, while Lake Chilau experienced wet conditions between AD 1200 and 1400 (750 and 550 cal yrs BP), then returning to drier conditions that prevailed until c. AD 1600. In Lake Nhauhache, however, drier conditions prevailed from c. AD 1200–1700 (750–250 cal yrs BP), shifting towards wetter at c. AD 1900 (50 cal yrs BP). The deviating signals between records can partly be explained by Lake Lungué basin being located on the Limpopo River floodplain, responding to flooding events associated with precipitation upstream the drainage area. Therefore, wet and dry periods in floodplain lakes (e.g. Lake Lungué) are not expected to correlate with precipitation changes on a local scale, as indicated by e.g. Lake Nhauhache. This is supported by a relatively weak agreement between Lake Lungué record and other nearby records (outside the floodplain), but a better correlation with records from the upper catchment, where a more regional climate signal is provided of the southern African summer rainfall region. / Denna avhandling behandlar studier av paleomiljöer i södra Mozambique med fokus på översvämningshistorik i Limpopo-flodens nedre lopp. Tidsspannet är mitt- och sen-holocen och inkluderar även klimat och havsnivåvariationer. Följande analysmetoder har applicerats på ett flertal sedimentkärnor för att belysa ovanstående frågeställningar: mineralmagnetiska parameterar, kornstorlek, organiskt kol samt kiselmikrofossil (diatoméeter och fytoliter). Åldrar har bestämts med 14C-metoden. Analyserna visar att mineralmagnetiska parametrar är lämpliga för att identifiera översvämningar, speciellt magnetisk susceptibilitet och SIRM. Dessa parametrar visar på ett sediments magnetiska kornstorlerkar och koncentrationen av finkorniga magnetiska mineral. Även kornstorleksanalyser fungerade som ett bra komplement till dessa metoder. Sammantaget har ett minimum av 16 översvämningar registrerats i Limpopo/flodens nedre lopp under de senaste 1100 åren. Särskilt stora översvämningar har daterats till AD 1250 (700 kal år BP), AD 1370 (580 kal år BP), AD 1580 (370 kal år BP), AD 1855 (95 kal år BP), AD 1920 (30 kal år BP), AD 1970 (20 kal år AP) och AD 2000 (50 kal år AP), där AP betyder ”after present”, vilket är 1950. Mindre kraftiga översvämningar har daterats till AD 940 (1010 kal år BP), AD 980 (970 kal år BP), AD 1040 (910 kal år BP), AD 1100 (850 kal år BP), AD 1300 (650 kal år BP), AD 1665 (285 kal år BP), AD 1730 (220 kal år BP), AD 1755 (195 kal år BP) och AD 1945 (5 kal år BP). Skriftliga källor visar på att åtminstone åtta översvämningar har ägt rum under de senaste 62 åren. Under samma period har denna undersökning registrerat två händelser, vilket indikerar att endast ett fåtal har registrerats med ovan nämnda metoder. Det är sannolikt att sedimentationsmönstret under en översvämning är komplicerat och inte heller likartad från gång till gång. Detta innebär att ett flertal sedimentkärnor behöver analyseras och dateras väl. Ytterligare en försvårande faktor är flodens mycket aktiva meandringsaktivitet. Analys av diatoméer har visats vara värdefulla när det gäller översvämningshistorik, klimatförändringar och havsytevariationer. Sedimenten i den något till flodslättens nedre lopp perifert belägna sjön Lungué indikerar fuktiga förhållanden mellan AD 1360 och 1560 (590 till 390 kal år BP). Kombinerade fytolit- och diatoméanalyser av sedimenten i sjön Chilau indikerar fuktiga förhållanden från AD 1200 till 1400 (750 till 550 kal år BP), varefter torrare förhållanden rådde till ca AD 1600 (350 kal år BP). Diatoméanalys av sedimenten i sjön Nhauhache indikerar generellt sett torrare förhållanden mellan AD 1200 och AD 1700 (750 till 250 kal år BP) då klimatet blev fuktigare. De fuktiga och torra förhållanden som dokumenterats i sjön Lungué och översvämningshistoriken korrelerar inte helt med lokala nederbördsförhållanden. Däremot stämmer erhållna data bättre med förhållanden i den övre delen av Limpopoflodens dräneringsområde. Även sjöar och fyllda meanderbågar på själva flodslätten verkar reagera tydligare på översvämningar orsakade av nederbörd i den övre delen av flodloppet. Undersökningen indikerar två faser av en förhöjd havsyta längs kusten i södra Mozambique. En äldre fas är daterad till ca 5000–4200 f.Kr. (6950–6150 kal år BP), vilken representerar den mellersta delen av det postglaciala värmeoptimet. Denna tolkning stöds även av andra undersökningar. En yngre fas har daterats till AD 300–950 (1650–1000 kal år BP), vilken korresponderar till en period med något förhöjda temperaturer i ett globalt perspektiv. / O presente projecto teve como objectivo a reconstrução do paleoambiente, paleohidrologia e paleoclima da costa Sul de Moçambique, com ênfase na identificação de vestígios de eventos de cheias que tenham, no passado, afectado a planície de inundação do Rio Limpopo, com vista a fazer a extensão das datações de cheias para o período anterior aos instrumentos de medição. Deste modo, foram estudados sedimentos recuperados através de testemunhos de sondagem em lagos dentro da planície de inundação (Lago Magandane, Lago Lungué, Lago Soane e o canal abandonado Coassane). As variações do nível do mar e mudanças climáticas do passado foram deduzidas a partir da análise de sedimentos de áreas costeiras a norte da planície de inundação (Lago Chilau, Lago Nhauhache e a Baía de Macassa). Para o alcance destes objectivos, os sedimentos dos testemunhos de sondagem recuperados foram submetidos a várias análises laboratoriais que incluem propriedades de minerais magnéticos, granulometria, teor de matéria orgânica e de microfósseis (diatomáceas e fitólitos). Para o estabelecimento do modelo cronológico foram usadas datações pelo método 14C feitas em matéria orgânica, assim como conchas de gastrópodes e bivalves. A combinação dos resultados obtidos para os pontos de amostragem localizados dentro da planície de inundação do Rio Limpopo, sugerem que esta área foi afectada por um mínimo de 16 eventos de cheias de variada magnitude nos últimos 1100 anos. As cheias de alta magnitude tiveram lugar nos anos 1250, 1370, 1580, 1855, 1920, 1970 e 2000. Por seu turno, as cheias de magnitude moderada ocorrerram nos anos 940, 980, 1040, 1100, 1300, 1665, 1730, 1755 e 1945.. Os anos a negrito são indicativos de eventos de cheias de alta magnitude. O número total de eventos identificados no presente estudo é um mínimo que poderá ter afectado a planície de inundação, tendo em consideração que fontes escritas reportam a ocorrência de pelo menos oito eventos nos últimos 62 anos, tendo o presente estudo revelado somente dois. Isto indica que apenas eventos de cheias intensos podem ser revelados pelos métodos aplicados nesta investigação. Adicionalmente, este estudo mostra a necessidade de aumentar o número de pontos de amostragem para permitir a identificação de mais eventos de cheias ocorridos no passado, devido à diferenciada resposta sedimentológica e geomagnética às cheias, a qual se encontra directamente relacionada à distância do rio meandrante. As análises de microfósseis de diatomáceas permitiram reconstruir o paleoclima e as influências do nível do mar nas áreas de estudo deste projecto. Os registros de diatomáceas do Lago Lungué indicam um período húmido entre AD 1360 e 1560. No Lago Chilau, dados de diatomáceas e fitólitos sugerem condições de humidade entre AD 1200 e 1400. Por seu turno, no Lago Nhauhache, condições de seca dominam entre AD 1200 e 1700. As condições de seca e humidade documentadas no Lago Lungué e os eventos de cheias revelados pelos sedimentos analisados da planície de inundação do Rio Limpopo não mostram total correlação com períodos de baixa e alta precipitação a nível local, mas apresentam boa correlação com evidências a montante na área de drenagem do Rio Limpopo. Em geral, lagos activos ou preenchidos por sedimentos mostrarão ser mais susceptíveis a cheias com origem a montante do que a nível local. As investigações conduzidas permitiram identificar dois períodos de alto nível do mar na região sul de Moçambique. A fase mais antiga teve lugar há cerca de 5000–4200 BC (6950–6150 anos do calendário BP), representando a fase mais recente do pós-glaciar climático óptimo (postglacial climatic optimum, PCA). A fase recente é datada de AD 300–950 (1650–1000 anos do calendário BP), correspondendo a um período de temperaturas relativamente altas a nível global. / Climate and Environmental Research
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The activities of the Southern African Development Community in relation to its purpose statementMagakwe, Jack 06 1900 (has links)
The study focuses on and explores the Southern African Development Community’s activities to determine whether the intended objectives have been accomplished as stated in its purpose statement. The study argues that the achievement of the Southern Africa Development Community’s purpose statement is important with regard to the implementation of developmental initiatives. This is because the SADC objectives are measured in the operationalisation and implementation of policies and the operationalisation of key activities. The Southern African region is rich in natural resources but lacks the political will and capacity for the institutionalisation of key processes to, among others, alleviate poverty and HIV/AIDS and address human security matters.
This study revealed that SADC did not achieve all its intended objectives. Several challenges, such as the full convertibility of regional currencies among member states still need to be addressed. One of the major challenges impacting negatively on the implementation and completion of SADC’s projects are the capacity, skills and expertise to drive key business processes. This study has found that in spite of complexities and challenges to implement SADC’s policies and programmes as stated in its purpose statement, there is a need to align the member states’ priorities with SADC’s objectives to maximise impact and overall successful execution thereof. Coupled with this challenge is another crucial challenge relating to the SADC structure, mechanisms and methodologies that are used for achieving SADC’s objectives. The study revealed that the structures, mechanisms and methodologies are inadequate to successfully implement and evaluate SADC’s projects.
Consequently, this study proposes some reforms in SADC’s Regional Indicative Strategic Plan that should be considered and integrated into the national plans, budgets and priorities of all SADC member states. Critically, it is important to ensure the alignment and buy-in of member states with regard to the development and implementation of SADC’s projects and programmes in the Southern African region. Firstly, the study proposes that partnerships with research institutions should be explored to strengthen the limited capacity of SADC’s Secretariat. Benchmarking and best practices with other international government organisations such as the African Union and the United Nations will provide a platform to improve the current activities of SADC to be more focused towards the desired outcomes. Secondly,
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SADC’s activities that are linked to its objectives should be intensified through the mobilisation of resources and expertise that are geared to all key result areas to improve regional integration and ultimately the achievement of SADC’s objectives as stated in its purpose statement. / Public Administration and Management / M.P.A.
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The decision to apply a modified Reagan doctrine towards Mozambique : a case study of the bureaucratic political modelVenables, Robert Andrew 01 1900 (has links)
The Reagan Administration took office in 1981 and began to implement against the
Union of Soviet Socialist Republics (USSR), what became known as the Reagan
Doctrine. The was an effort to break with previous the previous presidential
administration’s policies toward the USSR and would involve the rollback of
Communism, instead of simply just co-existing with Communism (Détente) or containing
the spread of it. Part of the area that was subject to the Reagan Doctrine included the
volatile southern African region, which had two Marxist-Leninist Regimes, namely
Angola and Mozambique. Using Graham Allison’s bureaucratic political model,
this study attempts to answer the question: “Even when all the prerequisites were met,
why was there a decision to only implement a modified form of the Reagan
Doctrine in Mozambique, instead of a full-blown effort, such as in, for example Angola
or Afghanistan?” As will be shown in the research, the Reagan Doctrine was not a
written doctrine, but had many different facets, as will be shown. The most significant
part of the Reagan Doctrine was the recognition and arming of insurgents who confronted
the Soviet backed regimes including RENAMO. There have been claims that the US
Government did not recognize RENAMO. This is false as will be shown by the fact that
President Reagan urged FRELIMO to negotiate with the RENAMO resistance. The real
significance of this is that even if all prerequisites were met, why was there such
reluctance to apply the doctrine with the veracity as compared to the effort in Angola and
Afghanistan in arming RENAMO. Was the United States Government still trapped in the
“Vietnam Syndrome”? Did the Mozambique National Resistance (RENAMO) have the
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same political and charismatic qualities as the Union for the Total Independence of
Angola (UNITA)? Were special interests or lobbyists influencing government
bureaucrats to view decisions in a specific way? A significant part of this study is
devoted to the question of how much influence did the bureaucracy and the politicians
(both appointed and career) had on the important national security decision-making
process involving Mozambique. Another question that could be asked is: Was the
doctrine indirectly applied through third parties? In 1989 when the Reagan
Administration ended, did President Reagan and the Reagan Administration achieve their
objectives toward Mozambique. If so, was this due to the Reagan Doctrine or other
factors? If not, did any actors or events interfere with the strategy? / Political Sciences / M.A. (International Politics)
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THE ROLE OF THE CHURCH OF THE PROVINCE OF SOUTHERN AFRICA IN THE SOCIAL TRANSFORMATIO OF THE WESTERN CAPE 1960 - 1990Haddad, Beverley Gail January 1992 (has links)
Magister Artium (Development Studies) - MA(DVS) / This study reflects the vital role the church should play in the social transformation of society. It undoubtedly has the potential to be a strategic organisation for social change. However, in the past it has failed to reach that potential. The hope for the future is that the church will embrace that potential and become active in the process of social transformation. The Church of the Province of Southern Africa (CPSA) has been the researcher's spiritual home for her entire life. During this time, and particularly over the past five years, she has sought to
find her place in the church's inflexible, bureaucratic and patriarchal structure. While this study was in the final stages of being written, the CPSA took the historic decision to ordain women to the priesthood. Her personal struggle had been vindicated. However, more importantly, the church's decision attests to that organisation's potential for creative change. Thus this study is dedicated to the members of the CPSA in the Diocese of Cape Town, in the hope that they will embrace the challenge, both as individuals and as a community to become active agents of social change. The field research was conducted during the period March 1989 to March 1990 by the researcher herself, who was a paid employee of the Diocese of Cape Town at the time. Both the promoter and co-promoter of this thesis supervised this research. The results were first published in August 1990 by the Diocese of Cape Town in a report entitled, Voices of the Church: An Anglican perspective on welfare and development in the Diocese of Cape Town. Permission to use the research material in this study has been granted by the Most Reverend Desmond Mpilo Tutu, and is acknowledged with thanks. There are many people who during that period enabled the research to take place because of their willingness, enthusiasm and interest: the Most Reverend Desmond Tutu; Bishop Edward the liaison Bishop; members of Chapter and Diocesan Council; the support committee; the 130 people in the parishes who so willingly shared of themselves and their opinions, and in many instances opened their homes; and the clergy of the diocese, who participated wholeheartedly in the process.
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Human trafficking as a security issue : selected case studiesIroanya, Richard Obinna January 2014 (has links)
This study examined and analysed human trafficking as a security issue using South Africa and Mozambique as country case studies. Information gathered through documentary analysis methodology is relied upon to develop a conceptual framework of human trafficking and security. The link between trafficking and security is evaluated based on the conceptualisation of trafficking in the Palermo Protocol as well as the criteria for declaring social phenomena security threats, as articulated by the UN and several scholars. Through global and national overviews of human trafficking, its patterns, extent and enabling conditions are identified and analysed. In South Africa and Mozambique, human trafficking has domestic and international dimensions and is facilitated by several factors. However, factors facilitating domestic trafficking do not necessarily facilitate international trafficking in South Africa. The opposite is however, the case in the Mozambican context. An analysis of global, regional, and national counter trafficking measures, shows that the national security implications of human trafficking are not explicitly addressed. Trafficking involves national border violations; organised crime; corruption, and physical violence which have implications for security at all levels. Consequently, recommendations are made for the explicit securitisation of trafficking as well as the demonstration of sufficient political will to combat it. Regional and international co-operation is also considered necessary to combat trafficking, as well as prosecution of offenders and the introduction of poverty alleviating measures. / Thesis (DPhil)--University of Pretoria, 2014. / tm2015 / Political Sciences / DPhil / Unrestricted
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