Implantación de semi-presencialidad en una asignatura optativa de la Licenciatura en Ciencias y Técnicas Estadísticas.

Monográfico con el título: 'Educación matemática y tecnologías de la información'. Resumen basado en el de la publicación

Blended learning (formaci??n semi-presencial) en educaci??n f??sica

Se describe una actividad llevada a cabo en el IES Bembezar (Azuaga, Badajoz) cuyo objetivo era el desarrollo de contenidos te??rico pr??cticos del bloque de condici??n f??sica y salud a trav??s de un modelo de blended-learning.

Conflictos semi??ticos sobre la correlaci??n y regresi??n en los libros de texto de bachillerato

Resumen basado en el de la publicaci??n

Explorando el uso de estrategias discursivas y semi??ticas en la construcci??n guiada del conocimiento

Resumen basado en el de la publicaci??n

Integración de los estándares OGC en los clientes 2D y 3D de visualización de mapas

A través de la propuesta Styled Layer Descriptor 3D (SLD3D), cuya especificación se encuentra en el Open Geospatial Consortium (OGC), se posibilitará la generación de información tridimensional. La interpretación de estos estilos a través del Keyhole Markup Language (KML) y su representación en los interfaces 3D, garantizarán el aprovechamiento de la tercera componente espacial permitiendo una representación realista del entorno

Evaluación de la competencia comunicativa académica en semi-presencialidad

En la E.U. de Magisterio de Donostia de la Universidad del País Vasco (UPV/EHU), este curso 2010/2011 ha comenzado la oferta semi-presencial para aquellos estudiantes que no pueden matricularse a todas las asignaturas de primer curso. Dentro de esta experiencia piloto se ha impartido la asignatura "Desarrollo de la competencia comunicativa I" en el Grado de Educación Primaria, centrada en la competencia comunicativa académica. El diseño de esta asignatura se ha apoyado en investigaciones relacionadas con el desarrollo de esta competencia en entornos virtuales y ha contado con actividades diversas que han permitido a los estudiantes su autoevaluación y también la coevaluación

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.

Benchmarking 2D hydraulic models for urban flooding

This paper describes benchmark testing of six two-dimensional (2D) hydraulic models (DIVAST, DIVASTTVD, TUFLOW, JFLOW, TRENT and LISFLOOD-FP) in terms of their ability to simulate surface flows in a densely urbanised area. The models are applied to a 1·0 km × 0·4 km urban catchment within the city of Glasgow, Scotland, UK, and are used to simulate a flood event that occurred at this site on 30 July 2002. An identical numerical grid describing the underlying topography is constructed for each model, using a combination of airborne laser altimetry (LiDAR) fused with digital map data, and used to run a benchmark simulation. Two numerical experiments were then conducted to test the response of each model to topographic error and uncertainty over friction parameterisation. While all the models tested produce plausible results, subtle differences between particular groups of codes give considerable insight into both the practice and science of urban hydraulic modelling. In particular, the results show that the terrain data available from modern LiDAR systems are sufficiently accurate and resolved for simulating urban flows, but such data need to be fused with digital map data of building topology and land use to gain maximum benefit from the information contained therein. When such terrain data are available, uncertainty in friction parameters becomes a more dominant factor than topographic error for typical problems. The simulations also show that flows in urban environments are characterised by numerous transitions to supercritical flow and numerical shocks. However, the effects of these are localised and they do not appear to affect overall wave propagation. In contrast, inertia terms are shown to be important in this particular case, but the specific characteristics of the test site may mean that this does not hold more generally.

Impact of mass lumping on gravity and Rossby waves in 2D finite-element shallow-water models

The goal of this study is to evaluate the effect of mass lumping on the dispersion properties of four finite-element velocity/surface-elevation pairs that are used to approximate the linear shallow-water equations. For each pair, the dispersion relation, obtained using the mass lumping technique, is computed and analysed for both gravity and Rossby waves. The dispersion relations are compared with those obtained for the consistent schemes (without lumping) and the continuous case. The P0-P1, RT0 and P-P1 pairs are shown to preserve good dispersive properties when the mass matrix is lumped. Test problems to simulate fast gravity and slow Rossby waves are in good agreement with the analytical results.

The timing of Quaternary calcrete development in semi-arid southeast Spain: Investigating the role of climate on calcrete genesis

Quaternary-aged calcrete horizons are common weathering products in arid and semi-arid regions. It is, however, unclear how calcrete forming processes respond to the major oscillations in climate that occur over the Quaternary period. This paper presents a U-series-based calcrete age database from the Sorbas basin, southeast Spain. The study constructs an age frequency distribution of these ages which is consequently compared to a range of palaeoenvironmental records from the Mediterranean. The age distribution presented here suggests that the formation of pedogenic calcrete horizons in the Sorbas basin primarily occurs during 'warm' isotope stages (MIS 1 and 5), with very few calcrete ages occurring during cold glacial/stadial stages (MIS 2, 3 and 4). It is suggested that this is a function of the environments that existed during 'warm' isotope stages being more conducive to calcrete development than those that existed during cold climate episodes. In a semi-arid region such as the Sorbas basin it is likely that increased aridity during glacial stages, coupled with reduced vegetation and accelerated landscape instability, was crucial in reducing rates of calcrete formation. In a semi-arid region such as southeast Spain, calcrete formation during the Quaternary, therefore, oscillates with climate change but is primarily a "warm" episode phenomenon. It is suggested that further studies are required to see how calcrete genesis responds to environmental change in more humid parts of the Mediterranean. (C) 2009 Elsevier B.V. All rights reserved.