In situ (enciclopèdia audiovisual de les ciències i les tècniques) : ones i vibracions. 'In situ (enciclopedia audiovisual de las ciencias y las técnicas) : ondas y vibraciones'.

Este vídeo forma parte de la Enciclopedia Audiovisual de las Ciencias y las Técnicas, y se estructura en capítulos de cuatro minutos. Cada capítulo expone el estudio de un objeto o fenómeno científico y propone: recordatorios, definiciones, exploraciones para entender mejor un funcionamiento, animaciones para representar fenómenos complejos, descubrimientos y aplicaciones y puntos que remiten a otros capítulos de la enciclopedia directamente relacionados con el tema que se trata. Los capítulos incluidos en este volumen son: la cámara fotográfica; la luz de colores; la propagación de la luz; el láser; las ondas electromagnéticas; los rayos X y los rayos gamma; el sónar; el radar; las ondas sonoras; la guitarra; el micrófono; el altavoz; la modulación y la frecuencia, y, las antenas.

Las celebraciones de centenarios en ciencias como recurso didáctico : sugerencias para el año 2004.

Resumen basado en el de la publicación

Validación de un protocolo para la medición de la velocidad de golpeo en fútbol.

Resumen tomado de la publicación

I'm coming to get you!

Un horrible monstruo surge de las profundidades de otra galaxia en una nave espacial y se dirige a un bonito planeta azul llamado Tierra. El monstruo localiza en su radar al pequeño Tommy Brown, que, en ese momento, se marcha a la cama asustado de las historias de miedo que le acaban de contar.

Aplicaciones de la electrónica.

Repaso del desarrollo de la electrónica a lo largo del siglo XX, desde el descubrimiento de los electrones, las diferentes ramas de estudio, los diferentes aparatos electrónicos desarrollados como el oscilógrafo de rayos catódicos, el radar, y otras aplicaciones electrónicas como la telemedida y telecontrol.

Anàlisi cronològica de la pesca al Port de Llançà: període 1977-1996

A partir del buidatge exhaustiu dels fulls de subhasta del peix i de les fitxes tècniques de les embarcacions de la Confraria del Port de Llançà, es fa una anàlisi cronològica qualitativa i quantitativa dels darrers vint anys de pesca. La flota, inicialment constituïda per barques d'arrossegament i de pesca artesanal (palangre petit i tresmail), ha anat evolucionant, i ha quedat bàsicament constituïda actualment pel ròssec i el palangre de fons, que ha substituit progressivament la pesca artesanal. Les pesqueries, notablement multiespecífiques els primers anys, van donar pas, bàsicament amb la incorporació del radar, a una pesca molt més selectiva, dominada essencialment per la captura de lluç entre els anys 1980 i 1985. La progressiva incorporació del palangre de fons fa que a partir del 1986 es tendeixi novament cap a una captura més multiespecífica, perd amb canvis qualitatius importants en la composició d'espècies capturades en relació amb els primers anys

Estratégias de inovação visando a competitividade empresarial- um estudo multicasos de gestão dos hotéis portas da Amazónia e faraó no município de Belém-Pará

Esta dissertação teve como objetivo principal analisar como a Estratégia da Inovação poderia ser empregada em benefício da competitividade das organizações hoteleiras, tendo em vista as experiências de inovação dos Hotéis Portas da Amazônia e Faraó. Os Hotéis Portas da Amazônia e Faraó destacam-se pela realização de experiências inovadoras, o primeiro apresenta uma proposta de Hotel Histórico, nasceu a partir da restauração de um casarão do início do século XIX e atende o segmento do Turismo Internacional e o segundo uma proposta de Hotel Temático, sendo entitulado o primeiro hotel temático do norte. O acirramento da concorrência no mercado hoteleiro de Belém-Pará, devido aos novos entrantes (grandes redes hoteleiras) e substitutos como flats, está provocando a redução das margens de lucro ademais está obrigando os gestores das empresas de micro e pequeno porte a repensarem suas estratégias de competição. Sendo que a inovação é uma estratégia que pode contribuir para criação e sustentação da vantagem competitiva. A metodologia adotada nesta investigação foi inicialmente o levantamento bibliográfico. Além disso, foram aplicadas entrevistas semi-estruturadas para os gestores dos hotéis. A entrevista baseou-se no Radar da Inovação para a classificação das Estratégias de Inovação. A investigação revelou que o empresário do Hotel Portas da Amazônia realizou uma inovação em modelo de negócios e inovação em descoberta de um novo mercado. Porém, no Hotel Faraó, identificou-se apenas um caso de inovação incremental em suas instalações como na decoração do prédio, pois para a proposta de um hotel temático, a gestão precisaria explorar a experiência do cliente. Nos dois casos, constatou-se que várias dimensões da inovação são negligenciadas como ofertas, experiências do consumidor e a inovação na organização.

Solo los Hechos 2001-2002. Un breve recorrido por las relaciones de los Estados Unidos en materia de defensa y seguridad con América Latina y El Caribe

A comienzos de septiembre del año 2001, el Congreso de los Estados Unidos se encontraba inmerso en el debate de algunos temas de seguridad nacional relacionados con América Latina, entre ellos, la nueva Iniciativa Andina Antidrogas propuesta por la administración Bush y la continuidad de la presencia militar en la isla puertorriqueña de Vieques. Después del 11 de septiembre, y a pesar de su importancia crucial en la región, ambos temas pasaron a ser señales casi imperceptibles en la pantalla del radar político de Washington, y si bien es cierto que los programas militares que los Estados Unidos desarrollan en América Latina no se detendrán, es posible anticipar algunos cambios en su desarrollo como respuesta a los ataques terroristas de que fue objeto este país.

The biometeorology of high-altitude insect layers.

Flight at high altitude is part of a migration strategy that maximises insect population displacement. This thesis represents the first substantial analysis of insect migration and layering in Europe. Vertical-looking entomological radar has revealed specific characteristics of high-altitude flight: in particular layering (where a large proportion of the migrating insects are concentrated in a narrow altitude band). The meteorological mechanisms underpinning the formation of these layers are the focus of this thesis. Aerial netting samples and radar data revealed four distinct periods of high-altitude insect migration: dawn, daytime, dusk, and night-time. The most frequently observed nocturnal profiles during the summertime were layers. It is hypothesised that nocturnal layers initiate at a critical altitude (200–500 m above ground level) and time (20:00–22:00 hours UTC). Case study analysis, statistical analysis, and a Lagrangian trajectory model showed that nocturnal insect layers probably result from the insects’ response to meteorological conditions. Temperature was the variable most correlated with nocturnal insect layer presence and intensity because insects are poikilothermic, and temperatures experienced during high-altitude migration in temperate climates are expected to be marginal for many insects’ flight. Hierarchical effects were detected such that other variables—specifically wind speed—were only correlated with insect layer presence and intensity once temperatures were warm. The trajectory model developed comprised: (i) insect flight characteristics; (ii) turbulent winds (which cause vertical spread of the layer); and (iii) mean wind speed, which normally leads to horizontal displacements of hundreds of kilometres in a single migratory flight. This thesis has revealed that there is considerable migratory activity over the UK in the summer months, and a range of fascinating phenomena can be observed (including layers). The UK has moved from one of the least studied to perhaps the best studied environments of aerial insect migration and layering in the world.

Relationships between lightning and properties of convective cloud clusters

Satellite observations of convective system properties and lightning flash rate are used to investigate the ability of potential lightning parameterizations to capture both the dominant land-ocean contrast in lightning occurrence and regional differences between Africa, the Amazon and the islands of the maritime continent. As found in previous studies, the radar storm height is tightly correlated with the lightning flash rate. A roughly second order power-law fit to the mean radar echo top height above the 0C isotherm is shown to capture both regional and land-ocean contrasts in lightning occurrence and flash rate using a single set of parameters. Recent developments should soon make it possible to implement a parameterization of this kind in global models. Parameterizations based on cloud top height, convective rain rate and convective rain fraction all require the use of separate fits over land and ocean and fail to capture observed differences between continental regions.

Deep Convective System Evolution over Africa and the Tropical Atlantic

In the tropical African and neighboring Atlantic region there is a strong contrast in the properties of deep convection between land and ocean. Here, satellite radar observations are used to produce a composite picture of the life cycle of convection in these two regions. Estimates of the broadband thermal flux from the geostationary Meteosat-8 satellite are used to identify and track organized convective systems over their life cycle. The evolution of the system size and vertical extent are used to define five life cycle stages (warm and cold developing, mature, cold and warm dissipating), providing the basis for the composite analysis of the system evolution. The tracked systems are matched to overpasses of the Tropical Rainfall Measuring Mission satellite, and a composite picture of the evolution of various radar and lightning characteristics is built up. The results suggest a fundamental difference in the convective life cycle between land and ocean. African storms evolve from convectively active systems with frequent lightning in their developing stages to more stratiform conditions as they dissipate. Over the Atlantic, the convective fraction remains essentially constant into the dissipating stages, and lightning occurrence peaks late in the life cycle. This behavior is consistent with differences in convective sustainability in land and ocean regions as proposed in previous studies. The area expansion rate during the developing stages of convection is used to provide an estimate of the intensity of convection. Reasonable correlations are found between this index and the convective system lifetime, size, and depth.

The Convective Storm Initiation Project

The Convective Storm Initiation Project (CSIP) is an international project to understand precisely where, when, and how convective clouds form and develop into showers in the mainly maritime environment of southern England. A major aim of CSIP is to compare the results of the very high resolution Met Office weather forecasting model with detailed observations of the early stages of convective clouds and to use the newly gained understanding to improve the predictions of the model. A large array of ground-based instruments plus two instrumented aircraft, from the U.K. National Centre for Atmospheric Science (NCAS) and the German Institute for Meteorology and Climate Research (IMK), Karlsruhe, were deployed in southern England, over an area centered on the meteorological radars at Chilbolton, during the summers of 2004 and 2005. In addition to a variety of ground-based remote-sensing instruments, numerous rawin-sondes were released at one- to two-hourly intervals from six closely spaced sites. The Met Office weather radar network and Meteosat satellite imagery were used to provide context for the observations made by the instruments deployed during CSIP. This article presents an overview of the CSIP field campaign and examples from CSIP of the types of convective initiation phenomena that are typical in the United Kingdom. It shows the way in which certain kinds of observational data are able to reveal these phenomena and gives an explanation of how the analyses of data from the field campaign will be used in the development of an improved very high resolution NWP model for operational use.

Analysis of convectively-generated gravity waves in mesoscale model simulations and wind profiler observations

The characteristics of convectively-generated gravity waves during an episode of deep convection near the coast of Wales are examined in both high resolution mesoscale simulations [with the (UK) Met Oce Unified Model] and in observations from a Mesosphere-Stratosphere-Troposphere (MST) wind profiling Doppler radar. Deep convection reached the tropopause and generated vertically propagating, high frequency waves in the lower stratosphere that produced vertical velocity perturbations O(1 m/s). Wavelet analysis is applied in order to determine the characteristic periods and wavelengths of the waves. In both the simulations and observations, the wavelet spectra contain several distinct preferred scales indicated by multiple spectral peaks. The peaks are most pronounced in the horizontal spectra at several wavelengths less than 50 km. Although these peaks are most clear and of largest amplitude in the highest resolution simulations (with 1 km horizontal grid length), they are also evident in coarser simulations (with 4 km horizontal grid length). Peaks also exist in the vertical and temporal spectra (between approximately 2.5 and 4.5 km, and 10 to 30 minutes, respectively) with good agreement between simulation and observation. Two-dimensional (wavenumber-frequency) spectra demonstrate that each of the selected horizontal scales contains peaks at each of preferred temporal scales revealed by the one- dimensional spectra alone.

Tripleclouds: an efficient method for representing horizontal cloud inhomogeneity in 1D radiation schemes by using three regions at each height

Radiation schemes in general circulation models currently make a number of simplifications when accounting for clouds, one of the most important being the removal of horizontal inhomogeneity. A new scheme is presented that attempts to account for the neglected inhomogeneity by using two regions of cloud in each vertical level of the model as opposed to one. One of these regions is used to represent the optically thinner cloud in the level, and the other represents the optically thicker cloud. So, along with the clear-sky region, the scheme has three regions in each model level and is referred to as “Tripleclouds.” In addition, the scheme has the capability to represent arbitrary vertical overlap between the three regions in pairs of adjacent levels. This scheme is implemented in the Edwards–Slingo radiation code and tested on 250 h of data from 12 different days. The data are derived from cloud retrievals using radar, lidar, and a microwave radiometer at Chilbolton, southern United Kingdom. When the data are grouped into periods equivalent in size to general circulation model grid boxes, the shortwave plane-parallel albedo bias is found to be 8%, while the corresponding bias is found to be less than 1% using Tripleclouds. Similar results are found for the longwave biases. Tripleclouds is then compared to a more conventional method of accounting for inhomogeneity that multiplies optical depths by a constant scaling factor, and Tripleclouds is seen to improve on this method both in terms of top-of-atmosphere radiative flux biases and internal heating rates.

Calibration of uncertain flood inundation models using remotely sensed water levels

A traditional method of validating the performance of a flood model when remotely sensed data of the flood extent are available is to compare the predicted flood extent to that observed. The performance measure employed often uses areal pattern-matching to assess the degree to which the two extents overlap. Recently, remote sensing of flood extents using synthetic aperture radar (SAR) and airborne scanning laser altimetry (LIDAR) has made more straightforward the synoptic measurement of water surface elevations along flood waterlines, and this has emphasised the possibility of using alternative performance measures based on height. This paper considers the advantages that can accrue from using a performance measure based on waterline elevations rather than one based on areal patterns of wet and dry pixels. The two measures were compared for their ability to estimate flood inundation uncertainty maps from a set of model runs carried out to span the acceptable model parameter range in a GLUE-based analysis. A 1 in 5-year flood on the Thames in 1992 was used as a test event. As is typical for UK floods, only a single SAR image of observed flood extent was available for model calibration and validation. A simple implementation of a two-dimensional flood model (LISFLOOD-FP) was used to generate model flood extents for comparison with that observed. The performance measure based on height differences of corresponding points along the observed and modelled waterlines was found to be significantly more sensitive to the channel friction parameter than the measure based on areal patterns of flood extent. The former was able to restrict the parameter range of acceptable model runs and hence reduce the number of runs necessary to generate an inundation uncertainty map. A result of this was that there was less uncertainty in the final flood risk map. The uncertainty analysis included the effects of uncertainties in the observed flood extent as well as in model parameters. The height-based measure was found to be more sensitive when increased heighting accuracy was achieved by requiring that observed waterline heights varied slowly along the reach. The technique allows for the decomposition of the reach into sections, with different effective channel friction parameters used in different sections, which in this case resulted in lower r.m.s. height differences between observed and modelled waterlines than those achieved by runs using a single friction parameter for the whole reach. However, a validation of the modelled inundation uncertainty using the calibration event showed a significant difference between the uncertainty map and the observed flood extent. While this was true for both measures, the difference was especially significant for the height-based one. This is likely to be due to the conceptually simple flood inundation model and the coarse application resolution employed in this case. The increased sensitivity of the height-based measure may lead to an increased onus being placed on the model developer in the production of a valid model