cartografia
cartografia_undefined
1708 record(s)
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cartografia
geographicCoverage
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hvd
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Two beach profiles (P2 and P3) were collected at S. Pedro do Estoril, Cascais (Portugal) as part of shoreline monitoring exercises. Survey was conducted in a situation of low tide and these beach profiles run perpendicular to the shoreline. Profile location and a description of points used are available in profile data (.xls).
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Estabelecimentos abrangidos (DL 150/2015): Localização pontual; Estabelecimento; Nível de Perigosidade (Superior/Inferior)
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Estabelecimentos abrangidos (DL 150/2015): Localização pontual; Estabelecimento; Nível de Perigosidade (Superior/Inferior)
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O PPSAH tem a natureza de regulamento administrativo e as suas disposições vinculam as entidades públicas e os particulares. Esta planta corresponde à planta de património sendo um elemento de acompanhamento do PPSAH. (Regulamento: http://geoangra.cmah.pt/ppsah/Regulamento_PPSAH.pdf)
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Web Map Visualization, INSPIRE (ISO19128-WMS 1.3.0) compliance, of the monthly minimum air temperature, mean values of the period 1971-2000, obtained by multivariate regression with altitude and distance to the coast, explanatory variables, and ordinary kriging of residues.
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Serviço de Visualização (WMS) do Programa Regional de Alterações Climáticas (PRAC).
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Serviço de Visualização (WMS) de Cartografia Vectorial à escala 1:5000 do Município de Nordeste, cedida pela Associação de Municípios da Região Autónoma dos Açores ao Município de Nordeste.
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Web Map Visualization, INSPIRE (ISO19128-WMS 1.3.0) compliance, of the Annual Map of the number of days with minimum air temperature ≥20ºC (Number of tropical nights) in the period 1971-2000, obtained by ordinary kriging from the surface observations network of climatological stations of the Institute of Meteorology and the pluviometric stations from INAG.
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Web Map Visualization, INSPIRE (ISO19128-WMS 1.3.0) compliance, of the Annual Map of the number of days with minimum air temperature ≤0ºC (Number of days of frost) in the period 1971-2000, obtained by ordinary kriging from the surface observations network of climatological stations of the Institute of Meteorology and the pluviometric stations from INAG.