Application of Entropy and Fractal Dimension Analyses to the Pattern Recognition of Contaminated Fish Responses in Aquaculture

The objective of the work was to develop a non-invasive methodology for image acquisition, processing and nonlinear trajectory analysis of the collective fish response to a stochastic event. Object detection and motion estimation were performed by an optical flow algorithm in order to detect moving fish and simultaneously eliminate background, noise and artifacts. The Entropy and the Fractal Dimension (FD) of the trajectory followed by the centroids of the groups of fish were calculated using Shannon and permutation Entropy and the Katz, Higuchi and Katz-Castiglioni's FD algorithms respectively. The methodology was tested on three case groups of European sea bass (Dicentrarchus labrax), two of which were similar (C1 control and C2 tagged fish) and very different from the third (C3, tagged fish submerged in methylmercury contaminated water). The results indicate that Shannon entropy and Katz-Castiglioni were the most sensitive algorithms and proved to be promising tools for the non-invasive identification and quantification of differences in fish responses. In conclusion, we believe that this methodology has the potential to be embedded in online/real time architecture for contaminant monitoring programs in the aquaculture industry.

¿Cómo podemos hacer que Michelin sea green?

Duración (en horas): Más de 50 horas. Destinatario: Estudiante y Docente

Daily scale wintertime sea surface temperature and IPC-Navidad variability in the southern Bay of Biscay from 1981 to 2010

The combination of remotely sensed gappy Sea surface temperature (SST) images with the missing data filling DINEOF (data interpolating empirical orthogonal functions) technique, followed by a principal component analysis of the reconstructed data, has been used to identify the time evolution and the daily scale variability of the wintertime surface signal of the Iberian Poleward Current (IPC), or Navidad, during the 1981-2010 period. An exhaustive comparison with the existing bibliography, and the vertical temperature and salinity profiles related to its extremes over the Bay of Biscay area, show that the obtained time series accurately reflect the IPC-Navidad variability. Once a time series for the evolution of the SST signal of the current over the last decades is well established, this time series is used to propose a physical mechanism in relation to the variability of the IPC-Navidad, involving both atmospheric and oceanic variables. According to the proposed mechanism, an atmospheric circulation anomaly observed in both the 500 hPa and the surface levels generates atmospheric surface level pressure, wind-stress and heat-flux anomalies. In turn, those surface level atmospheric anomalies induce mutually coherent SST and sea level anomalies over the North Atlantic area, and locally, in the Bay of Biscay area. These anomalies, both locally over the Bay of Biscay area and over the North Atlantic, are in agreement with several mechanisms that have separately been related to the variability of the IPC-Navidad, i.e. the south-westerly winds, the joint effect of baroclinicity and relief (JEBAR) effect, the topographic beta effect and a weakened North Atlantic gyre.

Variability in the air-sea interaction patterns and timescales within the south-eastern Bay of Biscay, as observed by HF radar data

Two high-frequency (HF) radar stations were installed on the coast of the south-eastern Bay of Biscay in 2009, providing high spatial and temporal resolution and large spatial coverage of currents in the area for the first time. This has made it possible to quantitatively assess the air-sea interaction patterns and timescales for the period 2009-2010. The analysis was conducted using the Barnett-Preisendorfer approach to canonical correlation analysis (CCA) of reanalysis surface winds and HF radar-derived surface currents. The CCA yields two canonical patterns: the first wind-current interaction pattern corresponds to the classical Ekman drift at the sea surface, whilst the second describes an anticyclonic/cyclonic surface circulation. The results obtained demonstrate that local winds play an important role in driving the upper water circulation. The wind-current interaction timescales are mainly related to diurnal breezes and synoptic variability. In particular, the breezes force diurnal currents in waters of the continental shelf and slope of the south-eastern Bay. It is concluded that the breezes may force diurnal currents over considerably wider areas than that covered by the HF radar, considering that the northern and southern continental shelves of the Bay exhibit stronger diurnal than annual wind amplitudes.

La marca personal como seña de identidad del directivo: competencias distintivas

La gestión empresarial -economía, finanzas, recursos humanos, marketing, etc.- debe caracterizarse por la eficacia y por la eficiencia; sin embargo, en la mayoría de las ocasiones, ambos rasgos no están presentes en las organizaciones por el perfil mediocre de los directivos, que no solo es responsabilidad de los propios interesados, sino también de las personas que los han puesto en ese cargo. Esta situación perjudica a la rentabilidad de las organizaciones, por lo que es fundamental solventar este problema con directivos que se distingan por una excelencia, la cual solo se conseguirá con una marca personal basada en unas competencias técnicas, una formación humanística, unas habilidades directivas y unos valores humanos sólidos.

La gestión de la materia prima ósea en la fabricación de objetos durante la Prehistoria

Homenaje a Ignacio Barandiarán Maestu / coord. por Javier Fernández Eraso, Juan Santos Yanguas

La industria ósea del Paleolítico superior de la cueva de Gatzarria (Zuberoa, País Vasco)

[ES] La cueva de Gatzarria ofrece un rico e interesante relleno del Paleolítico medio y superior. La industria ósea «elaborada» (puntas,puntas en extremo, alisadores y varillas) se halla documentada en los niveles Protoauriñacienses (cjn2 y cjnl), en el Auriñaciense antiguo de cbci-cbf y en el Autiñaciense evolucionado de cb. De todas las categorías atestiguadas que aquí tratamos, el grupo más numeroso e interesante es el de las puntas: junto a una serie de ejemplares sin denominación específica que se repiten en los mencionados niveles, existen algunos tipos ligados específicamente a algunos de ellos; es el caso de las puntas fusiformes en cjn2, de las puntas sublosángicas en cjnl y de las puntas de base hendida en cbci-cbf.