Os processos de conversão de energia nos oceanos: uma revisão do diagrama de Lorenz

• Autor(a) principal: Azevedo, José Luiz Lima de
• Data de Publicação: 2008
• Outros Autores: Oliveira, Leopoldo Rota de, Souza, José Francisco Almeida de, Soares, Ivan Dias, Mata, Mauricio Magalhães
• Tipo de documento: Artigo
• Idioma: por
• Título da fonte: Repositório Institucional da FURG (RI FURG)
• Texto Completo: http://repositorio.furg.br/handle/1/1915
• topic: Lorenz diagram; Potential energy; Eddy kinetic energy; Barotropic conversion; Baroclinic conversion and quasi-geostrophy; Diagrama de Lorenz; Energia potencial; Energia cinética; Conversão barotrópica; Conversão baroclínica quase-geostrófia

The energetic analysis is an important diagnostic tool for the identification of dynamic processes associated with events of energy conversion in the ocean. In brief, that analysis shows the energetic interactions which are taking place among the mean and eddy fields of a certain geophysical flow, as well as the transfers involved between the reservoirs of energy in the oceans. Those processes are detailed in the Lorenz Diagram which links, through four boxes, the reservoirs of the mean kinetic energy, eddy kinetic energy, mean potential energy and eddy potential energy of the flow. Moreover, the Diagram identifies the interactions that occur between those four energy forms, as well as the exchanges through the boundaries (sources and sinks). After an extensive review, we have identified that the specialized literature lacks in texts which detail the several mechanisms of energetic conversion among the main forms of energy in the oceans, with most publications detailing only part of those components. This article presents a detailed review on this subject, gathering information of several sources and having as main objective the step by step construction of the Lorenz Diagram, with their respective formulations. The discussion of each term of the Diagram is presented objectively thus enabling a better understanding of this tool, which is instrumental in summarizing the energy processes at a given area of the ocean.