Application of Mathieu functions for the study of non-slanted reflection gratings

In this work we prensent an analysis of non-slanted reflection gratings by using exact solution of the second order differential equation derived from Maxwell equations, in terms of Mathieu functions. The results obtained by using this method will be compared to those obtained by using the well known Kogelnik's Coupled Wave Theory which predicts with great accuracy the response of the efficieny of the zero and first order for volume phase gratings, for both reflection and transmission gratings.

Australian water mass variations from GRACE data linked to Indo-Pacific climate variability

Time-variable gravity data from the Gravity Recovery And Climate Experiment (GRACE) mission are used to study total water content over Australia for the period 2002–2010. A time-varying annual signal explains 61% of the variance of the data, in good agreement with two independent estimates of the same quantity from hydrological models. Water mass content variations across Australia are linked to Pacific and Indian Ocean variability, associated with El Niño-Southern Oscillation (ENSO) and the Indian Ocean Dipole (IOD), respectively. From 1989, positive (negative) IOD phases were related to anomalously low (high) precipitation in southeastern Australia, associated with a reduced (enhanced) tropical moisture flux. In particular, the sustained water mass content reduction over central and southern regions of Australia during the period 2006–2008 is associated with three consecutive positive IOD events.

Steric and mass-induced sea level variations in the Mediterranean Sea revisited

The total sea level variation (SLV) is the combination of steric and mass␣induced SLV, whose exact shares are key to understanding the oceanic response to climate system changes. Total SLV can be observed by radar altimetry satellites such as TOPEX/POSEIDON and Jason 1/2. The steric SLV can be computed through temperature and salinity profiles from in situ measurements or from ocean general circulation models (OGCM), which can assimilate the said observations. The mass-induced SLV can be estimated from its time-variable gravity (TVG) signals. We revisit this problem in the Mediterranean Sea estimating the observed, steric, and mass-induced SLV, for the latter we analyze the latest TVG data set from the GRACE (Gravity Recovery and Climate Experiment) satellite mission launched in 2002, which is 3.5 times longer than in previous studies, with the application of a two-stage anisotropic filter to reduce the noise in high-degree and -order spherical harmonic coefficients. We confirm that the intra-annual total SLV are only produced by water mass changes, a fact explained in the literature as a result of the wind field around the Gibraltar Strait. The steric SLV estimated from the residual of “altimetry minus GRACE” agrees in phase with that estimated from OGCMs and in situ measurements, although showing a higher amplitude. The net water fluxes through both the straits of Gibraltar and Sicily have also been estimated accordingly.

On the steric and mass-induced contributions to the annual sea level variations in the Mediterranean Sea

The sea level variation (SLVtotal) is the sum of two major contributions: steric and mass-induced. The steric SLVsteric is that resulting from the thermal and salinity changes in a given water column. It only involves volume change, hence has no gravitational effect. The mass-induced SLVmass, on the other hand, arises from adding or subtracting water mass to or from the water column and has direct gravitational signature. We examine the closure of the seasonal SLV budget and estimate the relative importance of the two contributions in the Mediterranean Sea as a function of time. We use ocean altimetry data (from TOPEX/Poseidon, Jason 1, ERS, and ENVISAT missions) to estimate SLVtotal, temperature, and salinity data (from the Estimating the Circulation and Climate of the Ocean ocean model) to estimate SLVsteric, and time variable gravity data (from Gravity Recovery and Climate Experiment (GRACE) Project, April 2002 to July 2004) to estimate SLVmass. We find that the annual cycle of SLVtotal in the Mediterranean is mainly driven by SLVsteric but moderately offset by SLVmass. The agreement between the seasonal SLVmass estimations from SLVtotal – SLVsteric and from GRACE is quite remarkable; the annual cycle reaches the maximum value in mid-February, almost half a cycle later than SLVtotal or SLVsteric, which peak by mid-October and mid-September, respectively. Thus, when sea level is rising (falling), the Mediterranean Sea is actually losing (gaining) mass. Furthermore, as SLVmass is balanced by vertical (precipitation minus evaporation, P–E) and horizontal (exchange of water with the Atlantic, Black Sea, and river runoff) mass fluxes, we compared it with the P–E determined from meteorological data to estimate the annual cycle of the horizontal flux.

Reply to comment by L. Fenoglio-Marc et al. on “On the steric and mass-induced contributions to the annual sea level variations in the Mediterranean Sea”

Reply to comment by L. Fenoglio-Marc et al. on “On the steric and mass-induced contributions to the annual sea level variations in the Mediterranean Sea”.

Steric sea-level variations inferred from combined Topex/Poseidon altimetry and GRACE gravimetry

In this study, we propose to estimate the steric sea-level variations over a < 2-year period (April 2002 through December 2003) by combining global mean sea level (GMSL) based on Topex/ Poseidon (T/P) altimetry with time-variable geoid averaged over the oceans, as observed by the GRACE (Gravity Recovery and Climate Experiment) satellite. In effect, altimetry-derived GMSL changes results from two contributions: Steric (thermal plus salinity) effects due to sea water density change and ocean mass change due to water exchange with atmosphere and continents. On the other hand, GRACE data over the oceans provide the ocean mass change component only. The paper first discusses the corrections to apply to the GRACE data. Then the steric contribution to the GMSL is estimated using GRACE and T/P data. Comparison with available thermal expansion based on in situ hydrographic data is performed.

Vertical crustal motion along the Mediterranean and Black Sea coast derived from ocean altimetry and tide gauge data

Tide gauge (TG) data along the northern Mediterranean and Black Sea coasts are compared to the sea-surface height (SSH) anomaly obtained from ocean altimetry (TOPEX/Poseidon and ERS-1/2) for a period of nine years (1993–2001). The TG measures the SSH relative to the ground whereas the altimetry does so with respect to the geocentric reference frame; therefore their difference would be in principle a vertical ground motion of the TG sites, though there are different error sources for this estimate as is discussed in the paper. In this study we estimate such vertical ground motion, for each TG site, from the slope of the SSH time series of the (non-seasonal) difference between the TG record and the altimetry measurement at a point closest to the TG. Where possible, these estimates are further compared with those derived from nearby continuous Global Positioning System (GPS) data series. These results on vertical ground motion along the Mediterranean and Black Sea coasts provide useful source data for studying, contrasting, and constraining tectonic models of the region. For example, in the eastern coast of the Adriatic Sea and in the western coast of Greece, a general subsidence is observed which may be related to the Adriatic lithosphere subducting beneath the Eurasian plate along the Dinarides fault.

Red de coordinación de la implantación del primer curso del Grado en Ingeniería en Sonido e Imagen

El profesorado de la red docente realizó durante el curso 2009/10 un proyecto para la planificación de las asignaturas del primer curso del Grado en Ingeniería en Sonido e Imagen de la Escuela Politécnica Superior, y nos toca ahora la puesta a punto del primer curso del Grado. En el marco creado por los nuevos estudios dentro del EEES, el proyecto tiene como objetivo principal es el seguimiento, coordinación, evaluación, y mejora de la planificación realizada el curso anterior ya con las nuevas experiencias.

Red de coordinación y seguimiento del primer curso del Grado en Ing. Sonido e Imagen en Telecomunicación (GISIT) de la Escuela Politécnica Superior

El profesorado de la red docente durante el curso 2011/12 ha realizado un proyecto coordinar las las asignaturas del primer curso del Grado en Ingeniería en Sonido e Imagen en Telecomunicación de la Escuela Politécnica Superior. Se ha realizado una puesta en común con los coordinadores de todos los cursos para realizar las recomendaciones de matriculación a los estudiantes que realizan su matricula a tiempo parcial o no superan cada curso todos los créditos matriculados. Se ha realizado un ajuste de los temarios con las asignaturas que comienzan su implantación en el siguiente curso y por otro lado una coordinación en la evaluación para eliminar las numerosas coincidencias de evaluaciones continuas, de diferentes actividades en cada semana.

Coordinación y seguimiento de los tres primeros cursos del Grado en Ing. Sonido e Imagen en Telecomunicación

El reto de implantar los nuevos grados exige un continuado esfuerzo de coordinación de las asignaturas de cada curso y de los diferentes cursos entres sí. En este trabajo se presentan los resultados de los diferentes proyectos que se han realizado para coordinar las asignaturas de los tres primeros cursos del Grado en Ingeniería en Sonido e Imagen en Telecomunicación de la Escuela Politécnica Superior. Además se analiza la coordinación de los proyectos entre sí, analizando los cambios surgidos en las fichas de las asignaturas, evaluación, metodología, etc. También se presenta una puesta en común con los coordinadores de todos los cursos para realizar las recomendaciones de matriculación a los estudiantes que realizan su matrícula a tiempo parcial o no superan cada curso todos los créditos matriculados. Y por último, se estudia la continuidad con los contenidos de las asignaturas que comienzan su implantación en el siguiente curso y por otro lado la coordinación en la evaluación para eliminar las numerosas coincidencias de evaluaciones continuas, de diferentes actividades en cada semana.

Comisión de plan de estudios de la titulación de Ingeniería Técnica de Telecomunicaciones, especialidad en Sonido e Imagen de la EPS

La red docente de la Comisión de plan de estudios de la titulación de Ingeniería Técnica de Telecomunicación, especialidad en Sonido e Imagen de la EPS ha realizado durante el curso 2007/08 un estudio de los objetivos y competencias del futuro título de grado, así como el análisis y diseño de la posible estructura en bloques y asignaturas obligatorias en la que se podría distribuir dicho título. El estudio toma como base los resultados obtenidos en redes de cursos anteriores (ver memoria de redes 2005/06 y 2006/07), las cuales estaban orientadas al diseño curricular dentro del marco de los créditos ECTS para la convergencia al Espacio Europeo de Educación Superior, y sobre todo, se basa en la experiencia de los propios participantes en trabajos o redes previas. El objetivo principal de este proyecto es el diseño curricular del futuro título de grado en Ingeniería de Telecomunicación en Sonido e Imagen, directamente relacionada con la actual Ingeniería Técnica de Telecomunicación, especialidad en Sonido e Imagen, que se imparte en la Universidad de Alicante. Para ello se han seguido las pautas generales establecidas por el Real Decreto de ordenación de Enseñanzas Universitarias Oficiales (BOE, 30 de octubre de 2007), así como otros documentos elaborados por el Colegio Oficial de Ingenieros Técnicos de Telecomunicación y la Comisión de Universidades de Ingeniería Técnica de Telecomunicación.

Materiales y metodologías docentes en el EEES: informe general de primer curso de la titulación de Telecomunicación

La red docente durante el curso 2006/07 ha realizado un estudio en cuanto a materiales y metodologías docentes en las asignaturas de primer curso de Ingeniería Técnica de Telecomunicación, especialidad en Sonido e Imagen. Esta titulación es impartida en la Escuela Politécnica Superior de la Universidad de Alicante. Dicho estudio está encaminado a suplir las necesidades que marca el nuevo Marco Europeo de Aprendizaje. Se ha definido una ficha de la asignatura (cuyos contenidos y estructura se detallan) que permita al alumnado una visión directa y lo más concisa posible de las actividades que se desarrollarán en cada asignatura a lo largo de su periodo lectivo. El conjunto de estas fichas conformará la denominada Agenda del Estudiante, que fomentará la organización personal de cada alumno. La puesta en común de las experiencias y conocimientos de los diversos miembros de la red debe redundar en una mayor eficacia de la docencia. En este trabajo se incluyen las experiencias de las siete asignaturas implicadas en el proceso.

A new algorithm to accelerate harmonic analysis of time series

The Lomb periodogram has been traditionally a tool that allows us to elucidate if a frequency turns out to be important for explaining the behaviour of a given time series. Many linear and nonlinear reiterative harmonic processes that are used for studying the spectral content of a time series take into account this periodogram in order to avoid including spurious frequencies in their models due to the leakage problem of energy from one frequency to others. However, the estimation of the periodogram requires long computation time that makes the harmonic analysis slower when we deal with certain time series. Here we propose an algorithm that accelerates the extraction of the most remarkable frequencies from the periodogram, avoiding its whole estimation of the harmonic process at each iteration. This algorithm allows the user to perform a specific analysis of a given scalar time series. As a result, we obtain a functional model made of (1) a trend component, (2) a linear combination of Fourier terms, and (3) the so-called mixed secular terms by reducing the computation time of the estimation of the periodogram.

Exact and analytic-numerical solutions of lagging models of heat transfer in a semi-infinite medium

Different non-Fourier models of heat conduction have been considered in recent years, in a growing area of applications, to model microscale and ultrafast, transient, nonequilibrium responses in heat and mass transfer. In this work, using Fourier transforms, we obtain exact solutions for different lagging models of heat conduction in a semi-infinite domain, which allow the construction of analytic-numerical solutions with prescribed accuracy. Examples of numerical computations, comparing the properties of the models considered, are presented.