999 resultados para Angola Benguela Front


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Currently, it is widely perceived among the English as a Foreign Language (EFL) teaching professionals, that motivation is a central factor for success in language learning. This work aims to examine and raise teachers’ awareness about the role of assessment and feedback in the process of language teaching and learning at polytechnic school in Benguela to develop and/or enhance their students’ motivation for learning. Hence the paper defines and discusses the key terms and, the techniques and strategies for an effective feedback provision in the context under study. It also collects data through the use of interview and questionnaire methods, and suggests the assessment and feedback types to be implemented at polytechnic school in Benguela

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A violência doméstica em Angola – mormente em Benguela não é um problema novo. Mas nos últimos dez anos, este fenómeno muda de figura, pois, toma um carácter cada vez mais perturbador já que frequentemente resulta em mutilações e não raras vezes em vítimas mortais. Assim, este trabalho de investigação procura esclarecer as causas, os factores sobretudo, os de ordem sociocultural que estejam na base do incremento da violência doméstica no seio familiar nestes últimos anos. Deste modo, este trabalho consiste numa análise sociocultural do problema da violência doméstica em Benguela. E os resultados alcançados nesta investigação revelam que, os factores que estão na base desta alteração comportamental dos elementos da família são: a desagregação da família tradicional, desestruturação socioeconómica das famílias, a desorientação cultural e axiológica - deturpação da escala de valores. Estes factores constituem a consequência do conflito armado que o país viveu durante cerca de três décadas. Por outro lado, emergem outros factores resultantes da dinâmica social como, a modernização da vida social, a emancipação da mulher - sua promoção social e profissional - a influência dos meios de comunicação social e o intercâmbio cultural com vários povos de outras culturas, e ainda outros, como os desajustes de carácter educacional que afecta o pensar e o carácter das novas gerações. Estes factores não são um registo habitual da história deste povo, mas foram favorecidos pelas vicissitudes do tempo. Na verdade, o conflito armado foi o principal responsável na destruição dos valores que serviam de base a boa convivência dos elementos das famílias angolanas. Pois, deturpou a escala de valores, deixou sequelas de vária ordem o que resulta em frustrações que frequentemente desorientam a reflexão crítica perante os problemas quotidianos, criando assim comportamentos violentos. Desta feita, esta investigação com os conhecimentos que traz á luz, constitui uma contribuição para o ponto de partida para a tomada de medidas por quem é de direito para lutar contra este flagelo, que é na realidade um mal social.

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Nitrogen fixation data from the cruise number MSM18/5 with research vessel "Maria S. Merian" from 22.08.-20.09.2011 (from Walvis Bay to Walvis Bay) in front of Angola and northern Namibia. Samples taken by CTD- rosette sampler from different depths and incubated in glass bottles (535 ml) at light intensities that resemble the in situ light intensities of the sampling depth after 15N2 gas was injected to the sample. After the incubation time of 6 hours, the complete bottle content was filtered onto a pre-combusted Whatman GF/F filter. Filters were frozen, transported to the institute on dry ice and measured in a mass spectrometer for Delta 15N. The principle of the method was described by Montoya et al. (1996) and calculation was done according to their spread sheet. From the data of the single depths, the nitrogen fixation per square meter within the upper 40 m of the water column was calculated. The methods are described in detail in a paper submitted by Wasmund et al. in 2014 to be printed in 2015. Some results are surprisingly below zero. This occurs if the Delta 15N of the blank is higher than the measurement after incubation. It indicates that no nitrogen fixation occurred. Due to natural variability, the variability of the nitrogen fixation data is high. In an overall estimate, also over several cruises, negative and positive values compensate more or less, suggesting that nitrogen fixation is insignificant in the waters in front of northern Namibia and southern Angola.

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Nitrogen fixation data from the cruise number MSM17/3 with research vessel "Maria S. Merian" from 30.01.-10.02.2011 (= "leg a" from Walvis Bay to Walvis Bay) in front of Namibia. Samples taken by CTD- rosette sampler from different depths and incubated in glass bottles (535 ml) at light intensities that resemble the in situ light intensities of the sampling depth after 15N2 gas was injected to the sample. After the incubation time of 6-8 hours, the complete bottle content was filtered onto a pre-combusted Whatman GF/F filter. Filters were frozen, transported to the institute on dry ice and measured in a mass spectrometer for Delta 15N. The principle of the method was described by Montoya et al. (1996) and calculation was done according to their spread sheet. From the data of the single depths, the nitrogen fixation per square meter within the upper 40 m of the water column was calculated. The methods are described in detail in a paper submitted by Wasmund et al. in 2014 to be printed in 2015. Some results are surprisingly below zero. This occurs if the Delta 15N of the blank is higher than the measurement after incubation. It indicates that no nitrogen fixation occurred. Due to natural variability, the variability of the nitrogen fixation data is high. In an overall estimate, also over several cruises, negative and positive values compensate more or less, suggesting that nitrogen fixation is insignificant in the waters in front of northern Namibia and southern Angola.

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Nitrogen fixation data from the cruise number M100 with research vessel "Meteor" from 01.09.-01.10.2013 (1st leg from Walvis Bay to Walvis Bay) in front of Namibia. Samples taken by CTD- rosette sampler from different depths and incubated in glass bottles (270-1070 ml) at light intensities that resemble the in situ light intensities of the sampling depth after 15N2 gas was injected to the sample. After the incubation time of 24 hours, the complete bottle content was filtered onto a pre-combusted Whatman GF/F filter. Filters were frozen, transported to the institute on dry ice and measured in a mass spectrometer for Delta 15N. The principle of the method was described by Montoya et al. (1996) and calculation was done according to their spread sheet. From the data of the single depths, the nitrogen fixation per square meter within the upper 40 m of the water column was calculated. The methods are described in detail in a paper submitted by Wasmund et al. in 2014 to be printed in 2015. Some results are surprisingly below zero. This occurs if the Delta 15N of the blank is higher than the measurement after incubation. It indicates that no nitrogen fixation occurred. Due to natural variability, the variability of the nitrogen fixation data is high. In an overall estimate, also over several cruises, negative and positive values compensate more or less, suggesting that nitrogen fixation is insignificant in the waters in front of northern Namibia and southern Angola.

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Nitrogen fixation data from the cruise number M103/2 with research vessel "Meteor" from 21.01.-11.02.2014 (second leg from Walvis Bay to Walvis Bay) in front of Namibia. Samples taken by CTD- rosette sampler from different depths and incubated in glass bottles (535 ml) at light intensities that resemble the in situ light intensities of the sampling depth after 15N2 gas was injected to the sample. After the incubation time of 24 hours, the complete bottle content was filtered onto a pre-combusted Whatman GF/F filter. Filters were frozen, transported to the institute on dry ice and measured in a mass spectrometer for Delta15N. The principle of the method was described by Montoya et al. (1996) and calculation was done according to their spread sheet. From the data of the single depths, the nitrogen fixation per square meter within the upper 40 m of the water column was calculated. The methods are described in detail in a paper submitted by Wasmund et al. in 2014 to be printed in 2015. Some results are surprisingly below zero. This occurs if the Delta15N of the blank is higher than the measurement after incubation. It indicates that no nitrogen fixation occurred. Due to natural variability, the variability of the nitrogen fixation data is high. In an overall estimate, also over several cruises, negative and positive values compensate more or less, suggesting that nitrogen fixation is insignificant in the waters in front of northern Namibia and southern Angola.

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Nitrogen fixation data from the cruise number MSM18/4 with research vessel "Maria S. Merian" from 24.07.-20.08.2011 (from Libreville to Walvis Bay) in front of Angola and northern Namibia. Samples taken by CTD- rosette sampler from different depths and incubated in glass bottles (535 ml) at light intensities that resemble the in situ light intensities of the sampling depth after Delta 15 N2 gas was injected to the sample. After the incubation time of 6 hours, the complete bottle content was filtered onto a pre-combusted Whatman GF/F filter. Filters were frozen, transported to the institute on dry ice and measured in a mass spectrometer for Delta15N. The principle of the method was described by Montoya et al. (1996) and calculation was done according to their spread sheet. From the data of the single depths, the nitrogen fixation per square meter within the upper 40 m of the water column was calculated. The methods are described in detail in a paper submitted by Wasmund et al. in 2014 to be printed in 2015. Some results are surprisingly below zero. This occurs if the Delta15N of the blank is higher than the measurement after incubation. It indicates that no nitrogen fixation occurred. Due to natural variability, the variability of the nitrogen fixation data is high. In an overall estimate, also over several cruises, negative and positive values compensate more or less, suggesting that nitrogen fixation is insignificant in the waters in front of northern Namibia and southern Angola.

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A família é o meio natural em que a criança começa sua vida e sua aprendizagem básica por meio de uma série de estímulos e de vivências que a condicionam profundamente ao longo de toda a sua existência. A escola representa o espaço em que a criança consolida a sua aprendizagem e se prepara para vida futura. A cooperação entre família e escola constitui o pilar fundamental na construção de um processo de ensino aprendizagem de qualidade, sobre tudo para crianças com Necessidades Educativas Especiais (N.E.E). Com base nestes pressupostos o objetivo geral da presente dissertação de natureza qualitativa é aferir o impato do envolvimento familiar no processo de ensino aprendizagem dos alunos com necessidades educativas especiais na cidade de BenguelaAngola, através de inquéritos e entrevistas aplicadas a uma amostra constituída pelos familiares dos alunos, os respetivos alunos, professores e antigos gestores da única escola de Ensino Especial da cidade de Benguela. Os resultados do estudo revelaram um fraco grau de envolvimento familiar, tendo em conta as orientações da Lei, nº 13/01, Lei de Bases do Sistema de Educação (L.B.S.E), e o Decreto Presidencial nº 20/11, sobre o Estatuto da Modalidade de Educação Especial que recomendam a participação indispensável da família na elaboração dos programas (E.M.E.E) educativos dos alunos com N.E.E, bem como os resultados de estudos que ressaltam a importância da relação escola e família para melhoria da qualidade do Ensino Especial em Angola. A dissertação constitui uma abordagem pioneira no contexto em que se insere e o seu valor prático é determinado pelo contributo que os seus resultados podem aportar a compreensão e melhoria da qualidade de ensino e das relações familiares dos alunos com N.E.E num contexto fortemente marcado por barreiras culturais e tradicionais.

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Processes of enrichment, concentration and retention are thought to be important for the successful recruitment of small pelagic fish in upwelling areas, but are difficult to measure. In this study, a novel approach is used to examine the role of spatio-temporal oceanographic variability on recruitment success of the Northern Benguela sardine Sardinops sagax. This approach applies a neural network pattern recognition technique, called a self-organising map (SOM), to a seven-year time series of satellite-derived sea level data. The Northern Benguela is characterised by quasi-perennial upwelling of cold, nutrient-rich water and is influenced by intrusions of warm, nutrient-poor Angola Current water from the north. In this paper, these processes are categorised in terms of their influence on recruitment success through the key ocean triad mechanisms of enrichment, concentration and retention. Moderate upwelling is seen as favourable for recruitment, whereas strong upwelling, weak upwelling and Angola Current intrusion appear detrimental to recruitment success. The SOM was used to identify characteristic patterns from sea level difference data and these were interpreted with the aid of sea surface temperature data. We found that the major oceanographic processes of upwelling and Angola Current intrusion dominated these patterns, allowing them to be partitioned into those representing recruitment favourable conditions and those representing adverse conditions for recruitment. A marginally significant relationship was found between the index of sardine recruitment and the frequency of recruitment favourable conditions (r super(2) = 0.61, p = 0.068, n = 6). Because larvae are vulnerable to environmental influences for a period of at least 50 days after spawning, the SOM was then used to identify windows of persistent favourable conditions lasting longer than 50 days, termed recruitment favourable periods (RFPs). The occurrence of RFPs was compared with back-calculated spawning dates for each cohort. Finally, a comparison of RFPs with the time of spawning and the index of recruitment showed that in years where there were 50 or more days of favourable conditions following spawning, good recruitment followed (Mann-Whitney U-test: p = 0.064, n = 6). These results show the value of the SOM technique for describing spatio-temporal variability in oceanographic processes. Variability in these processes appears to be an important factor influencing recruitment in the Northern Benguela sardine, although the available data time series is currently too short to be conclusive. Nonetheless, the analysis of satellite data, using a neural network pattern-recognition approach, provides a useful framework for investigating fisheries recruitment problems.

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Hoje, nenhuma língua está livre de influências de outra língua; fruto da facilidade com que os homens interagem. Uma das consequências desta interacção reside na influência da língua de uns sobre a de outros, o que geralmente ocorre com interferência da língua materna (LM) do indivíduo na sua segunda língua (LS). Para abordar este fenómeno realizámos em Benguela um estudo que consistiu no levantamento e análise de algumas expressões activas no dia-a-dia dos Benguelenses para detectar elementos de interferência do Umbundu no Português, como resultado da coabitação das duas línguas e desta forma contribuir para estudos linguísticos que visem esclarecer os processos inerentes a coabitação entre linguas africanas e europeias. Para o efeito, levamos a cabo uma análise das expressões inventariadas para melhor compreender as razões que concorrem para ocorrência de tais interferências, as quais se converteram num dos principias elementos na caracterização do português falado naquela região de Angola. Assim, na nossa condição de docentes, se torna absolutamente necessário identificar estes fenómenos, já que eles constituem parte integrante da nossa tarefa quotidiana de orientação das aprendizagens em Português.

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Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)

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Fundação de Amparo à Pesquisa do Estado de São Paulo (FAPESP)

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A feature of Pliocene climate is the occurrence of "permanent El Niño-like" or "El Padre" conditions in the Pacific Ocean. From the analysis of sediment cores in the modern northern Benguela upwelling, we show that the mean oceanographic state off Southwest Africa during the warm Pliocene epoch was also analogous to that of a persistent Benguela "El Niño". At present these events occur when massive southward flows of warm and nutrient-poor waters extend along the coasts of Angola and Namibia, with dramatic effects on regional marine ecosystems and rainfall. We propose that the persistent warmth across the Pliocene in the Benguela upwelling ended synchronously with the narrowing of the Indonesian seaway, and the early intensification of the Northern Hemisphere Glaciations around 3.0-3.5 Ma. The emergence of obliquity-related cycles in the Benguela sea surface temperatures (SST) after 3 Ma highlights the development of strengthened links to high latitude orbital forcing. The subsequent evolution of the Benguela upwelling system was characterized by the progressive intensification of the meridional SST gradients, and the emergence of the 100 ky cycle, until the modern mean conditions were set at the end of the Mid Pleistocene transition, around 0.6 Ma. These findings support the notion that the interplay of changes in the depth of the global thermocline, atmospheric circulation and tectonics preconditioned the climate system for the end of the warm Pliocene epoch and the subsequent intensification of the ice ages.