940 resultados para Track and field


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Estudo sobre a problemática da Evasão Escolar na Educação de Jovens e Adultos – EJA da Unidade de Educação Básica Alberto Pinheiro em São Luís – Maranhão. Fundamenta-se na análise da literatura sobre as políticas de Educação de Jovens e Adultos no Brasil, no estado da arte sobre a evasão escolar desse segmento de ensino e ainda na análise dos documentos escolares, relatórios e atas de avaliação, que subsidiaram esta investigação. Aplicaram-se questionários e entrevistas, além de pesquisa de campo através da observação direta. Os sujeitos investigados foram os ex-alunos evadidos, professores e pedagogos desse segmento de ensino. A pesquisa indicou que nesse segmento da EJA existe um percentual consistente de evasão escolar, cujas causas vão desde a necessidade de trabalhar até a baixa escolaridade da família. Os resultados mostram o perfil de uma clientela que em sua maioria deseja estudar, mas é impelida a se evadir por diversos motivos, como: a falta de tempo, distância entre o domicílio e a escola, gravidez precoce e despreparo dos professores que atuam nessa modalidade de ensino. Conclui-se que existe a necessidade de melhora das condições físicas e estruturais da oferta da EJA, o que compreende a valorização do professor e as condições materiais da escola.

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Inúmeras pesquisas estão sendo desenvolvidas sobre a importância da formação continuada dos professores para a prática educativa, a fim de melhorar o entendimento sobre as variáveis necessárias para assegurar que os alunos possam obter o aprendizado almejado. Afirma-se ainda que a maioria desses estudos considere que o professor reflexivo possui melhores oportunidades de crescimento profissional e pedagógico, disponibilizando aos seus alunos melhores estratégias didáticas. Para tanto, o objetivo deste estudo é Analisar se a formação continuada de professores, aplicada pelo “Programa Escola que Vale”, tem contribuído para as mudanças das práticas docentes dos professores dos anos iniciais do ensino fundamental I, e como a formação continuada, desenvolvida por este Programa, tem contribuído para as mudanças das práticas docente dos professores dos anos iniciais. Assim, a metodologia deste estudo foi realizada através de uma pesquisa exploratória de caráter bibliográfica e uma pesquisa de campo com docentes, supervisores e orientadores do município de Ourilândia do Norte. Os resultados desta análise nos mostraram que a formação continuada de professores do Programa Escola que Vale, contribuiu muito propiciando melhorias ao desenvolvimento da ação pedagógica, que o profissional torna-se motivado para continuar aprendendo e melhorando sua ação docente, sobretudo utilizando de meios que possibilitam envolvimentos de toda comunidade educativa em prol de uma educação de qualidade.

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Esta pesquisa, cujo referencial metodológico é predominantemente de cunho qualitativo, com participação ativa do pesquisador e dos sujeitos abordados, teve como objetivo identificar os fatores que motivam os educadores a buscarem a continuidade da formação profissional e qual a contribuição dessa continuidade para o desenvolvimento de competências reflexivas, autônomas, críticas, políticas e humanas, e o aperfeiçoamento de sua prática pedagógica. A metodologia utilizada foi a pesquisa de campo e bibliográfica, contemplando a aplicação de questionários, entrevistas e observações participantes em sala de aula, junto a 58 educadores de duas escolas da rede pública municipal de educação de Aracaju. Trata-se de um estudo de caso. Os dados da pesquisam revelaram que os esforços esparsos e fragmentados que têm assinalado a formação continuada oferecida pelos órgãos próprios do sistema educacional tendem a ser superados por um modelo formativo centrado nas necessidades da própria escola, desde a disponibilidade de recursos materiais, tecnológicos e humanos até as metodologias de ensino e de aprendizagem. Conclui tendo a escola como o espaço formativo por excelência de educadores e educandos.

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O trabalho apresentado é decorrente do Projeto de Intervenção realizado no âmbito do Curso de 2º Ciclo em Educação Especial – domínio cognitivo e motor, da Universidade Lusófona de Humanidades e Tecnologias. Resumo A referida intervenção contempla a minimização das dificuldades apresentadas por uma menina a nível da leitura e escrita e da sua socialização, numa perspetiva inclusiva. M. é o nome fictício da aluna alvo da intervenção. Atualmente, frequenta o 3º ano de escolaridade numa escola pública, em Lisboa área da sua residência. A revisão da literatura vai sustentar e facilitar a compreensão clara e concisa da intervenção realizada e das posições defendidas sobre esta matéria. Deste modo, são tratados temas no âmbito da exclusão social e escolar, da escola Inclusiva e dos obstáculos que ainda encontramos nas escolas, dos preconceitos, dos alunos com necessidades educativas especiais, das adaptações curriculares, da aprendizagem cooperativa e diferenciação pedagógica, referimo-nos ainda às dificuldades de aprendizagem e, por último, à comunicação e à linguagem oral e escrita. Para obter informações sobre a M. e sobre o contexto da intervenção, bem como sobre todo o seu processo de inclusão escolar, utilizamos como suporte metodológico, a pesquisa documental, as entrevistas semi-diretivas à professora titular de turma e à professora de ensino especial, a observação naturalista, a sociometria e as notas de campo para se poder complementar as informações. A planificação global da intervenção foi elaborada a partir do relacionamento/ cruzamento dos dados que resultaram da análise da informação recolhida. Para uma intervenção fundamentada caracterizamos inicialmente o seu contexto escolar e familiar e posteriormente a M. Os princípios orientadores da intervenção realizada, assentam numa perspetiva de investigação para a ação, e tiveram presentes os objetivos definidos para a M. As atividades foram realizadas, numa perspetiva de aprendizagem muito estruturada, muito refletida e avaliada durante todo o processo, implicando todos os intervenientes. Esta intervenção, levou-nos a estimular práticas educativas, diferenciadas e inclusivas na turma, com a professora titular dessa turma e com a professora do ensino especial com os colegas da M.

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The clustering in time (seriality) of extratropical cyclones is responsible for large cumulative insured losses in western Europe, though surprisingly little scientific attention has been given to this important property. This study investigates and quantifies the seriality of extratropical cyclones in the Northern Hemisphere using a point-process approach. A possible mechanism for serial clustering is the time-varying effect of the large-scale flow on individual cyclone tracks. Another mechanism is the generation by one parent cyclone of one or more offspring through secondary cyclogenesis. A long cyclone-track database was constructed for extended October March winters from 1950 to 2003 using 6-h analyses of 850-mb relative vorticity derived from the NCEP NCAR reanalysis. A dispersion statistic based on the varianceto- mean ratio of monthly cyclone counts was used as a measure of clustering. It reveals extensive regions of statistically significant clustering in the European exit region of the North Atlantic storm track and over the central North Pacific. Monthly cyclone counts were regressed on time-varying teleconnection indices with a log-linear Poisson model. Five independent teleconnection patterns were found to be significant factors over Europe: the North Atlantic Oscillation (NAO), the east Atlantic pattern, the Scandinavian pattern, the east Atlantic western Russian pattern, and the polar Eurasian pattern. The NAO alone is not sufficient for explaining the variability of cyclone counts in the North Atlantic region and western Europe. Rate dependence on time-varying teleconnection indices accounts for the variability in monthly cyclone counts, and a cluster process did not need to be invoked.

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Problem structuring methods or PSMs are widely applied across a range of variable but generally small-scale organizational contexts. However, it has been argued that they are seen and experienced less often in areas of wide ranging and highly complex human activity-specifically those relating to sustainability, environment, democracy and conflict (or SEDC). In an attempt to plan, track and influence human activity in SEDC contexts, the authors in this paper make the theoretical case for a PSM, derived from various existing approaches. They show how it could make a contribution in a specific practical context-within sustainable coastal development projects around the Mediterranean which have utilized systemic and prospective sustainability analysis or, as it is now known, Imagine. The latter is itself a PSM but one which is 'bounded' within the limits of the project to help deliver the required 'deliverables' set out in the project blueprint. The authors argue that sustainable development projects would benefit from a deconstruction of process by those engaged in the project and suggest one approach that could be taken-a breakout from a project-bounded PSM to an analysis that embraces the project itself. The paper begins with an introduction to the sustainable development context and literature and then goes on to illustrate the issues by grounding the debate within a set of projects facilitated by Blue Plan for Mediterranean coastal zones. The paper goes on to show how the analytical framework could be applied and what insights might be generated.

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Accurate estimation of the soil water balance (SWB) is important for a number of applications (e.g. environmental, meteorological, agronomical and hydrological). The objective of this study was to develop and test techniques for the estimation of soil water fluxes and SWB components (particularly infiltration, evaporation and drainage below the root zone) from soil water records. The work presented here is based on profile soil moisture data measured using dielectric methods, at 30-min resolution, at an experimental site with different vegetation covers (barley, sunflower and bare soil). Estimates of infiltration were derived by assuming that observed gains in the soil profile water content during rainfall were due to infiltration. Inaccuracies related to diurnal fluctuations present in the dielectric-based soil water records are resolved by filtering the data with adequate threshold values. Inconsistencies caused by the redistribution of water after rain events were corrected by allowing for a redistribution period before computing water gains. Estimates of evaporation and drainage were derived from water losses above and below the deepest zero flux plane (ZFP), respectively. The evaporation estimates for the sunflower field were compared to evaporation data obtained with an eddy covariance (EC) system located elsewhere in the field. The EC estimate of total evaporation for the growing season was about 25% larger than that derived from the soil water records. This was consistent with differences in crop growth (based on direct measurements of biomass, and field mapping of vegetation using laser altimetry) between the EC footprint and the area of the field used for soil moisture monitoring. Copyright (c) 2007 John Wiley & Sons, Ltd.

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A multi-scale framework for decision support is presented that uses a combination of experiments, models, communication, education and decision support tools to arrive at a realistic strategy to minimise diffuse pollution. Effective partnerships between researchers and stakeholders play a key part in successful implementation of this strategy. The Decision Support Matrix (DSM) is introduced as a set of visualisations that can be used at all scales, both to inform decision making and as a communication tool in stakeholder workshops. A demonstration farm is presented and one of its fields is taken as a case study. Hydrological and nutrient flow path models are used for event based simulation (TOPCAT), catchment scale modelling (INCA) and field scale flow visualisation (TopManage). One of the DSMs; The Phosphorus Export Risk Matrix (PERM) is discussed in detail. The PERM was developed iteratively as a point of discussion in stakeholder workshops, as a decision support and education tool. The resulting interactive PERM contains a set of questions and proposed remediation measures that reflect both expert and local knowledge. Education and visualisation tools such as GIS, risk indicators, TopManage and the PERM are found to be invaluable in communicating improved farming practice to stakeholders. (C) 2008 Elsevier Ltd. All rights reserved.

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A generic Nutrient Export Risk Matrix (NERM) approach is presented. This provides advice to farmers and policy makers on good practice for reducing nutrient loss and is intended to persuade them to implement such measures. Combined with a range of nutrient transport modelling tools and field experiments, NERMs can play an important role in reducing nutrient export from agricultural land. The Phosphorus Export Risk Matrix (PERM) is presented as an example NERM. The PERM integrates hydrological understanding of runoff with a number of agronomic and policy factors into a clear problem-solving framework. This allows farmers and policy makers to visualise strategies for reducing phosphorus loss through proactive land management. The risk Of Pollution is assessed by a series of informed questions relating to farming intensity and practice. This information is combined with the concept of runoff management to point towards simple, practical remedial strategies which do not compromise farmers' ability to obtain sound economic returns from their crop and livestock.

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Partnerships are complex, diverse and subtle relationships, the nature of which changes with time, but they are vital for the functioning of the development chain. This paper reviews the meaning of partnership between development institutions as well as some of the main approaches taken to analyse the relationships. The latter typically revolve around analyses based on power, discourse, interdependence and functionality. The paper makes the case for taking a multianalytical approach to understanding partnership but points out three problem areas: identifying acceptable/unacceptable trade-offs between characteristics of partnership, the analysis of multicomponent partnerships (where one partner has a number of other partners) and the analysis of long-term partnership. The latter is especially problematic for long-term partnerships between donors and field agencies that share an underlying commitment based on religious beliefs. These problems with current methods of analysing partnership are highlighted by focusing upon the Catholic Church-based development chain, linking donors in the North (Europe) and their field partners in the South (Abuja Ecclesiastical Province, Nigeria). It explores a narrated history of a relationship with a single donor spanning 35 years from the perspective of one partner (the field agency).

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In this paper we pledge that physically based equations should be combined with remote sensing techniques to enable a more theoretically rigorous estimation of area-average soil heat flux, G. A standard physical equation (i.e. the analytical or exact method) for the estimation of G, in combination with a simple, but theoretically derived, equation for soil thermal inertia (F), provides the basis for a more transparent and readily interpretable method for the estimation of G; without the requirement for in situ instrumentation. Moreover, such an approach ensures a more universally applicable method than those derived from purely empirical studies (employing vegetation indices and albedo, for example). Hence, a new equation for the estimation of Gamma(for homogeneous soils) is discussed in this paper which only requires knowledge of soil type, which is readily obtainable from extant soil databases and surveys, in combination with a coarse estimate of moisture status. This approach can be used to obtain area-averaged estimates of Gamma(and thus G, as explained in paper II) which is important for large-scale energy balance studies that employ aircraft or satellite data. Furthermore, this method also relaxes the instrumental demand for studies at the plot and field scale (no requirement for in situ soil temperature sensors, soil heat flux plates and/or thermal conductivity sensors). In addition, this equation can be incorporated in soil-vegetation-atmosphere-transfer models that use the force restore method to update surface temperatures (such as the well-known ISBA model), to replace the thermal inertia coefficient.

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The beds of active ice streams in Greenland and Antarctica are largely inaccessible, hindering a full understanding of the processes that initiate, sustain and inhibit fast ice flow in ice sheets. Detailed mapping of the glacial geomorphology of palaeo-ice stream tracks is, therefore, a valuable tool for exploring the basal processes that control their behaviour. In this paper we present a map that shows detailed glacial geomorphology from a part of the Dubawnt Lake Palaeo-Ice Stream bed on the north-western Canadian Shield (Northwest Territories), which operated at the end of the last glacial cycle. The map (centred on 63 degrees 55 '' 42'N, 102 degrees 29 '' 11'W, approximate scale 1:90,000) was compiled from digital Landsat Enhanced Thematic Mapper Plus satellite imagery and digital and hard-copy stereo-aerial photographs. The ice stream bed is dominated by parallel mega-scale glacial lineations (MGSL), whose lengths exceed several kilometres but the map also reveals that they have, in places, been superimposed with transverse ridges known as ribbed moraines. The ribbed moraines lie on top of the MSGL and appear to have segmented the individual lineaments. This indicates that formation of the ribbed moraines post-date the formation of the MSGL. The presence of ribbed moraine in the onset zone of another palaeo-ice stream has been linked to oscillations between cold and warm-based ice and/or a patchwork of cold-based areas which led to acceleration and deceleration of ice velocity. Our hypothesis is that the ribbed moraines on the Dubawnt Lake Ice Stream bed are a manifestation of the process that led to ice stream shut-down and may be associated with the process of basal freeze-on. The precise formation of ribbed moraines, however, remains open to debate and field observation of their structure will provide valuable data for formal testing of models of their formation.

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The aim of the study was to establish and verify a predictive vegetation model for plant community distribution in the alti-Mediterranean zone of the Lefka Ori massif, western Crete. Based on previous work three variables were identified as significant determinants of plant community distribution, namely altitude, slope angle and geomorphic landform. The response of four community types against these variables was tested using classification trees analysis in order to model community type occurrence. V-fold cross-validation plots were used to determine the length of the best fitting tree. The final 9node tree selected, classified correctly 92.5% of the samples. The results were used to provide decision rules for the construction of a spatial model for each community type. The model was implemented within a Geographical Information System (GIS) to predict the distribution of each community type in the study site. The evaluation of the model in the field using an error matrix gave an overall accuracy of 71%. The user's accuracy was higher for the Crepis-Cirsium (100%) and Telephium-Herniaria community type (66.7%) and relatively lower for the Peucedanum-Alyssum and Dianthus-Lomelosia community types (63.2% and 62.5%, respectively). Misclassification and field validation points to the need for improved geomorphological mapping and suggests the presence of transitional communities between existing community types.

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Using topographic data collected by radar interferometry, stereo-photogrammetry, and field survey we have measured the changing surface of Volcan Arenal in Costa Rica over the period from 1980 to 2004. During this time this young volcano has mainly effused basaltic andesite lava, continuing the activity that began in 1968. Explosive products form only a few percent of the volumetric output. We have calculated digital elevation models for the years 1961, 1988 and 1997 and modified existing models for 2000 and 2004. From these we have estimated the volume of lava effused and coupled this with the data presented by an earlier study for 1968-1980. We find that a dense rock equivalent volume of 551 M m(3) was effused from 1968 to 2004. The dense rock equivalent effusion rate fell from about 2 m(3) s(-1) to about 0.1-0.2 m(3) s(-1) over the same period, with an average rate of about 0.5 m(3) s(-1). Between 1980 and 2004, the average effusion rate was 0.36 m(3) s(-1), a similar rate to that measured between 1974 and 1980. There have been two significant deviations from this long-term rate. The effusion rate increased from 1984 to 1991, at the same time as explosivity increased. After a period of moderate effusion rates in the 1990s, the rate fell to lower levels around 1999. (c) 2006 Elsevier B.V. All rights reserved.