How to assess, plan and teach shared and guided reading and writing 2 : key stage two, primary 4-7.

En esta etapa del desarrollo de la alfabetización, la mayoría de los niños han comprendido sus conceptos fundamentales y ya saben hablar, leer y escribir para distintos tipos de oyentes y para distintos propósitos. Para la consolidación de estos conocimientos y la adquisición de nuevas habilidades necesitan contar con una amplia gama de textos y contextos, aprender a decodificar palabras desconocidas, deletrear palabras difíciles. El modelo de lectura y escritura compartida y guiada es la estrategia de enseñanza más idónea.

Guided reading : teacher's workbook.

Es un módulo, de carácter interactivo, en el que se recomienda que no haya más de doce participantes, para que cada uno tenga la oportunidad de expresar sus pensamientos, preguntas e investigaciones en el aula. Lectura guiada es una técnica de instrucción y evaluación que apoya y fomenta el desarrollo de estrategias de lectura independiente. El grupo debe estar formado por cuatro o seis niños, cada uno de los cuales tiene una copia del libro a leer y su actividad debe de ser la de dar sentido de forma independiente al texto, con el apoyo de los demás miembros del grupo y del profesor. El apoyo del docente es breve, y su actitud es observar, afirmar y responder a las necesidades de los niños e invitarles a utilizar los recursos y estrategias de los que disponen.

Guided reading : course co-ordinator's book.

Es un módulo, de carácter interactivo, sobre 'lectura guiada' en el que se recomienda que no haya más de doce participantes, uno de los cuales es el responsable de la organización de las sesiones. Lectura guiada es una técnica de instrucción y evaluación que apoya y fomenta el desarrollo de estrategias de lectura independiente. El responsable del módulo propone las actividades que se realizan en las sesiones para las diferentes etapas en los primeros años de escolarización, los materiales y equipos que serán necesarios para apoyar cada período de sesiones,las sugerencias de textos de ficción y no ficción que los participantes apoyan para las actividades de lectura guiada, y por último,cómo llevar a cabo las sesiones de apoyo y las tareas y actividades.

Book bands for guided reading : organising key stage one texts for the literacy hour.

Ha sido pensado para ayudar a los profesores a revisar, organizar y completar en las escuelas, las existencias de materiales de lectura para la etapa uno (Key Stage uno). También, proporciona las bases para establecer los procedimientos de lectura guiada en la etapa de alfabetización infantil, y para indicar cómo la lectura guiada encaja dentro de la National Literacy Strategy Framework for Teaching (Estrategia Nacional de Alfabetización Marco para la Enseñanza). Se reunieron casi cuatro mil libros para los niños, que se han agrupado teniendo en cuenta la gradación de dificultad de los textos en diez bloques, desde los más sencillos para los primeros lectores a áquellos utilizados al final de la etapa uno (Key stage uno) para lectores con más fluidez.

New wave!

Ayudas a la Innovación Educativa, 1997-98. Anexo Memoria en C-Innov. 54

Integrative Behavioral Couple Therapy (IBCT) as a third-wave therapy

Resumen tomado de la publicaci??n

Simple finite field nuclear relaxation method for calculating vibrational contribution to degenerate four-wave mixing

A simple extended finite field nuclear relaxation procedure for calculating vibrational contributions to degenerate four-wave mixing (also known as the intensity-dependent refractive index) is presented. As a by-product one also obtains the static vibrationally averaged linear polarizability, as well as the first and second hyperpolarizability. The methodology is validated by illustrative calculations on the water molecule. Further possible extensions are suggested

The counter-propagating Rossby-wave perspective on baroclinic instability. I: Mathematical basis

It is shown that Bretherton's view of baroclinic instability as the interaction of two counter-propagating Rossby waves (CRWs) can be extended to a general zonal flow and to a general dynamical system based on material conservation of potential vorticity (PV). The two CRWs have zero tilt with both altitude and latitude and are constructed from a pair of growing and decaying normal modes. One CRW has generally large amplitude in regions of positive meridional PV gradient and propagates westwards relative to the flow in such regions. Conversely, the other CRW has large amplitude in regions of negative PV gradient and propagates eastward relative to the zonal flow there. Two methods of construction are described. In the first, more heuristic, method a ‘home-base’ is chosen for each CRW and the other CRW is defined to have zero PV there. Consideration of the PV equation at the two home-bases gives ‘CRW equations’ quantifying the evolution of the amplitudes and phases of both CRWs. They involve only three coefficients describing the mutual interaction of the waves and their self-propagation speeds. These coefficients relate to PV anomalies formed by meridional fluid displacements and the wind induced by these anomalies at the home-bases. In the second method, the CRWs are defined by orthogonality constraints with respect to wave activity and energy growth, avoiding the subjective choice of home-bases. Using these constraints, the same form of CRW equations are obtained from global integrals of the PV equation, but the three coefficients are global integrals that are not so readily described by ‘PV-thinking’ arguments. Each CRW could not continue to exist alone, but together they can describe the time development of any flow whose initial conditions can be described by the pair of growing and decaying normal modes, including the possibility of a super-modal growth rate for a short period. A phase-locking configuration (and normal-mode growth) is possible only if the PV gradient takes opposite signs and the mean zonal wind and the PV gradient are positively correlated in the two distinct regions where the wave activity of each CRW is concentrated. These are easily interpreted local versions of the integral conditions for instability given by Charney and Stern and by Fjørtoft.

The counter-propagating Rossby-wave perspective on baroclinic instability. II: Application to the Charney model

The constant-density Charney model describes the simplest unstable basic state with a planetary-vorticity gradient, which is uniform and positive, and baroclinicity that is manifest as a negative contribution to the potential-vorticity (PV) gradient at the ground and positive vertical wind shear. Together, these ingredients satisfy the necessary conditions for baroclinic instability. In Part I it was shown how baroclinic growth on a general zonal basic state can be viewed as the interaction of pairs of ‘counter-propagating Rossby waves’ (CRWs) that can be constructed from a growing normal mode and its decaying complex conjugate. In this paper the normal-mode solutions for the Charney model are studied from the CRW perspective. Clear parallels can be drawn between the most unstable modes of the Charney model and the Eady model, in which the CRWs can be derived independently of the normal modes. However, the dispersion curves for the two models are very different; the Eady model has a short-wave cut-off, while the Charney model is unstable at short wavelengths. Beyond its maximum growth rate the Charney model has a neutral point at finite wavelength (r=1). Thereafter follows a succession of unstable branches, each with weaker growth than the last, separated by neutral points at integer r—the so-called ‘Green branches’. A separate branch of westward-propagating neutral modes also originates from each neutral point. By approximating the lower CRW as a Rossby edge wave and the upper CRW structure as a single PV peak with a spread proportional to the Rossby scale height, the main features of the ‘Charney branch’ (0wave propagation mechanism and the CRW interaction. The behaviour of the Charney modes and the first neutral branch, which rely on tropospheric PV gradients, are arguably more applicable to the atmosphere than modes of the Eady model where the positive PV gradient exists only at the tropopause

The counterpropagating Rossby wave perspective on Kelvin Helmholtz instability as a limiting case of a Rayleigh shear layer with zero width

The Kelvin Helmholtz (KH) problem, with zero stratification, is examined as a limiting case of the Rayleigh model of a single shear layer whose width tends to zero. The transition of the Rayleigh modal dispersion relation to the KH one, as well as the disappearance of the supermodal transient growth in the KH limit, are both rationalized from the counterpropagating Rossby wave perspective.

The counter-propagating Rossby-wave perspective on baroclinic instability. Part III: Primitive-equation disturbances on the sphere

Baroclinic instability of perturbations described by the linearized primitive quations, growing on steady zonal jets on the sphere, can be understood in terms of the interaction of pairs of counter-propagating Rossby waves (CRWs). The CRWs can be viewed as the basic components of the dynamical system where the Hamiltonian is the pseudoenergy and each CRW has a zonal coordinate and pseudomomentum. The theory holds for adiabatic frictionless flow to the extent that truncated forms of pseudomomentum and pseudoenergy are globally conserved. These forms focus attention on Rossby wave activity. Normal mode (NM) dispersion relations for realistic jets are explained in terms of the two CRWs associated with each unstable NM pair. Although derived from the NMs, CRWs have the conceptual advantage that their structure is zonally untilted, and can be anticipated given only the basic state. Moreover, their zonal propagation, phase-locking and mutual interaction can all be understood by ‘PV-thinking’ applied at only two ‘home-bases’—potential vorticity (PV) anomalies at one home-base induce circulation anomalies, both locally and at the other home-base, which in turn can advect the PV gradient and modify PV anomalies there. At short wavelengths the upper CRW is focused in the mid-troposphere just above the steering level of the NM, but at longer wavelengths the upper CRW has a second wave-activity maximum at the tropopause. In the absence of meridional shear, CRW behaviour is very similar to that of Charney modes, while shear results in a meridional slant with height of the air-parcel displacement-structures of CRWs in sympathy with basic-state zonal angular-velocity surfaces. A consequence of this slant is that baroclinically growing eddies (on jets broader than the Rossby radius) must tilt downshear in the horizontal, giving rise to up-gradient momentum fluxes that tend to accelerate the barotropic component of the jet.