Reflexiones sobre la educación tecnológica desde el enfoque CTS.

Los autores son miembros del Grupo Argo de Renovación Pedagógica y profesores del instituto de Enseñanza Secundaria número cinco de Avilés, Asturias (España); además son profesores itinerantes de la Cátedra CTS+I de OEI y del Curso Virtual sobre el enfoque CTS en la Enseñanza de las Ciencias, organizado por dicho Organismo y la Universidad de Oviedo. Resumen basado en el de la publicación

Controversias tecnocientíficas : diez casos simulados sobre ciencia, tecnología, sociedad y valores.

Resumen basado en el de la publicación

Las plataformas petrolíferas : un caso sobre energía, combustibles fósiles y sostenibilidad.

Se presenta una actividad dirigida a los docentes con el objetivo de crear en el aula escenarios democráticos propicios para el fomento de la participación pública. Incluye una unidad didáctica complementada con una serie de documentos que tratan en torno a una noticia (documento 1) sobre la implantación de una plataforma petrolífera en la costa cantábrica. Además de la noticia se presenta un cuestionario (documento 2) que puede ser utilizado al comienzo y al final de la simulación para conocer las variaciones en las ideas y actitudes de los alumnos ante el tema; unas orientaciones (documento 3) que definen el perfil de cada actor social y sugieren el tipo de investigaciones que puede desarrollar cada equipo para defender su postura en el debate. Varios documento polémicos (documento 4) que completan la información de la noticia inicial y desarrollan de forma verosímil argumentos e informaciones que podría utilizar cada actor social en la controversia. Un cuestionario (documento 5) que permitirá centrar el debate y facilitará la decisión final. Indicaciones y pautas (documento 6) que guiarán el trabajo de los equipos y facilitarán los procedimientos para su evaluación. Por último una serie de informaciones complementarias (documento 7) que profundizan en el tema y pueden ser utilizadas por los alumnos como primera fuente de información. El último de los documentos que se incluyen es una relación de sitios de Internet en los que se puede encontrar más información relacionada con el tema de la controversia.

Las antenas de telefonía : un caso sobre radiaciones, riesgos biológicos y vida cotidiana.

Se presenta una actividad dirigida a los docentes con el objetivo de crear en el aula escenarios democráticos propicios para el fomento de la participación pública. Incluye una guía didáctica complementada con una serie de documentos que tratan en torno a una noticia (documento 1) sobre la colocación de antenas de telefonía en los edificios, en este caso concreto en un centro escolar. Además de la noticia se presenta un cuestionario (documento 2) que puede ser utilizado al comienzo y al final de la simulación para conocer las variaciones en las ideas y actitudes de los alumnos ante el tema; unas orientaciones (documento 3) que definen el perfil de cada actor social y sugieren el tipo de investigaciones que puede desarrollar cada equipo para defender su postura en el debate. Varios documento polémicos (documento 4) que completan la información de la noticia inicial y desarrollan de forma verosímil argumentos e informaciones que podría utilizar cada actor social en la controversia. Un cuestionario (documento 5) que permitirá centrar el debate y facilitará la decisión final. Indicaciones y pautas (documento 6) que guiarán el trabajo de los equipos y facilitarán los procedimientos para su evaluación. Por último una serie de informaciones complementarias (documento 7) que profundizan en el tema y pueden ser utilizadas por los alumnos como primera fuente de información. El último de los documentos que se incluyen es una relación de sitios de Internet en los que se puede encontrar más información relacionada con el tema de la controversia.

Impact of hydrographic data assimilation on the modelled Atlantic meridional overturning circulation

Here we make an initial step toward the development of an ocean assimilation system that can constrain the modelled Atlantic Meridional Overturning Circulation (AMOC) to support climate predictions. A detailed comparison is presented of 1° and 1/4° resolution global model simulations with and without sequential data assimilation, to the observations and transport estimates from the RAPID mooring array across 26.5° N in the Atlantic. Comparisons of modelled water properties with the observations from the merged RAPID boundary arrays demonstrate the ability of in situ data assimilation to accurately constrain the east-west density gradient between these mooring arrays. However, the presence of an unconstrained "western boundary wedge" between Abaco Island and the RAPID mooring site WB2 (16 km offshore) leads to the intensification of an erroneous southwards flow in this region when in situ data are assimilated. The result is an overly intense southward upper mid-ocean transport (0–1100 m) as compared to the estimates derived from the RAPID array. Correction of upper layer zonal density gradients is found to compensate mostly for a weak subtropical gyre circulation in the free model run (i.e. with no assimilation). Despite the important changes to the density structure and transports in the upper layer imposed by the assimilation, very little change is found in the amplitude and sub-seasonal variability of the AMOC. This shows that assimilation of upper layer density information projects mainly on the gyre circulation with little effect on the AMOC at 26° N due to the absence of corrections to density gradients below 2000 m (the maximum depth of Argo). The sensitivity to initial conditions was explored through two additional experiments using a climatological initial condition. These experiments showed that the weak bias in gyre intensity in the control simulation (without data assimilation) develops over a period of about 6 months, but does so independently from the overturning, with no change to the AMOC. However, differences in the properties and volume transport of North Atlantic Deep Water (NADW) persisted throughout the 3 year simulations resulting in a difference of 3 Sv in AMOC intensity. The persistence of these dense water anomalies and their influence on the AMOC is promising for the development of decadal forecasting capabilities. The results suggest that the deeper waters must be accurately reproduced in order to constrain the AMOC.

Steric sea level variability (1993-2010) in an ensemble of ocean reanalyses and objective analyses

Quantifying the effect of the seawater density changes on sea level variability is of crucial importance for climate change studies, as the sea level cumulative rise can be regarded as both an important climate change indicator and a possible danger for human activities in coastal areas. In this work, as part of the Ocean Reanalysis Intercomparison Project, the global and regional steric sea level changes are estimated and compared from an ensemble of 16 ocean reanalyses and 4 objective analyses. These estimates are initially compared with a satellite-derived (altimetry minus gravimetry) dataset for a short period (2003–2010). The ensemble mean exhibits a significant high correlation at both global and regional scale, and the ensemble of ocean reanalyses outperforms that of objective analyses, in particular in the Southern Ocean. The reanalysis ensemble mean thus represents a valuable tool for further analyses, although large uncertainties remain for the inter-annual trends. Within the extended intercomparison period that spans the altimetry era (1993–2010), we find that the ensemble of reanalyses and objective analyses are in good agreement, and both detect a trend of the global steric sea level of 1.0 and 1.1 ± 0.05 mm/year, respectively. However, the spread among the products of the halosteric component trend exceeds the mean trend itself, questioning the reliability of its estimate. This is related to the scarcity of salinity observations before the Argo era. Furthermore, the impact of deep ocean layers is non-negligible on the steric sea level variability (22 and 12 % for the layers below 700 and 1500 m of depth, respectively), although the small deep ocean trends are not significant with respect to the products spread.

Ocean heat content variability and change in an ensemble of ocean reanalyses

Accurate knowledge of the location and magnitude of ocean heat content (OHC) variability and change is essential for understanding the processes that govern decadal variations in surface temperature, quantifying changes in the planetary energy budget, and developing constraints on the transient climate response to external forcings. We present an overview of the temporal and spatial characteristics of OHC variability and change as represented by an ensemble of dynamical and statistical ocean reanalyses (ORAs). Spatial maps of the 0–300 m layer show large regions of the Pacific and Indian Oceans where the interannual variability of the ensemble mean exceeds ensemble spread, indicating that OHC variations are well-constrained by the available observations over the period 1993–2009. At deeper levels, the ORAs are less well-constrained by observations with the largest differences across the ensemble mostly associated with areas of high eddy kinetic energy, such as the Southern Ocean and boundary current regions. Spatial patterns of OHC change for the period 1997–2009 show good agreement in the upper 300 m and are characterized by a strong dipole pattern in the Pacific Ocean. There is less agreement in the patterns of change at deeper levels, potentially linked to differences in the representation of ocean dynamics, such as water mass formation processes. However, the Atlantic and Southern Oceans are regions in which many ORAs show widespread warming below 700 m over the period 1997–2009. Annual time series of global and hemispheric OHC change for 0–700 m show the largest spread for the data sparse Southern Hemisphere and a number of ORAs seem to be subject to large initialization ‘shock’ over the first few years. In agreement with previous studies, a number of ORAs exhibit enhanced ocean heat uptake below 300 and 700 m during the mid-1990s or early 2000s. The ORA ensemble mean (±1 standard deviation) of rolling 5-year trends in full-depth OHC shows a relatively steady heat uptake of approximately 0.9 ± 0.8 W m−2 (expressed relative to Earth’s surface area) between 1995 and 2002, which reduces to about 0.2 ± 0.6 W m−2 between 2004 and 2006, in qualitative agreement with recent analysis of Earth’s energy imbalance. There is a marked reduction in the ensemble spread of OHC trends below 300 m as the Argo profiling float observations become available in the early 2000s. In general, we suggest that ORAs should be treated with caution when employed to understand past ocean warming trends—especially when considering the deeper ocean where there is little in the way of observational constraints. The current work emphasizes the need to better observe the deep ocean, both for providing observational constraints for future ocean state estimation efforts and also to develop improved models and data assimilation methods.

An assessment of upper ocean salinity content from the ocean reanalyses inter-comparison project (ORA-IP)

Many institutions worldwide have developed ocean reanalyses systems (ORAs) utilizing a variety of ocean models and assimilation techniques. However, the quality of salinity reanalyses arising from the various ORAs has not yet been comprehensively assessed. In this study, we assess the upper ocean salinity content (depth-averaged over 0–700 m) from 14 ORAs and 3 objective ocean analysis systems (OOAs) as part of the Ocean Reanalyses Intercomparison Project. Our results show that the best agreement between estimates of salinity from different ORAs is obtained in the tropical Pacific, likely due to relatively abundant atmospheric and oceanic observations in this region. The largest disagreement in salinity reanalyses is in the Southern Ocean along the Antarctic circumpolar current as a consequence of the sparseness of both atmospheric and oceanic observations in this region. The West Pacific warm pool is the largest region where the signal to noise ratio of reanalysed salinity anomalies is >1. Therefore, the current salinity reanalyses in the tropical Pacific Ocean may be more reliable than those in the Southern Ocean and regions along the western boundary currents. Moreover, we found that the assimilation of salinity in ocean regions with relatively strong ocean fronts is still a common problem as seen in most ORAs. The impact of the Argo data on the salinity reanalyses is visible, especially within the upper 500m, where the interannual variability is large. The increasing trend in global-averaged salinity anomalies can only be found within the top 0–300m layer, but with quite large diversity among different ORAs. Beneath the 300m depth, the global-averaged salinity anomalies from most ORAs switch their trends from a slightly growing trend before 2002 to a decreasing trend after 2002. The rapid switch in the trend is most likely an artefact of the dramatic change in the observing system due to the implementation of Argo.

Changes in facial morphology after adenotonsillectomy in mouth-breathing children

Background. Morphological and dentofacial alterations have been attributed to impaired respiratory function. Objective. To examine the influence of mouth breathing (MB) on children facial morphology before and after adenoidectomy or adenotonsillectomy. Methods. Thirty-three MB children who restored nasal breathing (NB) after surgery and 22 NB children were evaluated. Both groups were submitted to lateral cephalometry, at time 1 (T1) before and at time 2 (T2) 28months on average postoperatively. Results. Comparison between the MB and NB groups at T1 showed that mouth breathers had higher inclination of the mandibular plane; more obtuse gonial angle; dolichofacial morphology; and a decrease in the total and inferior posterior facial heights. Twenty-eight months after the MB surgical intervention, they still presented a dolichofacial morphologic pattern. During this period, MB altered the face growth direction and decreased their mandible plane inclination, with reduction in the SN.GoGn, PP.MP, SNGn, and ArGo.GoMe parameters as well as an increase in BaN.PtGn. Conclusion. After the MB rehabilitation, children between 3 and 6years old presented significant normalization in the mandibular growth direction, a decrease in the mandible inclination, and an increase in the posterior facial height. Instead, they still persisted with a dolichofacial pattern when compared with nasal breathers. © 2011 The Authors. International Journal of Paediatric Dentistry © 2011 BSPD, IAPD and Blackwell Publishing Ltd.

Construção de perfis de temperatura a partir de dados de Satélites,Climatologia e dados in situ

A aquisição de dados da estrutura termohalina dos oceanos sempre foi limitada pelo alto custo das missões oceanográficas. Sistemas de amostragem in situ menos dispendiosos, como o lançamento de XBTs por navios de oportunidade, a utilização de bóias de deriva, e mais recentemente, de sistemas de observação autõnomos como gliders e flutuadores Argo, foram concebidos como alternativas aos cruzeiros. Estes sistemas são capazes de cobrir vastas porções oceanicas e de fornecer grande quantidade de medições, porem seus dados nem sempre estão disponíveis ou mesmo são adequados `a resolução de um determinado problema ou ao estudo de um fenômeno em questão, devido principalmente à sua falta de sinopticidade e/ou cobertura espacial irregular. Sensores orbitais provaram ser valiosos e comparativamente possuem excelente periodicidade e cobertura espacial, mas suas observações são limitadas apenas à superfície dos oceanos. Assim, a capacidade de se inferir com boa precisão a estrutura termohalina de feições oceanográficas à partir de uma amostragem reduzida e/ou utilizando medições¸ indiretas é desejável e vem sido aprimorada em diversos trabalhos. Métodos clássicos incluem o desenvolvimento de modelos de feição pelo ajuste de curvas paramétricas (e.g. GANGOPADHYAY et al., 1997; CHU et al., 1999) e a reconstrução de perfis utilizando modos EOF (e.g. CARNES et al., 1990; AGARWAL et al., 2007)

Wind-driven cross-equatorial flow in the Indian ocean

Máster en Oceanografía

Flujos meridionales en el Océano Índico Ecuatorial

[ES]Un modelo estacionario propuesto por Joyce (1988a) es evaluado en el Océano Índico ecuatorial, usando el estrés de vientos NCEP y temperaturas y salinidades de WOA05 y Argo. El transporte zonal integrado de los datos WOA05 se parece al de los datos Argo en el monzón de invierno (WM) y en los periodos de transición (TP), presentando valores mayores en el caso de datos Argo. En cambio, para el monzón de verano (SM) los transportes zonales integrados de los datos WOA05 y Argo tienen direcciones opuestas debido a que en los datos de WOA05 la Corriente de Somalia (SC) es débil y casi inexistente. Aunque los datos Argo tienen mayor cantidad de estructuras mesoscalares que los datos WOA05, los datos Argo obtienen una SC que se ajusta mejor a los estudios previos y, en consecuencia, los datos Argos son los únicos que serán utilizados para estimar transporte de volumen y calor. Los datos Argo muestran una SC que fluye hacia el sur durante el WM y hacia el norte durante el SM, y un flujo en el océano interior contrario a la corriente. Durante el WM, la SC es somera (~200dbar) y bajo ella fluye una contracorriente. El transporte de calor meridional estimado para datos Argo muestra una inversión estacional. El transporte de calor neto en cada estación tiene la misma dirección que el calor transportado por la SC.

Towards the construction of a validated numerical system to study the mesoscale dynamics of the North East Atlantic (2003-2006)

Máster en Oceanografía

Multiscale variability in the North Atlantic Ocean

Programa de doctorado, Oceanografía ; 2004-2006

Observing Biogeochemical Cycles at Global Scales With Profiling Floats and Gliders Prospects for a Global Array

Chemical and biological sensor technologies have advanced rapidly in the past five years. Sensors that require low power and operate for multiple years are now available for oxygen, nitrate, and a variety of bio-optical properties that serve as proxies for important components of the carbon cycle (e.g., particulate organic carbon). These sensors have all been deployed successfully for long periods, in some cases more than three years, on platforms such as profiling floats or gliders. Technologies for pH, pCO(2), and particulate inorganic carbon are maturing rapidly as well. These sensors could serve as the enabling technology for a global biogeochemical observing system that might operate on a scale comparable to the current Argo array. Here, we review the scientific motivation and the prospects for a global observing system for ocean biogeochemistry.