Made available in DSpace on 2014-10-09T12:42:16Z (GMT). No. of bitstreams: 0 / Made available in DSpace on 2014-10-09T14:05:20Z (GMT). No. of bitstreams: 0 / Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP) / Dissertação (Mestrado) / IPEN/D / Instituto de Pesquisas Energeticas e Nucleares - IPEN-CNEN/SP / FAPESP:11/04051-3

Made available in DSpace on 2014-10-09T12:42:16Z (GMT). No. of bitstreams: 0 / Made available in DSpace on 2014-10-09T14:05:20Z (GMT). No. of bitstreams: 0 / Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP) / Este estudo teve como objetivo a determinação da concentração de entrada dos Gases de Efeito Estufa (GEE) no ar proveniente do Oceano Atlântico na região norte/nordeste da costa brasileira e o entendimento da origem destas massas de ar e o padrão circulatório e sua sazonalidade. Esta parte do litoral corresponde à área em que as massas de ar adentram no continente, antes de chegar à Bacia Amazônica. Em 2010 foram iniciados estudos em dois locais na costa, Salinópolis, no estado do Pará e Natal, no Rio Grande do Norte. Amostras de ar foram coletadas em superfície semanalmente e foram analisadas no Laboratório de Química Atmosférica do IPEN, quantificando-se os gases: dióxido de carbono (CO2), metano (CH4), óxido nitroso (N2O), hexafluoreto de enxofre (SF6) e monóxido de carbono (CO). Os resultados obtidos mostraram que Salinópolis (SAL) apresenta maior sazonalidade, entre as estações climáticas, quando comparada a Natal (NAT), sendo essa observação confirmada pelas trajetórias retrocedentes das massas de ar, para cada local de estudo. Observou-se que SAL recebe massas de ar, tanto do Oceano Atlântico Norte, como do Sul (dependendo da época do ano), e em NAT, as massas de ar são originárias apenas do Oceano Atlântico Sul. Este comportamento está relacionado com a zona de convergência intertropical. Os resultados de uma maneira geral mostram a ocorrência de um crescimento nas concentrações médias obtidas em SAL e NAT com o passar dos anos, acompanhando o crescimento mundial. A concentração média para o principal GEE, CO2, em SAL nos anos de 2010, 2011 e 2012 foi de 388,01, 390,39 e 392,14 ppm, respectivamente, e em NAT foi de 388,59, 389,65 e 392,59 ppm respectivamente. / Dissertação (Mestrado) / IPEN/D / Instituto de Pesquisas Energeticas e Nucleares - IPEN-CNEN/SP / FAPESP:11/04051-3

As crescentes preocupações com a mitigação das mudanças do clima levaram à criação de mecanismos de mercado que recompensassem financeiramente ações adicionais de remoção de gases do efeito estufa da atmosfera através de projetos voltados ao mercado de carbono. Embora, no âmbito do Protocolo de Kyoto, apenas atividades florestais de florestamento e reflorestamento sejam consideradas elegíveis, a maturação do mercado voluntário de carbono levou regimes de mercado como o Verified Carbon Standard (VCS) a aceitaram, entre outras, atividades de projeto envolvendo a melhoria do manejo florestal, incluindo a conversão da exploração madeireira convencional (EC) para o manejo florestal com exploração de impacto reduzido (MF-EIR), atividade esta que, muito provavelmente, estará inclusa no escopo de um futuro programa florestal de mitigação das mudanças do clima, o REDD+ (redução de emissões do desmatamento e degradação florestal mais os benefícios do seqüestro de carbono através de melhorias do manejo florestal). Utilizando uma série histórica de 16 anos de dados de uma área florestal explorada através da EC e do MFEIR em Paragominas, Estado do Pará, estimou-se os impactos dos tratamentos na dinâmica do carbono ao longo do tempo, sob a perspectiva de um projeto florestal de crédito de carbono envolvendo a conversão da EC para o MF-EIR. A comparação entre os tratamento MF-EIR e EC em relação às taxas de regeneração dos estoques de carbono apontou diferenças estatísticas significativas (P < 0,001). O tratamento MF-EIR apresentou um incremento médio observado de 12,30 Mg C ha-1 ano-1 e estimado de 13,01 Mg C ha-1 ano-1, enquanto que o tratamento EC apresentou um incremento médio observado de 5,42 Mg C ha-1 ano-1 e estimado de 5,43 Mg C ha-1 ano-1. O volume de créditos de carbono estimado para o projeto envolvendo a conversão da EC para o MFEIR foi de 61,81 VCUs ha-1. Considerando um buffer de créditos da ordem de 15%, o volume dos créditos passível de comercialização passou para 52,54 VCUs ha-1. A análise econômica realizada, considerando cenários distintos envolvendo a área do projeto (500; 1.000; 5.000; e 10.000 ha) e o preço do crédito de carbono (US$ 5,00; US$ 7,50; e US$ 10,00 unidade-1), resultou em uma matriz de resultados onde apenas projetos com área superior a 1.000 ha seriam possivelmente viáveis economicamente à atividade de projeto de carbono em questão. Por fim, o valor mínimo estimado do crédito de carbono para que não haja prejuízo financeiro aos madeireiros pela postergação do início do segundo ciclo de corte na área do projeto, tempo necessário para que os estoques de carbono da biomassa arbórea viva atinjam seu valor inicial pré-exploração, foi de US$ 5,33 por unidade, estando dentro da faixa de preços praticados pelo mercado de carbono apontada pela literatura. / Growing concerns over global climate change led to the development of market mechanisms that financially compensate additional retention or sequestration of greenhouse gases (GHGs). While under the Kyoto Protocol only forest activities related to afforestation and reforestation are eligible for compensation, maturation of voluntary carbon markets led to schemes such as the Verified Carbon Standard (VCS) to accept other sorts of forest-based offsets, such as the conversion from conventional logging (CL) to reduced-impact logging (RIL). It is anticipated that this sort of activity will also be included in the scope of the future REDD+ program (reduced emissions from deforestation and forest degradation plus the carbon sequestration benefits of improved forest management). Carbon dynamics over a16 year period after CL and RIL in Paragominas, Pará State, Brazil was assessed. The observed and estimated mean annual increments in carbon stocks after RIL were 12.30 Mg C ha-1 yr-1 and 13.01 Mg C ha-1 yr-1. After CL, in contrast, the annual increments in carbon stocks (observed and estimated) were only 5.42 Mg Cha-1 yr-1 and 5.43 Mg C ha-1 yr-1, respectively. The amount of carbon credits estimated for the project involving the conversion from CL to RIL was 61.81 VCUs ha-1. Assuming buffer credits of 15%, tradable carbon was reduced to 52.54 VCUs ha-1. The economic analysis performed, considering different scenarios involving the project area (500; 1,000; 5,000 and 10,000 ha) and carbon credit prices (USD 5.00; USD 7.00 and USD 10.00 unit-1), resulted in an array of results where only projects >1,000 ha would likely be economically viable. Finally, the minimum estimated carbon credit price that would imply in no financial loss to loggers by delaying the start of the second cutting cycle, that is, the, time required for the live carbon stocks to reach their pre-logging values, was USD 5.33 per unit, which is within the range of prices observed on the current carbon market.

L'objectif général de cette thèse est axé sur l’amélioration de modèles agro-hydrologique spatialement distribués pour l’analyse d'agro-hydrosystèmes, sous contrainte de changements climatiques et anthropiques. Cette thèse est structurée autour de trois questions de recherche liées à : i) la représentation de la dynamique spatio-temporelle des systèmes de cultures pour leur utilisation en entrée de modèles agro-hydrologiques distribués ; ii) la représentation du niveau exploitation agricole et des décisions des agriculteurs dans les modèles agro-hydrologiques distribués ; iii) la capacité de ces modèles à simuler des changements climatiques et anthropiquesDes éléments de réponse à ces questions sont apportés par des approches de modélisation réalisées dans différents contextes et à différentes échelles d’espace et de temps. Ces différentes approches sont discutées en les comparant notamment avec d’autres travaux réalisés. Ces différentes études soulèvent la nécessité de développer des méthodologies permettant i) d’une part l’acquisition de données et leur intégration dans les modèles agro-hydrologiques distribués ii) et d’autre part l’amélioration de l’exploitation des simulations, notamment pour les transformer en informations pertinentes et accessibles pour les parties prenantes au niveau d’un territoire. Des perspectives, portant à la fois sur la prise en compte des incertitudes des simulations des modèles agro-hydrologiques et l’analyse de la robustesse de ces modèles, sont également considérées. / The general objective of this thesis is to improve spatially distributed agro-hydrological models for agro-hydrosystems analysis, under climatic and anthropogenic changes, in order to contribute to the identification of levers of action to mitigate effects of non-point source agricultural pollution. This thesis is structured around three research questions related to: i) the representation of spatio-temporal dynamics of cropping systems for their use as input in distributed agro-hydrological models; ii) the representation of farm level and decisions of farmers in distributed agro-hydrological models; and iii) the ability of these models to simulate climate and anthropogenic changes.Elements of response to these questions are provided by modeling approaches carried out in different contexts and at different scales of space and time. These approaches are discussed by comparing them with other works carried out. These different studies raise the need to develop methodologies allowing (i) the acquisition of data and their integration in distributed agro-hydrological models (ii) and, the improvement of the use of simulations results, in particular to transform them into relevant and accessible information for stakeholders at territorial level. Perspectives, covering both uncertainties of the simulations of the agro-hydrological models and the analysis of the robustness of these models, are also considered

Thesis (Ph.D. (Administration)) -- University of Limpopo, 2015 / The thesis of this study is that food production systems for self-provisioning have historically constituted the backbone for survival and life-support in rural South Africa. Colonialism and apartheid capitalism bore harsh effects on the food production life support systems. However, these effects pale into insignificance compared to the present devastation of the food production systems associated with climate change. The contribution of rural South Africa towards climate change is at all scale negligible because poor people hold limited capacity to produce the deleterious gas emissions that allegedly causes global warming. However, the poor are disproportionately exposed to the adversarial effects of climate change and their food production systems have demonstrated beyond doubt that they cannot cope with stressors occasioned by climate change. Government policy and measures continue to be inadequate and inaccessible for rural households that produce for self-provisioning. The thesis further demonstrate that scientifically–based intervention measures adopted among rural poor in developing countries are viewed as alien and therefore not wholeheartedly adhered to by the users. The thesis points to this discrepancy to illustrate that the value systems among the rural population in South Africa describe changes in their food production in terms of climatic conditions that are, according to their belief systems, avoidable consequences of people’s conduct of life outside tradition, religion and so on. It engages a nascent argument relating to the failure of private and public scientifically-generated intervention measures within developing countries’ rurality, which is ironically exacerbated by the apparent inappropriateness and, often, destructiveness vi of the Green Revolution Technologies. As such interventions fail, the thesis points, they create skeletons of evidence, that appear to corroborate the traditionalist belief systems about the locus of causes of change in climatic conditions being extra-terrestrial as a consequence of people’s misconduct of life. The study investigates the effects of climate change on household food production systems in rural Makhado Local Municipality. 30 villages are used for this study in both households questionnaire survey, interview of the key informants and observation of different patterns of production process, geo-spatial features and current settlements patterns. The data analysis results reflect that different households within the municipality experiences variety of effects of climate change. Furthermore, the climatic conditions which consisted of enough reliable precipitation during food production stages have declined; rather in the post-1990 period, the area have been experiencing continuous heatwaves and drought which destroyed household’s crops and livestock. Using the normative and historical research designs the study found that the situation within villages has changed drastically because of climate change when comparing the conditions preand post-1990. The deliberate adoption of the historical design was crucial given that the thesis mission was to highlight the discrepancies in the so-called modern systems versus the traditionalist philosophies that continue to dominate the thinking and action rural populations in most developing countries. Equally, the historical design provides unquestionable possibility of applying appropriate research techniques to contextualize the research problem under investigation. Indeed, this manoeuvre has always been an important part and parcel of the research design and methodology because the thesis vii had to adopt a longitudinal research orientation through an appropriately designed data collection tool, specifically the questionnaire and interview schedule. From a philosophical perspective, the thesis demystifies the thinking that the so-called scientifically-generated interventions against climate change could resolve the attendant challenges, inclusive of food production. That is, it insinuates that appropriate research is needed for developing countries rurality in order to find intervention measures that are a product of the evolution of traditionalist value systems. Tacitly, the thesis challenges the statist and private sector habits of always parachuting the so-called scientifically generated solutions to climate change. / University of Limpopo Research Administration Department.

CLIMATIC CHANGE EFFECT ON HYDROLOGICAL DROUGHT IN THE OTAVA RIVER HEADWATERS Abstract The submitted thesis deals with hydrological drought in condition of climate change in Otava River headwaters. The topic is discussed from four different aspects that together create a complex view on the hydrological drought issues in the catchment. The first aspect, the hydrological drought analysis in daily series, is done by threshold level method and SPA. Second aspect studies the impact of climate change on the hydrological drought by using the BILAN model. Following aspect determines a prediction of low flows and deficit volumes during drought by the recession analysis. Final aspect suggests relating process of management, planning and adaptation measures on drought. Key words: hydrological drought, minimal discharges, deficit volumes, BILAN model, climatic change, recession analysis, Otava River, Modrava, Rejštejn, Sušice, adaptation measures

Marine and coastal ecosystems are subject to diverse and increasingly intensive anthropogenic activities, making understanding cumulative effects critically important. However, accurately accounting for the cumulative effects of human impacts can be difficult, with the possibility of multiple stressors interacting and having greater impacts than expected, compounding direct and indirect effects on individuals, populations, communities and ecosystems. Assessment of multiple stressors therefore requires extensive scientific research that directly tests how single or multiple ecological components are affected by stressors, both singly and when combined, and as a consequence, cumulative effects assessments are now increasingly included in environmental assessments. Currently, there is a need to assess these at larger spatial scales, with additional research also urgently needed on the responses of ecological components, processes and functions to single and cumulative stressors. As cumulative environmental impacts could be better addressed by regional stressor effects assessments that combine methods for predicting multiple pressures on ecosystem recovery alongside degradation, this study used several separate approaches that can be used in parallel to give support for local management measures. I tested four completely different methods - a range of multi-metric indices, a food web model (Ecopath), a predictive model (Ecosim) and a Bayesian Belief Network model. Each approach was tested and compared in two shallow water estuarine systems, in Scotland and England, initially concerning the impact of nutrient enrichment and subsequent recovery and was followed by an investigation of how the addition of multiple stressors (nutrient levels, temperature and river-flow rates) would impact the future state of each system. The response to stressors was highly context dependent, varying between and within geographic locations. Overall, each of the four different approaches complemented each other and gave strong support for the need to make big reductions in the pressures and to consider trade-offs between impacting pressures. The models and tools also indicate that in order to reach an improved overall environmental state of each ecosystem, a focus on nutrient reductions are likely to be the most effective of the controls on stressors explored and that cumulative effects of the management of nutrient inputs and increased water temperatures and river-flow are likely to exist.

Les sols de montagne constituent un réservoir majeur de carbone stocké sous forme de matière organique (carbone organique du sol, COS), potentiellement hautement vulnérable aux changements des conditions climatiques. Afin de comprendre les répercussions des changements des conditions climatiques sur la dynamique du COS des sols de montagne, cette thèse s'appuie sur une expérimentation de transplantation altitudinale de monolithes de sol de prairie subalpine calcaire, mise en place dans le Jura Suisse en 2009. Cette expérimentation permet de simuler deux scénarios réalistes de changements climatiques attendus au cours du 21éme siècle, visant à réchauffer et assécher le climat (+2°C et +4°C ; -20% et -40% de précipitations).La démarche conceptuelle de cette thèse a été d'étudier les effets des changements des conditions climatiques (variations saisonnières et manipulation climatique) au bout de quatre années d'expérimentation sur (i) la dynamique des communautés microbiennes et de leur activité enzymatique de décomposition du COS, (ii) la dynamique de différents pools de COS qui constituent la ressource énergétique des micro-organismes décomposeurs, (iii) les interactions s'établissant entre les communautés microbiennes et leurs ressources énergétiques et (iv) les stocks de COS du sol.Nos résultats montrent une très forte dynamique saisonnière du processus de décomposition microbienne se traduisant par de fortes activités enzymatiques de décomposition, une biomasse microbienne plus importante et une structure des communautés microbienne différente lors de la saison hivernale par rapport à la saison estivale. Ces résultats sont en lien avec la dynamique observée des pools les plus labiles du COS (C organique extractible à l'eau et C organique particulaire libre), et des modèles d'équations structurelles montrent que les conditions climatiques (variations saisonnières et manipulation climatique) modifient les interactions s'établissant entre les communautés microbiennes et leurs ressources pour contrôler la décomposition enzymatique du COS.Enfin, ce travail de thèse montre une forte diminution des concentrations en COS sous l'effet de la manipulation climatique, qui ne peut être expliquée par une décomposition microbienne accrue du COS. Au contraire, nos résultats suggèrent que la diminution de la concentration en COS pourrait être due à l'accélération des processus pédologiques naturels sous les scénarios de changement climatique au sein de ces sols calcaires de prairies subalpines, avec une décarbonatation accrue favorisant la lixiviation du carbone organique dissous et le lessivage du pool de COS associé aux argiles. Ces résultats inédits offrent de nouvelles perspectives de recherche sur les effets des changements climatiques sur l'évolution des stocks de COS. / Mountain soils stocks huge quantities of carbon as soil organic matter (SOM) which may be highly vulnerable to climate change and thus alter the atmospheric greenhouse gases concentration at a decadal timescale. To understand the effect of climate conditions on the dynamics of mountain soil organic carbon (SOC), a climate change experiment was set up in October 2009 in Swiss Jura subalpine grassland soils. The climate change experiment (soil transplantation) simulated two realistic climate change scenarios, with increased air temperatures ranging between 2 °C and 4 °C and decreased precipitation ranging between 20% and 40%. These changes reflect current predictions of climate change for the 21th century in temperate mountain regions.We studied the effect of climate conditions (climate manipulation and seasonal changes) after four years of climate experiment on (i) the dynamic of microbial decomposition, microbial abundance and community structure, (ii) the dynamic soil organic matter pools with contrasted turnover rate and representing the energetic resource of microbial communities, (iii) the interactions between microbial communities and soil organic matter pools and (iv) the soil organic carbon stocks.This work shows a strong seasonal dynamics of microbial decomposition with higher enzymatic activities, higher microbial abundance and shift of microbial community structure in winter than in summer. These results were linked to the seasonal organic matter labile pools dynamics. Moreover structural equation modeling shows that climate manipulation differently influences the drivers of SOC enzymatic decomposition in summer and winter.Finally, this work shows a strong decrease of soil organic carbon concentration under the climate change manipulation which cannot be explained by an increase of microbial activities. In contrast, our results suggest that the observed climate-induced decrease in bulk soil organic C content was due a SOC decrease in the most biogeochemically stable SOM fraction associated with a decrease in clay content and a decrease of soil calcareous concentration. Thus, our results hint more so towards an effect of SOM leaching (Gavazov, 2013) to explain the climate effect on SOC content than an effect of microbial and/or plant activities.

MSc (Zoology) / Department of Zoology / The concept of taxonomic diversity has been widely used to investigate diversity patterns and the mechanism underlying community assembly. However, functional and trait diversity can further explain the factors driving community assembly because they capture different aspects of species ecological roles such as habitat requirements and resource use. To investigate the factors shaping community assembly along the elevational Soutpansberg transect, ants were used as a model study organism because they are widely distributed geographically, ubiquitous and play several important roles in ecosystems. Functional and taxonomic diversity patterns along the elevation, their drivers (seasonality, soil properties, temperature and habitat structure) were examined using a long-term dataset (8 years) collected seasonally. Morphological and physiological traits at a community level are quantified and their relationship to temperature, soil properties and habitat structure modelled. Traits were used to test the size-grain hypothesis, Janzen’s rule and Brett’s rule. Functional and taxonomic diversity had a humped-shaped pattern on the northern and a decreasing pattern on the southern aspect. However, taxonomic diversity did not decrease monotonically on the southern aspect. Functional diversity was mainly related to habitat structure and temperature while taxonomic diversity was explained by seasonality, soil properties and temperature. Functional and taxonomic diversity were positively related at a larger scale but habitat specific at a smaller scale. Taxonomic diversity explained more variation in functional diversity than habitat structure and their interactions. The results supported the size-grain hypothesis and Janzen’s rule but not the Brett’s rule. Patterns in taxonomic and functional diversity mirrored each other but were the result of different mechanisms. Temperature was however important for both measures. Incorporating functional diversity analysis into taxonomic diversity contributed significantly in understanding the different mechanisms underlying community assembly along the Soutpansberg transect. This together with trait responses to environmental variables such as a decrease in size with increased temperature could be used to model the responses of ant communities to global change drivers such as climate and land use change / NRF

Ethiopia is an agrarian country dominated by subsistence farming which is highly vulnerable to climate change. This study was therefore carried out to assess smallholder farmers’ perceptions of climate change and adaptation strategies followed to prevent vulnerability to climate change in the Medium and Upper highlands of the Amhara region of Ethiopia. Data was collected from 300 sample smallholder farmers using questionnaire, key informant interviews, and Focus Group discussions with farmers and experts. The survey result showed that households differ in terms of asset endowments, vulnerability, and coping and adaptation capability to climate change. About 87.3% noticed climatic change and their perception of climatic variable attributes indicated about 75% felt a decline in the amount of rainfall, 52.6% stated early onset, about 66.6 % showed late on set, 84% expressed poor distribution of rainfall, high temperature (83.7%) and desiccating wind (52.7%). The major adaptation strategies employed by the majority of small holder farmers included enhancing traditional irrigation, use of drought tolerant and early maturing varieties, converting farm land to tree growing and relay cropping immediately after harvesting. The coping strategies to climate variability are largely related to migrating to urban areas, engaging in daily work, selling of fuel wood and asset while mitigation measures have focused on ecosystem rehabilitation. “Multi Nominal Logit” (MNL) model analysis indicated gender, education, off farm activity, farm size, ownership of oxen, farmer to farmer extension, access to credit and information on climate change as determinants of adaptation to climate change and variability. Institutional support to farmers’ efforts to adapt to climate change is generally weak. The overall analysis leads to conclude that despite the presence of awareness on climate change and its likely impacts on livelihoods of the smallholder farmer, development intervention at local level are not systematically designed to address the problems of the resource poor farmers and environmental challenges. In the immediate future there is an urgent need to capitalize on existing awareness, document, package and disseminate successful adaptation interventions to farmers. As a long term solution it is recommended that institutions in charge of climate change need to develop a national drought and climate change management strategic plan with full accountability to facilitate ecosystem development, resilience against climate change and ultimately improvements in the livelihood of farmers. Such interventions could potentially be achieved by taking practical measures on policy support and Institutional building for climate change, knowledge management on adaptation to climate change, filling technological gaps related to agriculture including livestock husbandry in the context of climate change, applying innovative local level participatory land use planning and promoting livelihood diversification initiatives that could enable small holder farmers create assets to enhance their livelihoods. / Environmental Sciences / D. Phil. (Environment Management)