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1. Representação de Prof. Aldo von Wangenheim |
Apresentações
Abaixo você vai conhecer algumas técnicas e alguns exemplos muito interessantes. Veja aqui como são tomadas imagens de radar estereoscópicas e como se realiza a análise destas imagens para a geração de mapas topográficos e a descoberta de plantações, desertos, etc. A área da análise
de imagens do alto inclui não somente imagens de satélites,
mas também imagens tomadas a partir de aviões, técnica
denominada aerolevantamento.
Interferometria por Radar It is not possible to measure the three-dimensional position of a point on the ground using only one radar image. Therefore, in analogy to optical stereoscopy, two images taken from different positions are combined. Isto pode ser realizado através da intefrometria, que pode ser de passada única ou de dupla passada. The Shuttle Radar Topography Mission of DLR allows to record both images simultaneously using two antennas. The second antenna is placed at the tip of a 60 metres long mast. The inherent similarity of the two images, the coherence, is measured and serves as indicator of the expected quality of the derived digital elevation model. The similarity between the two radar images is determined using the so called coherence. The choherence values can also be used to indicate the expected quality of the Digital Elevation Model. In the coherence map for every pixel the similarity of the
two images is shown as a grey scale value. Coherent areas are shown bright, areas with a low coherence like open water are represented in dark colours. It is not possible to determine altitude values of in-coherent areas. Coherence maps are beeing sucessfuly used for vegetation- classification. In order to get an interferogram both images have to be fitted exactly to each other and filtered to enhance the image quality. Every colour value represents a phase value between 0 and 2pi, where the colours repeat to form so-called fringes (stripes). As can be seen in the image below, the topography of the area is already visible in the interferogram. To emphasis this, the image the Digital Elevation Model was overlain on the interferogram. An shaded relief model, coloured according to the height values was used. The phase differences together with orbit information of the two antennas are used to calculate height values. In a last step those values are transformed to a map projection (UTM) or geographic coordinates.
Mineração de Dados: A Interpretação de Imagens de Satélites "Looking for a needle in a bundle of hay!"
Imagem 1: Mapa de elevação digital da região de White Sands, EUA, artificialmente colorido de acordo com o tipo de estrutura gerado a partir da análise de imagens por radar do espaço. Mostra a localização dos exemplos abaixo The Digital Elevation Model
- DEM is complemented by information characterizing the shape and
the physical properties of the imaged objects and land cover structures,
making an evaluation and characterization of inhabited settlements possible,
providing information for agriculture and micro farming, mapping the humidity
and roughness of soil. The following examples illustrate results of advanced
methods for image information retrieval which can help users to find relevant
information in large sets of DEM and image data, to fuse the information
and to understand the scenes.
Como
se constrói um Mapa de Elevação Interpretado ?
Mapas de Altitude Baseados em Interferometria de Paranaguá, PR, Brasil
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