17 research outputs found

    Urbanyi, Feinmann y Quino : una crítica socio-política y plurigenérica a los tránsitos y desplazamientos de la modernidad

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    Fil: Ilu, Anice Mariela. Universidad Nacional de Córdoba. Facultad de Filosofía y Humanidades. Secretaría de Posgrado; Argentina.Urbanyi, Feinmann y Quino: la experiencia de la dictadura y su proyección en la estética. Pensar la literatura desde una perspectiva crítica implica construir redes de indagación entre los diversos niveles y factores que atraviesan las obras como producciones socioculturales singulares. Esta investigación se apoya en una red de fundamentos sociopolíticos y plurigenéricos para abordar un corpus compuesto por la novela Silver de Pablo Urbanyi, la obra de teatro inédita Cuatro jinetes apocalípticos de José Pablo Feinmann y una selección de humor gráfico de Joaquín Salvador Lavado “Quino”. La experiencia de la dictadura cívico-militar transcurrida desde 1976 a 1983 en Argentina, y sus consecuencias a nivel de ruptura de las libertades, los derechos y transformaciones en sus distintas dimensiones, alcanzan la trayectoria de estos autores. Así, el quiebre de la vida democrática se proyecta y reproduce en fragmentos históricos y generacionales que, experimentados en un escenario donde convivieron la censura, la persecución y el exilio, se diseminan en este corpus, marcando una impronta singular en cada una de las estéticas. Las condiciones históricas y un ensamble de recursos narrativos, humorísticos, retóricos y gráficos configuran aquí una crítica sociopolítica a los tránsitos y desplazamientos de la modernidad, que problematiza las distintas formas de poder y su ejercicio hegemónico como productor de violencia en el universo subjetivo, social, sistémico y global. Nos introducimos así en esta investigación, estableciendo como punto de partida la interpelación desde un paradigma fundado en la epistemología fronteriza. La multiplicidad de planteos vinculados a las transformaciones operadas en los desplazamientos de la modernidad que llegan hasta el fenómeno de la globalización y el capitalismo deshumanizante, son indagadas como problemáticas emergentes a través de las nociones de contradicción y conflicto. La extranjería y los derechos humanos, la explotación y el sometimiento y la configuración de las identidades atravesadas por las condiciones de interculturalidad y transnacionalidad, constituyen el núcleo de dichas problemáticas. Desde allí se proponen diálogos, tensiones y trayectorias de lecturas transversales entre el corpus central y el complementario, como así también entre la vida y estética de los autores. Por último, y dada la importancia que reviste en nuestro enfoque el sentido de la labor académica, se plantea una retroalimentación de los vínculos entre investigación y práctica docente, enmarcada en el trabajo por proyectos.2024-08-11Fil: Ilu, Anice Mariela. Universidad Nacional de Córdoba. Facultad de Filosofía y Humanidades. Secretaría de Posgrado; Argentina

    ENSINO E APRENDIZAGEM POR PROJETOS COMO PROPOSTA DIDÁTICO-PEDAGÓGICA NA FORMAÇÃO DE PROFESSORES

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    The didactic-pedagogical proposal of Project-based learning (PBL) has gained a new centrality in the needs and demands of 21st century education. But despite being included as a priority in curricular designs and in the national program "Transforming high school", there are few experiences at higher education in Argentina. The present article aims to problematize this disarticulation anchored in initial teacher training through the PBL experience developed at a teacher training institute of Argentina. Considering the disarticulations between higher education and the didactic-pedagogical performance required of teachers at the secondary level, we find a vacancy that demands investigation. There is a need to generate experiences in teacher training that establish the foundations and/or expand the borders of the PBL. Said proposal includes virtuality and technological alternatives in a more direct relationship with emerging realities and scaffolding for the students, future professionals, and subjects of social transformation.    La propuesta didáctico-pedagógica de la Enseñanza y Aprendizaje Basado en Proyectos (EABP) ha cobrado una nueva centralidad recontextualizada en las necesidades y demandas de la educación del siglo XXI. En contrapartida, a pesar de incluirse como prioridad en los diseños curriculares y ser una bandera del programa nacional “Transformar la escuela secundaria”, en Argentina son escasas las experiencias en el nivel superior. El objetivo del presente artículo es problematizar esta desarticulación anclada en la formación docente inicial a través de la experiencia de EABP desarrollada en un Instituto de Formación Docente Continua de Argentina. En las desarticulaciones entre la formación superior y el desempeño didáctico-pedagógico exigido a las/os docentes en el nivel secundario, hallamos una vacancia que demanda investigar y permite concluir la necesidad de generar en la formación docente experiencias que establezcan los cimientos y/o amplíen las fronteras de la EABP. Esto incluye la virtualidad y las alternativas tecnológicas en una relación más directa con las realidades emergentes y andamiajes para las trayectorias de las/os estudiantes, futuros profesionales y sujetos de transformación social.    A proposta didático-pedagógica de Ensino e Aprendizagem Baseada em Projetos (EABP) ganhou uma nova centralidade recontextualizada nas necessidades e demandas da educação do século XXI. Por outro lado, apesar de estar incluída como prioridade nos desenhos curriculares e ser uma bandeira do programa nacional “Transformando o ensino secundário”, na Argentina existem poucas experiências de nível superior. O objetivo deste artigo é problematizar esta desarticulação ancorada na formação inicial de professores através da experiência da EABP desenvolvida em um Instituto de Formação Continuada de Professores na Argentina. Nas desarticulações entre o ensino superior e a atuação didático-pedagógica exigida dos professores do ensino médio, encontramos uma vaga que exige investigação e nos permite concluir a necessidade de gerar experiências na formação docente que estabeleçam os alicerces e/ou ampliem as fronteiras da EABP. Isto inclui a virtualidade e as alternativas tecnológicas numa relação mais direta com as realidades emergentes e como andaimes para as trajetórias de estudantes, futuros profissionais e sujeitos de transformação social.   Palavras-chave: projetos; didática; treinamento de professor; autonomia; bimodalidade. &nbsp

    Work on the play "Helver's Night"

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    Ovaj diplomski rad bavi se radom na predstavi “Helverova noć” studenata druge godine diplomskog studija Gluma i animacija pod mentorstvom doc. art. Anice Tomić i sumentorstvom doc. art. Domagoja Mrkonjića. U radu se izlaže proces rada utjelovljenja uloge Karle putem istraživanja, analize, dramaturških intervencija, konceptualizacije i, najvažnije, praktičnih proba. Izlažući njihove prednosti i nedostatke autorica sistematizira i objašnjava donesene odluke u gradnji lika i predstave. Rad se referira i uspoređuje novonastali prilagođeni tekst s originalom.This graduation thesis deals with the work on the play "Helver's Night" by students of the second year of the graduate study of Acting and Animation under the mentorship of doc.art. Anice Tomić and with the co-mentorship of doc.art. Domagoj Mrkonjić. The paper presents the work process of embodying the role of Karla through research, analysis, dramaturgical interventions, conceptualization and, most importantly, practical rehearsals. Exposing its advantages and disadvantages, the author systematizes and explains the decisions made in the construction of the character and the play. The paper refers to and compares the newly created adapted text with the original

    Work on the play "Helver's Night"

    No full text
    Ovaj diplomski rad bavi se radom na predstavi “Helverova noć” studenata druge godine diplomskog studija Gluma i animacija pod mentorstvom doc. art. Anice Tomić i sumentorstvom doc. art. Domagoja Mrkonjića. U radu se izlaže proces rada utjelovljenja uloge Karle putem istraživanja, analize, dramaturških intervencija, konceptualizacije i, najvažnije, praktičnih proba. Izlažući njihove prednosti i nedostatke autorica sistematizira i objašnjava donesene odluke u gradnji lika i predstave. Rad se referira i uspoređuje novonastali prilagođeni tekst s originalom.This graduation thesis deals with the work on the play "Helver's Night" by students of the second year of the graduate study of Acting and Animation under the mentorship of doc.art. Anice Tomić and with the co-mentorship of doc.art. Domagoj Mrkonjić. The paper presents the work process of embodying the role of Karla through research, analysis, dramaturgical interventions, conceptualization and, most importantly, practical rehearsals. Exposing its advantages and disadvantages, the author systematizes and explains the decisions made in the construction of the character and the play. The paper refers to and compares the newly created adapted text with the original

    Work on the play "Helver's Night"

    No full text
    Ovaj diplomski rad bavi se radom na predstavi “Helverova noć” studenata druge godine diplomskog studija Gluma i animacija pod mentorstvom doc. art. Anice Tomić i sumentorstvom doc. art. Domagoja Mrkonjića. U radu se izlaže proces rada utjelovljenja uloge Karle putem istraživanja, analize, dramaturških intervencija, konceptualizacije i, najvažnije, praktičnih proba. Izlažući njihove prednosti i nedostatke autorica sistematizira i objašnjava donesene odluke u gradnji lika i predstave. Rad se referira i uspoređuje novonastali prilagođeni tekst s originalom.This graduation thesis deals with the work on the play "Helver's Night" by students of the second year of the graduate study of Acting and Animation under the mentorship of doc.art. Anice Tomić and with the co-mentorship of doc.art. Domagoj Mrkonjić. The paper presents the work process of embodying the role of Karla through research, analysis, dramaturgical interventions, conceptualization and, most importantly, practical rehearsals. Exposing its advantages and disadvantages, the author systematizes and explains the decisions made in the construction of the character and the play. The paper refers to and compares the newly created adapted text with the original

    Interactions between Ice Sheet Dynamics and Glacial Isostatic Adjustment: The development and application of a new method to simulate the Antarctic Ice Sheet over the last glacial cycle

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    The Antarctic ice sheet is a complex system highly influenced by global and local processes and characteristics including a varying bedrock elevation and structure of the solid Earth and a changing climate. Sea level rise has a high impact on society and the improvement of forecasts are vital to generate both adaptation and mitigation strategies. A recent comparison of 15 ice sheet models projected that the Antarctic Ice Sheet could contribute -7.8 to 30 centimeters of sea level rise between 2015 and 2100, meaning that sea level rise could increase a lot although the uncertainty is high. To better predict the future of the AIS, more accurate simulations of the evolution of the AIS are needed. The Antarctic ice sheet consist of three main components: grounded slow-moving ice, fast flowing ice streams or outlet glaciers and floating ice shelves. Over glacial-interglacial cycles, the evolution of an ice sheet is influenced by Glacial Isostatic Adjustment (GIA) via two negative feedback loops. First, vertical bedrock deformation due to a changing ice load alters ice-sheet surface elevation. Second, bedrock deformation will change the location of the grounding line of the ice sheet. GIA is mainly determined by the viscosity of the interior of the solid Earth which is radially and laterally varying. Underneath the Antarctic Ice Sheet (AIS), there are relatively low viscosities in West Antarctica and higher viscosities in East Antarctica, which affect the response time of the above-mentioned feedbacks. However, most ice-dynamic models do not consider lateral variations of viscosity in the upper mantle in GIA feedback loops when simulating the evolution of the AIS. The main research question of this study is: •What is the effect of the interaction between Glacial Isostatic Adjustment and ice sheet dynamics on the Antarctic Ice Sheet growth during the last glacial cycle? This study presents a new method to investigate 3D GIA feedback effects in detail at any chosen period during the last glacial cycle. The method is applied using ANICE and a 3D GIA FEM model. This led to the development of a fully coupled ice dynamic-3D GIA model with coupling timesteps of 1000 and 5000 years. Following the new method, the model computations alternate between the ice-sheet model, ANICE, and a 3D Finite Element Method model until convergence of the ice thickness occurs at each timestep. We simulate the evolution of the AIS from 120 000 years to 115 000 years before present, considering 1D and non-linear 3D rheologies. The results of the coupled model are discussed in detail for the period 120,000 years to 115,000 years before present with a focus on the Siple Coast and the Ross Ice Shelf. The maximum difference between the uncoupled deformation (iteration 1) and the coupled deformation (average between the last two iterations) for the period 120,000 to 115,000 years BP is 3 to 8 mm per year, depending on the viscosity of the upper mantle. The maximum difference in ice thickness at 115,000 years BP is 50 meters close the Ronne Ice Shelf and the Ross Ice Shelf. The grounding line position differs up to 80 meters when applying the coupling method compared to the uncoupled result. The increases in deformation using a 3D wet rheology with a grain size of 10 mm are highest at the Siple Coast, the Ronne Ice Shelf, and several other locations along the grounding line of the AIS. The results of this study emphasize the importance of the 3D GIA feedback effects when simulating the evolution of the AIS during the last glacial cycle. Therefore, the GIA feedback effects should be taken into account in future studies.Geoscience and Remote Sensin

    Feedback between ice dynamics and bedrock deformation with 3D viscosity in Antarctica

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    Over glacial-interglacial cycles, the evolution of an ice sheet is influenced by Glacial isostatic adjustment (GIA) via two negative feedback loops. Firstly, vertical bedrock deformation due to a changing ice load alters ice-sheet surface elevation. For example, an increasing ice load leads to a lower bedrock elevation that lowers ice-sheet surface elevation. This will increase surface melting of the ice sheet, following an increase of atmospheric temperature at lower elevations. Secondly, bedrock deformation will change the height of the grounding line of the ice sheet. For example, a lowering bedrock height following ice-sheet advance increases the melt due to ocean water that in turn leads to a retreat of the grounding line and a slow-down of ice-sheet advance. GIA is mainly determined by the viscosity of the interior of the solid Earth which is radially and laterally varying. Underneath the Antarctic ice sheet, there are relatively low viscosities in West Antarctica and higher viscosities in East Antarctica, in turn affecting the response time of the above mentioned feedbacks. However, most ice-dynamical models do not consider the lateral variations of the viscosity in the GIA feedback loops when simulating the evolution of the Antarctic ice sheet. The method developed by Gomez et al. (2018) includes the feedback between GIA and ice-sheet evolution and alternates between simulations of the two models where each simulation covers the full time period. We presents a different method to couple ANICE, a 3-D ice-sheet model, to a 3-D GIA finite element model. In this method the model computations alternates between the icesheet and GIA model until convergence of the result occurs at each timestep. We simulate the evolution of the Antarctic ice sheet from 120 000 years ago to the present. The results of the coupled simulation will be discussed and compared to results of the uncoupled ice-sheet model (using an ELRA GIA model) and the method developed by Gomez et al. (2018). Physical and Space GeodesyAstrodynamics & Space Mission

    Simulation of a fully coupled 3D glacial isostatic adjustment – ice sheet model for the Antarctic ice sheet over a glacial cycle

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    Glacial isostatic adjustment (GIA) has a stabilizing effect on the evolution of the Antarctic ice sheet by reducing the grounding line migration following ice melt. The timescale and strength of this feedback depends on the spatially varying viscosity of the Earth's mantle. Most studies assume a relatively long and laterally homogenous response time of the bedrock. However, the mantle viscosity is spatially variable, with a high mantle viscosity beneath East Antarctica and a low mantle viscosity beneath West Antarctica. For this study, we have developed a new method to couple a 3D GIA model and an ice sheet model to study the interaction between the solid Earth and the Antarctic ice sheet during the last glacial cycle. With this method, the ice sheet model and GIA model exchange ice thickness and bedrock elevation during a fully coupled transient experiment. The feedback effect is taken into account with a high temporal resolution, where the coupling time steps between the ice sheet and GIA model are 5000 years over the glaciation phase and vary between 500 and 1000 years over the deglaciation phase of the last glacial cycle. During each coupling time step, the bedrock elevation is adjusted at every ice sheet model time step, and the deformation is computed for a linearly changing ice load. We applied the method using the ice sheet model ANICE and a 3D GIA finite element model. We used results from a regional seismic model for Antarctica embedded in the global seismic model SMEAN2 to determine the patterns in the mantle viscosity. The results of simulations over the last glacial cycle show that differences in mantle viscosity of an order of magnitude can lead to differences in the grounding line position up to 700gkm and to differences in ice thickness of the order of 2gkm for the present day near the Ross Embayment. These results underline and quantify the importance of including local GIA feedback effects in ice sheet models when simulating the Antarctic ice sheet evolution over the last glacial cycle.Astrodynamics & Space Mission
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