As práticas de supervisão e liderança dos coordenadores do departamento de Matemática e Ciências Experimentais na harmonização de um emergente mega departamento

A escola é uma organização cuja missão se traduz no aperfeiçoamento das práticas pedagógicas e na melhoria da qualidade do ensino e da aprendizagem (Lima, 2008) muito embora se veja confrontada diariamente com vários desafios de ordem política, social, económica e ideológica que obrigam todos os agentes educativos a encontrar formas para os ultrapassar (Nóvoa, 2009). Atualmente, o sucesso dos mega agrupamentos recentemente criados pela tutela emerge como um enorme desafio quanto à organização e nova dinâmica da escola como instituição, realçando o papel fundamental dos promotores e harmonizadores da mudança que constituem os órgãos de gestão e nomeadamente os de gestão intermédia, representados pelos coordenadores dos departamentos curriculares. Com efeito, é a eles que cabe o difícil e delicado papel de unir realidades diferentes coordenando-as, orientando-as e harmonizando-as respeitando simultaneamente as diferentes ambições e expetativas dos alunos quanto ao seu futuro, as culturas escolares e os professores que de um momento para o outro são obrigados a adaptarem-se a contextos sociais ainda mais heterogéneos. Desta forma, a tarefa dos coordenadores de departamento vê-se substancialmente acrescida e dificultada não só pelo aumento do número de docentes que constitui o departamento mas, mais ainda pela explosão das diferenças que surgem entre os vários docentes, as suas práticas e o universo de alunos do mega agrupamento que se deve constituir numa única comunidade escolar (Sergiovanni, 2004). No intuito de realçar o papel dos coordenadores na promoção da integração das duas escolas e na implementação da efetiva colaboração entre coordenadores e grupos disciplinares, objetivo geral deste trabalho, é proposta uma ação de formação na modalidade de projeto. Esta proposta resulta da análise das entrevistas realizadas aos coordenadores do mega departamento de Matemática e Ciências Experimentais do mega agrupamento onde a autora deste estudo exerce funções, e através das quais se procurava responder à questão: qual o papel dos coordenadores na promoção de integração das duas escolas e na implementação da efetiva colaboração entre os coordenadores e grupos disciplinares.

A universidade e o seu contributo para o desenvolvimento da União Europeia

O trabalho presente é uma investigação sobre a Universidade sua génese e diversidade, caminhada e desenvolvimento, prosperidade em crescimento, papel cultural e fonte de conhecimento seus momentos de glória, seu de impasse e de crise e tentativas para devolver a glória e prestigio de outrora. Nasceu na Europa Meridional com o título de “Studium Generale”. Não nasceu nem “ex abrupto” nem “ex nihilo”, a sua génese remonta às escolas religiosas dos conventos e catedrais onde se conservavam os documentos da cultura greco – latina que mais tarde imperará na Europa sob o antropocentrismo, em oposição ao Teocentrismo. O “Studium General” nasce sobre o patrocínio da Igreja que mantinha como disciplinas principais nestes centros a Teologia e Filosofia, cuja leccionação é circunscrita a poucas Escolas e professores escolhidos. Acorriam à Universidade alunos de todos os cantos da Europa, evidentemente com meios e frades alunos pobres e para os frades criaram-se colégios que os acolhiam e protegiam. A reunião de estudantes devido a disturbios gerou ambiente controverso e obrigou as autoridades governamentais a medidas quer de contenção quer de protecção a residentes e forasteiros. O estudante era um estrangeiro que se deslocava no espaço europeu consoante a fama dos professores. A língua latina foi o veiculo de ligação e comunicação. Pouco a pouco os estados foram-se dando conta do valor da universidade e dos seus ensinamentos e disputavam com a Igreja o seu patrocínio. A Universidade contribui para o desenvolvimento dos Estados a nível administrativo, do direito, da criação de leis dando aos Estados uma maior e melhor organização no seu desenvolvimento. As Universidades concediam graus académicos, sendo o maior o de doutor. Todos esperavam o apoio do saber académico e científico para vencer a luta pela existência. O sistema escolático criticado pelo humanismo deu origem a novos modelos de universidade que surgiram com a supervisão dos Estados. Os modelos a partir do século XIX, são: ingês, alemão, americano, francês e russo. A universidade passa a ser o lugar do ensino superior, com o repúdio ao tradicinal e a investigação passa a fazer parte do papel da universidade. Em Portugal criou-se estruturas de apoio à formação de professores especialmente o sector de ciência e educação. Tardiamente a União Europeia dá atenção à educação criando programas como o Sócrates cujas acções são Comenios, Erasmus, Grundvig, Língua e Minerva. A mobilidade estudantil torna-se realidade na Europa e a flexibilidade na educação. A função da universidade actual ocupa-se do sector industrial e pós industrial da sociedade de informação, economia e empresa. Universidade como serviço público e mercado. Foi pena que a União Europeia, não reconhecesse ao Homem a centralidade de que tem direito, e esquecesse que sem o homem não há desenvolvimento nem criatividade. Estruturou-se a economia e a política obliterou a educação, a cultura, a formação, isto é um castelo construído sobre areia. Relembrando Antero cabe dizer: “Abrem-se as portas de ouro com fragor Mas dentro encontro só cheiro de dor Silêncio e escuridão nada mais”. Hoje a nossa Universidade é um problema. O seu caminho terá de ser o da cultura e a da educação. Tem de ser vista como poder em época de crise e o permanente primeiro que o transitório. Donde a necessidade de uma gestão de qualidade e de uma educação permanente.

Anatomías contrariadas: la representación del cuerpo en la literatura sobre los Andes (Estudios)

La autora analiza tres textos latinoamericanos que muestran construcciones del imaginario andino, extendidas a ciertos estereotipos sobre la corporalidad andina: frágil, dolorida, para la cual la esperanza de liberación radica en un azar. En «Boletín y Elegía de las Mitas», César Dávila presenta una versión del cuerpo indio «exclusivamente centrada en la vejación de lo anatómico» (de su cabeza y genitales, de órganos tan profundos como el corazón y el esqueleto), con lo que el cuerpo desnudo y forzado se convierte en ajeno. En «El sueño del Pongo», de José María Arguedas, el cuerpo del indio oprimido es diminuto, y porta una «gestualidad comprimida que se pone en juego a partir de posturas humilladas». Pese al final aparentemente optimista de ambos textos, se trata de productos culturales que cumplen un rol en el ejercicio de control social. En «Barraquera», de José de la Cuadra, el cuerpo de esta mujer es fundado a partir de violaciones, muertes y migraciones forzadas: habituado a sufrir y callar, para este cuerpo el dolor se convierte en la única vía posible de acceso al placer. Se remarca que el tiempo cronológico de los tres relatos es el de la espera, el tiempo del destino. Para estos cuerpos-lugares siempre vulnerables y violentados, burlados o invisibilizados, lo fatal fundamentaría un cierre de lo histórico.

¿Complicamos demasiado las cosas en los contratos financieros internacionales? (Tema Central)

Este es un momento de gran agitación dentro de los mercados de crédito. Durante los últimos seis meses, decenas de billones de dólares de inversiones en papeles o instrumentos de deuda han tenido que ser castigados. Poderosas instituciones financieras han caído. Algunas de ellas se han visto obligadas a vender importantes porciones de su participación accionarial a inversionistas no convencionales con el fin de mantener los porcentajes mínimos de capital requerido.

Los “enganchados”. La formación de grupos armados en la Costa del Ecuador a inicios del siglo XIX (Estudios)

Basado en fuentes primarias (epistolarios), el artículo ofrece una aproximación al proceso de formación de grupos armados irregulares, en la provincia de Manabí, a inicios del siglo XIX, como consecuencia de la disputa por el poder y el control del monopolio de la violencia, en el marco de construcción del nuevo régimen republicano. En esta región periférica del Estado central, la sociedad se torna violenta cuando es presionada tanto por el poder estatal, como por los caudillos locales que pretenden formar parte de las estructuras de poder local por medio del reclutamiento forzoso para engrosar las filas de milicias y grupos armados.

El legado de Cádiz: ciudadanía y cultura política en la Gobernación de Cuenca, 1812-1814 (Estudios)

Este trabajo analiza el legado de las Cortes de Cádiz y de la Constitución de 1812 en Cuenca entre 1812 y 1814. Estudia los principales cambios políticos relacionados con los derechos de diversos actores sociales, así como el rompimiento de antiguas formas de relación social. Los cambios políticos se relacionaron con la introducción de nuevos conceptos y prácticas como ciudadanía, soberanía, elección y representación, tanto en el mundo criollomestizo como en el indígena (población cañari) de la provincia. Se analiza la abolición del tributo indígena, el servicio personal y la mita, además se estudian algunos cambios administrativopolíticos como la creación de los ayuntamientos constitucionales, las diputaciones provinciales y nacionales.

Central Banks in Times of Crisis: The FED vs. the ECB. CEPS Policy Brief No. 276, 11 July 2012,

Different economic and financial structures require different crisis responses. Different crises also require different tools and resources. The first ‘stage’ of the financial crisis (2007-09) was similar on both sides of the Atlantic, and the response was also quite similar. The second stage of the crisis is unique to the euro area. Increasing financial disintegration within the region has forced the ECB to become the central counterparty for the entire cross-border banking market and to intervene in the sovereign bond market of some stressed countries. The actions undertaken by the European Central Bank (ECB), however, have not always represented the best response, in terms of effectiveness, consistency and transparency. This is especially true for the Securities Markets Programme (SMP): by de facto imposing its absolute seniority during the Greek PSI (private sector involvement), the ECB has probably killed its future effectiveness.

The implications for the EU and national budgets of the use of EU instruments for macro-financial stability. CEPS Special Report, 4 September 2012

The euro crisis has forced member states and the EU institutions to create a series of new instruments to safeguard macro-financial stability of the Union. This study describes the status of existing instruments, the role of the European Parliament and how the use of the instruments impinges on the EU budget also through their effects on national budgets. In addition, it presents a survey of other possible instruments that have been proposed in recent years (e.g. E-bonds and eurobonds), in order to provide an assessment of how EU macro-financial stability assistance could evolve in the future and what could be its impact on EU public finances.

The diabatic contour advective semi-Lagrangian model

This article describes a novel algorithmic development extending the contour advective semi-Lagrangian model to include nonconservative effects. The Lagrangian contour representation of finescale tracer fields, such as potential vorticity, allows for conservative, nondiffusive treatment of sharp gradients allowing very high numerical Reynolds numbers. It has been widely employed in accurate geostrophic turbulence and tracer advection simulations. In the present, diabatic version of the model the constraint of conservative dynamics is overcome by including a parallel Eulerian field that absorbs the nonconservative ( diabatic) tendencies. The diabatic buildup in this Eulerian field is limited through regular, controlled transfers of this field to the contour representation. This transfer is done with a fast newly developed contouring algorithm. This model has been implemented for several idealized geometries. In this paper a single-layer doubly periodic geometry is used to demonstrate the validity of the model. The present model converges faster than the analogous semi-Lagrangian models at increased resolutions. At the same nominal spatial resolution the new model is 40 times faster than the analogous semi-Lagrangian model. Results of an orographically forced idealized storm track show nontrivial dependency of storm-track statistics on resolution and on the numerical model employed. If this result is more generally applicable, this may have important consequences for future high-resolution climate modeling.

Storm tracks and climate change

Extratropical and tropical transient storm tracks are investigated from the perspective of feature tracking in the ECHAM5 coupled climate model for the current and a future climate scenario. The atmosphere-only part of the model, forced by observed boundary conditions, produces results that agree well with analyses from the 40-yr ECMWF Re-Analysis (ERA-40), including the distribution of storms as a function of maximum intensity. This provides the authors with confidence in the use of the model for the climate change experiments. The statistical distribution of storm intensities is virtually preserved under climate change using the Intergovernmental Panel on Climate Change (IPCC) Special Report on Emissions Scenarios (SRES) A1B scenario until the end of this century. There are no indications in this study of more intense storms in the future climate, either in the Tropics or extratropics, but rather a minor reduction in the number of weaker storms. However, significant changes occur on a regional basis in the location and intensity of storm tracks. There is a clear poleward shift in the Southern Hemisphere with consequences of reduced precipitation for several areas, including southern Australia. Changes in the Northern Hemisphere are less distinct, but there are also indications of a poleward shift, a weakening of the Mediterranean storm track, and a strengthening of the storm track north of the British Isles. The tropical storm tracks undergo considerable changes including a weakening in the Atlantic sector and a strengthening and equatorward shift in the eastern Pacific. It is suggested that some of the changes, in particular the tropical ones, are due to an SST warming maximum in the eastern Pacific. The shift in the extratropical storm tracks is shown to be associated with changes in the zonal SST gradient in particular for the Southern Hemisphere.

Climate response to basin-scale warming and cooling of the North Atlantic Ocean

Using experiments with an atmospheric general circulation model, the climate impacts of a basin-scale warming or cooling of the North Atlantic Ocean are investigated. Multidecadal fluctuations with this pattern were observed during the twentieth century, and similar variations--but with larger amplitude--are believed to have occurred in the more distant past. It is found that in all seasons the response to warming the North Atlantic is strongest, in the sense of highest signal-to-noise ratio, in the Tropics. However there is a large seasonal cycle in the climate impacts. The strongest response is found in boreal summer and is associated with suppressed precipitation and elevated temperatures over the lower-latitude parts of North and South America. In August­-September-­October there is a significant reduction in the vertical shear in the main development region for Atlantic hurricanes. In winter and spring, temperature anomalies over land in the extratropics are governed by dynamical changes in circulation rather than simply reflecting a thermodynamic response to the warming or cooling of the ocean. The tropical climate response is primarily forced by the tropical SST anomalies, and the major features are in line with simple models of the tropical circulation response to diabatic heating anomalies. The extratropical climate response is influenced both by tropical and higher-latitude SST anomalies and exhibits nonlinear sensitivity to the sign of the SST forcing. Comparisons with multidecadal changes in sea level pressure observed in the twentieth century support the conclusion that the impact of North Atlantic SST change is most important in summer, but also suggest a significant influence in lower latitudes in autumn and winter. Significant climate impacts are not restricted to the Atlantic basin, implying that the Atlantic Ocean could be an important driver of global decadal variability. The strongest remote impacts are found to occur in the tropical Pacific region in June­-August and September­-November. Surface anomalies in this region have the potential to excite coupled ocean­atmosphere feedbacks, which are likely to play an important role in shaping the ultimate climate response.

The influence of a weakening of the Atlantic meridional overturning circulation on ENSO

The influences of a substantial weakening of the Atlantic meridional overturning circulation (AMOC) on the tropical Pacific climate mean state, the annual cycle, and ENSO variability are studied using five different coupled general circulation models (CGCMs). In the CGCMs, a substantial weakening of the AMOC is induced by adding freshwater flux forcing in the northern North Atlantic. In response, the well-known surface temperature dipole in the low-latitude Atlantic is established, which reorganizes the large-scale tropical atmospheric circulation by increasing the northeasterly trade winds. This leads to a southward shift of the intertropical convergence zone (ITCZ) in the tropical Atlantic and also the eastern tropical Pacific. Because of evaporative fluxes, mixing, and changes in Ekman divergence, a meridional temperature anomaly is generated in the northeastern tropical Pacific, which leads to the development of a meridionally symmetric thermal background state. In four out of five CGCMs this leads to a substantial weakening of the annual cycle in the eastern equatorial Pacific and a subsequent intensification of ENSO variability due to nonlinear interactions. In one of the CGCM simulations, an ENSO intensification occurs as a result of a zonal mean thermocline shoaling. Analysis suggests that the atmospheric circulation changes forced by tropical Atlantic SSTs can easily influence the large-scale atmospheric circulation and hence tropical eastern Pacific climate. Furthermore, it is concluded that the existence of the present-day tropical Pacific cold tongue complex and the annual cycle in the eastern equatorial Pacific are partly controlled by the strength of the AMOC. The results may have important implications for the interpretation of global multidecadal variability and paleo-proxy data.

Is Antarctic climate most sensitive to ozone depletion in the middle or lower stratosphere?

Antarctic stratospheric ozone depletion has been associated with an observed downward trend in tropospheric geopotential height and temperature. Stratospheric ozone depletion peaks in October–November, whereas tropospheric trends are largest in December–January, concurrent with maximum ozone changes close to the tropopause. Surface temperatures are most sensitive to ozone loss near the tropopause, therefore it has been suggested that the observed tropospheric response is forced mainly by ozone depletion in the lower stratosphere. In this study the climate response to ozone depletion exclusively below 164 hPa is simulated using HadSM3-L64, and compared with simulations in which ozone depletion is prescribed exclusively above 164 hPa. Results indicate that the tropospheric response is dominated by ozone changes above 164 hPa, with ozone changes in the lowermost stratosphere playing an insignificant role. A tropospheric response is also seen in fall/winter which agrees well with observations and has not been found in modeling studies previously.

The effect of doubled CO2 and model basic state biases on the monsoon-ENSO system. II: Changing ENSO regimes

Integrations of a fully-coupled climate model with and without flux adjustments in the equatorial oceans are performed under 2×CO2 conditions to explore in more detail the impact of increased greenhouse gas forcing on the monsoon-ENSO system. When flux adjustments are used to correct some systematic model biases, ENSO behaviour in the modelled future climate features distinct irregular and periodic (biennial) regimes. Comparison with the observed record yields some consistency with ENSO modes primarily based on air-sea interaction and those dependent on basinwide ocean wave dynamics. Simple theory is also used to draw analogies between the regimes and irregular (stochastically forced) and self-excited oscillations respectively. Periodic behaviour is also found in the Asian-Australian monsoon system, part of an overall biennial tendency of the model under these conditions related to strong monsoon forcing and increased coupling between the Indian and Pacific Oceans. The tropospheric biennial oscillation (TBO) thus serves as a useful descriptor for the coupled monsoon-ENSO system in this case. The presence of obvious regime changes in the monsoon-ENSO system on interdecadal timescales, when using flux adjustments, suggests there may be greater uncertainty in projections of future climate, although further modelling studies are required to confirm the realism and cause of such changes.

Impact of Tibetan Orography and Heating on the Summer Flow over Asia

The influence on the summer flow over Asia of both the orographic and thermal forcing of the Tibetan Plateau is investigated using a sequence of idealised experiments with a global primitive equation model. The zonally averaged flow is prescribed and both realistic and idealised orography and heating are used. There is some similarity between the responses to the two forcings when applied separately. The upper tropospheric Tibetan anticyclone is predominantly forced by the heating but also weakly by the orography. Below this, both forcings tend to give air descending in an equatorward anticyclonic circulation down the isentropes to the west and rising in a similar poleward circulation to the east. However the heating-only response has a strong ascending southwesterly flow that is guided around the south and south-east of the orography when it is included. On the northern side, the westerly flow over the orography gives ascent on the upslope and descent on the downslope. It is found that heating over the Plateau leads to a potential vorticity (PV) minimum and that if it is sufficiently strong the flow is unstable, producing a quasi-biweekly oscillation. During this oscillation the Tibetan anticyclone changes between a single centre over the southwestern side of the Plateau and a split/double structure with centres over China and the Middle East. These characteristics are similar to observed variability in the region. Associated with this quasi-biweekly oscillation are significant variations in the strength of the ascent over the Plateau and the Rossby wave pattern over the North Pacific. The origin of the variability is instability associated with the zonally extended potential vorticity PV minimum on a θ-surface, as proposed by Hsu and Plumb (2000). This minimum is due to the tendency to reduce the PV above the heating over the Plateau and to advection by the consequent anticyclone of high PV around from the east and low PV to the west. The deep convection to the south and southeast of the Plateau tends to suppress the quasi-biweekly oscillation because the low PV produced above it acts to reduce the meridional PV gradient reversal. The occurrence of the oscillation depends on the relative magnitude of the heating in the two regions.