916 resultados para 883


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Inclui notas explicativas, bibliográficas e bibliografia

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Una de las competencias que debe adquirir un maestro de educación primaria es mirar profesionalmente aspectos de la enseñanza que le permitan identificar lo relevante para el aprendizaje, interpretarlo y tomar decisiones de acción. Durante las prácticas de enseñanza en los centros de Educación Primaria, se pidió a un grupo de futuros maestros que escribieran una narrativa en la que se identificara evidencias de lo que consideraban manifestaciones de la competencia matemática de los estudiantes. La narrativa consistía en (1) la descripción de la situación de enseñanza-aprendizaje en la que habían identificado evidencias de la competencia matemática de sus estudiantes. Debían describir la tarea, qué hacen los alumnos, y cómo el maestro apoya la interacción (2) la interpretación de la situación, que debía contener evidencias de la comprensión de los estudiantes y evidencias de cómo parecían estar desarrollándose diferentes aspectos de la competencia matemática y (3) completar la situación para potenciar el desarrollo de la competencia matemática identificada o algún otro aspecto de la competencia. La elaboración de las narrativas ayudó a los futuros maestros a empezar a desarrollar una mirada estructurada sobre las situaciones de enseñanza-aprendizaje que puede ayudarles a seguir aprendiendo a lo largo de la vida profesional.

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This article deals with both the word-formation mechanism of blending and the creative process involved in providing characters with proper names in cartoons or TV series for children in English. The study addresses the nature and features of proper and common names, two apparently well-distinguished categories, as well as, and basically fictional proper names, by suggesting differences between fictional proper names and other types of proper and common names. Furthermore, it discusses the presence of blending in fiction and in fictional proper names, with special reference to charactonyms. The main focus of this work is on blended charactonyms in cartoons addressed to children, which for the purposes of this study will be called cartoonyms or charactoons. Questions such as the following are addressed: the formation or creation of cartoonyms or charactoons from pre-existing material; the semantic motivations behind their formation; their resulting structural complexity; their particularly descriptive, expressive and meaningful nature; as well as how suitable they are to the genre in which they are used.

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Existen dos mitos fuertemente arraigados en un amplio sector de la sociedad española, convencido, por una parte, que la edad de setenta años constituye una patente de corso para delinquir sin que la consecuencia jurídica asociada entrañe el ingreso en prisión y, por otra, que quien se halla cumpliendo condena en un establecimiento penitenciario y alcanza dicha edad obtiene, de manera automática, la libertad condicional. Sin embargo, no solo ambas creencias han carecido, desde siempre, de escarpia normativa que las sustentase, sino que la realidad penitenciaria ha evidenciado, desde antiguo, la presencia de ancianos en sus centros.

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This layer is a georeferenced raster image of the historic paper map entitled: Plan von Dresden : 1902, Bearbeitet vom Vermessungsamte der Stadt Dresden. It was published by Giesecke & Devrient in 1902. 16th Aufl. Scale 1:10,000. Covers the Dresden region, Germany. Map in German. The image inside the map neatline is georeferenced to the surface of the earth and fit to the Deutsches Hauptdreiecksnetz (DHDN) 3-degree Gauss-Kruger Zone 5 coordinate system. All map collar and inset information is also available as part of the raster image, including any inset maps, profiles, statistical tables, directories, text, illustrations, index maps, legends, or other information associated with the principal map. This map shows features such as roads, railroads and stations, drainage, built-up areas and selected buildings, city districts, parks, ground cover, and more. Includes inset: Ergänzungsblatt zu der Flur Reick. This layer is part of a selection of digitally scanned and georeferenced historic maps from The Harvard Map Collection as part of the Imaging the Urban Environment project. Maps selected for this project represent major urban areas and cities of the world, at various time periods. These maps typically portray both natural and manmade features at a large scale. The selection represents a range of regions, originators, ground condition dates, scales, and purposes.

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The work in this sub-project of ESOP focuses on the advective and convective transforma-tion of water masses in the Greenland Sea and its neighbouring areas. It includes observational work on the sub-mesoscale and analysis of hydrographic data up to the gyre-scale. Observations of active convective plumes were made with a towed chain equipped with up to 80 CTD sensors, giving a horizontal and vertical resolution of the hydrographic fields of a few metres. The observed scales of the penetrative convective plumes compare well with those given by theory. On the mesoscale the structure of homogeneous eddies formed as a result of deep convection was observed and the associated mixing and renewal of the intermediate layers quantified. The relative importance and efficiency of thermal and haline penetrative convection in relation to the surface boundary conditions (heat and salt fluxes and ice cover) and the ambient stratification are studied using the multi year time series of hydro-graphic data in the central Greenland Sea. The modification of the water column of the Greenland Sea gyre through advection from and mixing with water at its rim is assessed on longer time scales. The relative contributions are quantified using modern water mass analysis methods based on inverse techniques. Likewise the convective renewal and the spreading of the Arctic Intermediate Water from its formation area is quantified. The aim is to budget the heat and salt content of the water column, in particular of the low salinity surface layer, and to relate its seasonal and interannual variability to the lateral fluxes and the fluxes at the air-sea-ice interface. This will allow to estimate residence times for the different layers of the Greenland Sea gyre, a quantity important for the description of the Polar Ocean carbon cycle.

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Arctic sea ice has declined and become thinner and younger (more seasonal) during the last decade. One consequence of this is that the surface energy budget of the Arctic Ocean is changing. While the role of surface albedo has been studied intensively, it is still widely unknown how much light penetrates through sea ice into the upper ocean, affecting sea-ice mass balance, ecosystems, and geochemical processes. Here we present the first large-scale under-ice light measurements, operating spectral radiometers on a remotely operated vehicle (ROV) under Arctic sea ice in summer. This data set is used to produce an Arctic-wide map of light distribution under summer sea ice. Our results show that transmittance through first-year ice (FYI, 0.11) was almost three times larger than through multi-year ice (MYI, 0.04), and that this is mostly caused by the larger melt-pond coverage of FYI (42 vs. 23%). Also energy absorption was 50% larger in FYI than in MYI. Thus, a continuation of the observed sea-ice changes will increase the amount of light penetrating into the Arctic Ocean, enhancing sea-ice melt and affecting sea-ice and upper-ocean ecosystems.

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A thick, apparently continuous section recording events of the latest Paleocene thermal maximum in a neritic setting was drilled at Bass River State Forest, New Jersey as part of ODP Leg 174AX [Miller, Sugarman, Browning et al., 1998]. Integrated nannofossil and magneto-stratigraphy provides a firm chronology supplemented by planktonic foraminiferal biostratigraphy. This chronologic study indicates that this neritic section rivals the best deep-sea sections in providing a complete record of late Paleocene climatic events. Carbon and oxygen isotopes measured on benthic foraminifera show a major (4.0% in carbon, 2.3% in oxygen) negative shift correlative with the global latest Paleocene carbon isotope excursion (CIE). A sharp increase in kaolinite content coincides with the isotope shift in the Bass River section, analogous to increases found in several other records. Carbon and oxygen isotopes remain low and kaolinite content remains high for the remainder of the depositional sequence above the CIE (32.5 ft, 9.9 m), which we estimate to represent 300-500 k.y. We interpret these data as indicative of an abrupt shift to a warmer and wetter climate along the North American mid-Atlantic coast, in concert with global events associated with the CIE.

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Vol. 883-930 issued in 2 sections: Patents and Trademarks.

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Also issued by Historical Section, General Staff, A.E.F., as Tactical studies, no. 1.