The science teacher's activity-a-day: over 180 reproducible pages of kick, fun projects that illustrate basic concepts.

Recurso para enseñar ciencias a los estudiantes de secundaria. Cada una de las ciento ochenta actividades tiene una duración de cinco minutos y están pensadas para captar la atención del alumno. Comienza con una breve explicación del concepto sobre el que se va a centrar e incluye una lista de materiales, el procedimiento a seguir, las preguntas de seguimiento, y las ampliaciones. Dividido en tres unidades: Ciencias Físicas, Ciencias de la Vida, y Ciencias de la Tierra y del Universo, las actividades son especialmente estimulantes para alumnos kinestésicos, ya que la mayoría de estos alumnos aprenden mejor al estar físicamente en contacto con la experiencia de aprendizaje. Todas deben estar supervisadas por un adulto y los estudiantes seguir las reglas de seguridad de de las clases de ciencias.

English day. 'El inglés de hoy'.

Premios Nacionales 1999 a la Innovación Educativa. Anexo Documentación en C-Innov. 14

La educaci??n intercultural : un reto en el presente de Europa = Intercultural education : a present-day challenge for Europe

Edici??n biling??e en espa??ol e ingl??s

A comparison of social-emotional patterns of day versus residential students enrolled in an oral educational setting

This paper reviews a study of CID students and their scores on the Meadow-Kendall Social-Emotional Assessment Inventory test (SEAI).

Monitoring present day changes in water vapour and the radiative energy balance using satellite data, reanalyses and models

A combination of satellite data, reanalysis products and climate models are combined to monitor changes in water vapour, clear-sky radiative cooling of the atmosphere and precipitation over the period 1979-2006. Climate models are able to simulate observed increases in column integrated water vapour (CWV) with surface temperature (Ts) over the ocean. Changes in the observing system lead to spurious variability in water vapour and clear-sky longwave radiation in reanalysis products. Nevertheless all products considered exhibit a robust increase in clear-sky longwave radiative cooling from the atmosphere to the surface; clear-sky longwave radiative cooling of the atmosphere is found to increase with Ts at the rate of ~4 Wm-2 K-1 over tropical ocean regions of mean descending vertical motion. Precipitation (P) is tightly coupled to atmospheric radiative cooling rates and this implies an increase in P with warming at a slower rate than the observed increases in CWV. Since convective precipitation depends on moisture convergence, the above implies enhanced precipitation over convective regions and reduced precipitation over convectively suppressed regimes. To quantify this response, observed and simulated changes in precipitation rate are analysed separately over regions of mean ascending and descending vertical motion over the tropics. The observed response is found to be substantially larger than the model simulations and climate change projections. It is currently not clear whether this is due to deficiencies in model parametrizations or errors in satellite retrievals.

Neolithic woodland composition and exploitation in the Southern Levant: a comparison between archaeobotanical remains from WF16 and present day woodland at Hammam Adethni

Excavations at the Pre-Pottery Neolithic site of WF16 in the Southern Levant produced an archaeobotanical assemblage constituted by plant macro-fossils and wood charcoal. As with all such assemblages, its species composition will most likely provide a biased reflection of those within the Neolithic woodland that had been exploited owing to cultural selection and differential preservation. As a means of facilitating its interpretation, a survey was undertaken of a relatively undisturbed patch of gallery woodland associated with a permanent water course at Hammam Adethni, approximately four kilometres south-east of WF16. The substantial overlap of the species within this woodland and those in the archaeobotanical assemblage suggests that this present-day woodland provides an analogue for that of the Neolithic and may therefore indicate what other plant resources the inhabitants of WF16 may have exploited, but which have left no archaeological trace. The interpretation of the results is supported by a comparative study of wood charcoal from present-day Bedouin hearths in Wadi Faynan.