Firsts results on the modelling of the Gran Canaria atmospheric wake

[EN] This poster shows the first attempt to modelize the Gran Canaria Island wake, an obstacle with almost a conical shape (60 km diameter and about 2000 m height). The leeside circulation was modelized for two well-defined street vortex cases during June 2010 and March 2011. Numerical simulations of these events were carried out using the 3.1.1 version of the Weather Research and Forecasting (WRF-ARW) Model. Three different domains with 4.5-km, 1.5-km and 0.5-km horizontal grid spacing and 70 vertical sigma levels were defined. The simulations were performed using two-way interactive nesting between the first and the second and third domains, using different land surface model parameterizations (Thermal diffusion, Noah LSM and RUC) for comparison. Initial conditions were provided by the NCAR Dataset analysis from April 2007. The poster is focused on both episodes using NoahLSM parameterizations.

Os Jesuítas nas Américas: "A República dos Guaranis"

[POR] Para este trabalho, elegemos um estudo sobre uma «experiência jesuíta» junto dos Guaranis, que designamos por «A República dos Guaranis». Trata-se de um processo histórico complexo que teve início no século XVII, sob o impacto da Contra-Reforma, e que terminou em pleno século XVIII, quando o Absolutismo, o Racionalismo e a Lei Natural dominavam a Europa. Este trabalho procura compreender como esta realidade sociocultural se relacionou com uma das regiões do Brasil colonial. [EN] This study analyzes a «Jesuit experience» with the Guarani people, also known as the «Guarani’s Republic». The latter is a complex historical venture which began in the 17th century, in the wake of the Counter-Reformation (1545-1648), and ended in the 18th century when Absolutism, Rationalism, and Natural Law dominated Europe. Our aim is thus that of analyzing how this socio-cultural reality was tied with one region of Colonial Brazil (1500-1822).

Potential vorticity conserving flows and vortex-wave interaction : the role of vertical velocity and isopycnal diffusion on plankton heterogeneity

Programa de doctorado de oceanografía

An observational study of oceanic eddy generation mechanisms by tall deep-water islands (Gran Canaria)

[EN]Oceanic eddy generation by tall deep-water islands is common phenomenon. It is recognized that these eddies may have a significant impact on the marine system and related biogeochemical fluxes. Hence, it is important to establish favourable conditions for their generation. With this objective, we present an observational study on eddy generation mechanisms by tall deep-water islands, using as a case study the island of Gran Canaria. Observations show that the main generation mechanism is topographic forcing, which leads to eddy generation when the incident oceanic flow is sufficiently intense. Wind shear at the island wake may acts only as an additional eddy-generation trigger mechanism when the impinging oceanic flow is not sufficiently intense. For the case of the island of Gran Canaria we have observed a mean of ten generated cyclonic eddies per year. Eddies are more frequently generated in summer coinciding with intense Trade winds and Canary Current.