Como aprender História e Geografia no 8º ano de escolaridade, usando o Google Earth ?

Actualmente no Ensino Básico as disciplinas de História e Geografia são vistas, maioritariamente , como desinteressantes e pouco úteis a grande parte dos alunos. Variadas razões podem ser apontadas, como a excessiva memorização de conteúdos, cultivados por um ensino expositivo enquanto forma de ensino com maiores adeptos pelos professores nas escolas. Aliada a esta memorização surge, inevitavelmente, a pouca retenção na memória no tempo dos conhecimentos adquiridos a estas disciplinas. Partindo dos pressupostos teóricos sobre os métodos de ensino mais inovadores, que sugerem a realização de experiências educativas com uma metodologia activa e um ensino por competências , efectuou-se uma experiência de aprendizagem em que se utilizou a ferramenta Google Earth nas aulas de História e Geografia do 8º ano de escolaridade. Pretendeu-se aferir se, com recurso às novas tecnologias, os alunos interiorizariam melhor conceitos relativos ás duas áreas do saber.

The high risk register and identification of hearing impaired infants in an NICU

This paper discusses hearing tests of infants in a NICU.

The use of a single channel, two attenuator hearing aid by severely hearing impaired children

This paper examines the results of testing five severely hearing impaired children using a special binaural system with s single amplification channel and two attenuators, allowing presentation of the stimulus materials monaurally or at different relative levels to the two ears.

Albumes de ciudad: representaciones de los procesos modernizantes en Cartagena de Indias y Santiago de Guayaquil a comienzos del siglo XX (1900-1930)

La presente tesis tiene como objetivo mostrar cual fue el papel, que a nivel simbólico, tuvo la fotografía en la consolidación de los procesos modernizadores puestos en marcha en las ciudades de Cartagena de Indias y Santiago de Guayaquil, a comienzos de siglo XX (1900-1920). De forma particular atiendo a las formas en que se representa a la ciudad como espacio moderno en las fotografías seleccionadas. Para esto, parto del estudio de tres álbumes de fotografía que se produjeron en dichas ciudades en la primera treintena del siglo XX: Cartagena Ilustrada de Carlos y Francisco Valiente, Álbum de Cartagena de Indias 1533-1933 de Pedro Donoso, y Guayaquil a la vista de Juan De Ceriola. Considero que las representaciones de ciudad que se encuentran en los álbumes fotográficos se entretejen con los procesos sociales y económicos que tienen lugar en ambas ciudades. Entonces, haciendo un seguimiento de los lugares escogidos para ser representados en las fotografías consignadas en estos álbumes, muestro la imagen de ciudad moderna que se construye visualmente desde las élites en las dos ciudades de mi interés. De este modo, en la medida en que se establece una relación entre la organización del campo de la visualidad y las estructuras sociales, económicas y políticas que caracterizan la modernidad, se puede decir que en este trabajo se evidencia la constitución de una economía visual moderna en las ciudades señaladas.

Kipus: revista andina de letras. 21 (Reseñas)

Presenta las reseñas de los siguientes libros: JAVIER VÁSCONEZ, JARDÍN CAPELO, Quito, Orogenia, 2007. APUESTA. LOS JUEGOS DE VÁSCONEZ, FRANCISCO ESTRELLA, COMP., Quito, Taurus, 2007, 194 pp. -- HUMBERTO E. ROBLES, LA NOCIÓN DE VANGURDIA EN EL ECUADOR (RECEPCIÓN, TRAYECTORIA Y DOCUMENTOS 1918-1934), Quito, Universidad Andina Simón Bolívar / Corporación Editora Nacional, 2006, 2a. ed., 198 pp. -- ABDÓN UBIDIA, CELEBRACIÓN DE LOS LIBROS, Quito, El Conejo / Eskeletra, 2007, 174 pp. -- CARLOS ARCOS, EL INVITADO, Quito, El Conejo, 2007, 334 pp. -- VICENTE ROBALINO, CUANDO EL CUERPO SE DESPRENDE DEL ALBA, Quito, Casa de la Cultura Ecuatoriana, 2006, 73, pp.

Estimates of Avian Mortality Attributed to Vehicle Collisions in Canada

Although mortality of birds from collisions with vehicles is estimated to be in the millions in the USA, Europe, and the UK, to date, no estimates exist for Canada. To address this, we calculated an estimate of annual avian mortality attributed to vehicular collisions during the breeding and fledging season, in Canadian ecozones, by applying North American literature values for avian mortality to Canadian road networks. Because owls are particularly susceptible to collisions with vehicles, we also estimated the number of roadkilled Barn owls (Tyto alba) in its last remaining range within Canada. (This species is on the IUCN red list and is also listed federally as threatened; Committee on the Status of Endangered Wildlife in Canada 2010, International Union for the Conservation of Nature 2012). Through seven Canadian studies in existence, 80 species and 2,834 specimens have been found dead on roads representing species from 14 orders of birds. On Canadian 1 and 2-lane paved roads outside of major urban centers, the unadjusted number of bird mortalities/yr during an estimated 4-mo (122-d) breeding and fledging season for most birds in Canada was 4,650,137 on roads traversing through deciduous, coniferous, cropland, wetlands and nonagricultural landscapes with less than 10% treed area. On average, this represents 1,167 birds killed/100 km in Canada. Adjusted for scavenging, this estimate was 13,810,906 (3,462 dead birds/100 km). For barn owls, the unadjusted number of birds killed annually on 4-lane roads during the breeding and fledging season, within the species geographic range in southern British Columbia, was estimated as 244 owls and, when adjusted for scavenging and observer bias (3.6 factor), the total was 851 owls.

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’ (0

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.

The counter-propagating Rossby-wave perspective on baroclinic instability. Part IV: Nonlinear life cycles

Pairs of counter-propagating Rossby waves (CRWs) can be used to describe baroclinic instability in linearized primitive-equation dynamics, employing simple propagation and interaction mechanisms at only two locations in the meridional plane—the CRW ‘home-bases’. Here, it is shown how some CRW properties are remarkably robust as a growing baroclinic wave develops nonlinearly. For example, the phase difference between upper-level and lower-level waves in potential-vorticity contours, defined initially at the home-bases of the CRWs, remains almost constant throughout baroclinic wave life cycles, despite the occurrence of frontogenesis and Rossby-wave breaking. As the lower wave saturates nonlinearly the whole baroclinic wave changes phase speed from that of the normal mode to that of the self-induced phase speed of the upper CRW. On zonal jets without surface meridional shear, this must always act to slow the baroclinic wave. The direction of wave breaking when a basic state has surface meridional shear can be anticipated because the displacement structures of CRWs tend to be coherent along surfaces of constant basic-state angular velocity, U. This results in up-gradient horizontal momentum fluxes for baroclinically growing disturbances. The momentum flux acts to shift the jet meridionally in the direction of the increasing surface U, so that the upper CRW breaks in the same direction as occurred at low levels