Plataforma Off-shore com Turbina Eólica Simulação e Controlo

O objetivo deste trabalho é o de simular e controlar a plataforma de um aerogerador flutuante. Este aerogerador flutuante consiste numa plataforma do tipo semi-submersível, nomeadamente o DeepCwind acoplado a um aerogerador de 5 MW, mais especificamente o NREL offshore 5-MW baseline wind turbine. Descreve-se o modelo físico do aerogerador flutuante, a formulação teórica a ele subjacente, bem como a caraterização dos diferentes estados do vento e do mar utilizados para simulação. O modelo não linear do aerogerador flutuante foi simulado, utilizando o FAST como emulador do aerogerador flutuante, para condições ambientais determinísticas, por forma a compreender a dinâmica associada à plataforma. Modelos lineares foram obtidos, por linearização do modelo não linear, aplicando técnicas de identificação de sistemas e utilizando o módulo de linearização do simulador FAST. Estes modelos foram posteriormente comparados, utilizando um único modelo para síntese de controladores. Controladores esses, desenvolvidos com base num modelo linear simplificado que consiste no pitch da plataforma, transformando o problema global da plataforma num problema bidimensional. Projetou-se um controlador proporcional-integral-derivativo (PID) e um controlador em espaço de estados por colocação de pólos. A simulação do modelo não linear, com o controlo do pitch da plataforma, para diferentes condições ambientais, demonstrou o bom desempenho dos controladores. Foi possível com ambos os controladores garantir os requisitos do sistema controlado, em que se exigia que se evitasse ressonâncias e em que o pitch da plataforma fosse nulo, por forma a garantir a perpendicularidade do plano das pás (plano do rotor) do aerogerador em relação à direção do vento.

Variation of the Chlorophyll a Related to Sea Surface Temperature, Wind and Geostrophic Currents in the Cape Verde Region Using Satellite Data

We present a comparative analysis of satellite derived climatologies in the Cape Verde region (CV). In order to establish chlorophyll a variability, in relation to other oceanographic phenomena, a set of, relatively long (from five to eight years), time series of chlorophyll a, sea surface temperature, wind and geostrophic currents, were ensembled for the Eastern Central Atlantic (ECA). We studied seasonal and inter-annual variability of phytoplankton concentration, in relation to the rest of the variables, with a special focus in CV. We compared the situation within the archipelago with those of the surrounding marine environments, such as the North West African Upwelling (NWAU), North Atlantic Subtropical Gyre (NASTG), North Equatorial Counter Current (NECC) and Guinea Dome (GD). At the seasonal scale, CV region behaves partly as the surrounding areas, nevertheless, some autochthonous features were also found. The maximum peak of the pigment having a positive correlation with temperature is found at the end of the year for all the points in the archipelago; a less remarkable rise with negative correlation is also detected in February for points CV2 and CV4. This is behavior that none of the surrounding environments have shown. This enrichment was found to be preceded by a drastic drop in wind intensity (SW Monsoon) during summer months. The inter-annual analysis shows a tendency for decreasing of the chlorophyll a concentration.

Variation of the Chlorophyll a Related to Sea Surface Temperature, Wind and Geostrophic Currents in the Cape Verde Region Using Satellite Data

We present a comparative analysis of satellite derived climatologies in the Cape Verde region (CV). In order to establish chlorophyll a variability, in relation to other oceanographic phenomena, a set of, relatively long (from five to eight years), time series of chlorophyll a, sea surface temperature, wind and geostrophic currents, were ensembled for the Eastern Central Atlantic (ECA). We studied seasonal and inter-annual variability of phytoplankton concentration, in relation to the rest of the variables, with a special focus in CV. We compared the situation within the archipelago with those of the surrounding marine environments, such as the North West African Upwelling (NWAU), North Atlantic Subtropical Gyre (NASTG), North Equatorial Counter Current (NECC) and Guinea Dome (GD). At the seasonal scale, CV region behaves partly as the surrounding areas, nevertheless, some autochthonous features were also found. The maximum peak of the pigment having a positive correlation with temperature is found at the end of the year for all the points in the archipelago; a less remarkable rise with negative correlation is also detected in February for points CV2 and CV4. This is behavior that none of the surrounding environments have shown. This enrichment was found to be preceded by a drastic drop in wind intensity (SW Monsoon) during summer months. The inter-annual analysis shows a tendency for decreasing of the chlorophyll a concentration.