www.geodatenkatalog.de (S3F)
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opendata
163624 record(s)
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Die Stadtgrenze entspricht dem Verwaltungsgebiet der Stadt Göttingen. Das Gebiet wird mittels eines Polygons dargestellt.
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Two strong eruptions of Stromboli Volcano (38.789°N 15.213°E, 920 m) occurred on July 3rd and August 28th 2019. This data set provides the infrasound records in terms of raw pressure data in Pascal of both eruptions available at BGR’s infrasound array I26DE in Germany as well as infrasound arrays OHP and CEA in France. The publication “Using dense seismo-acoustic network to provide timely warning of the 2019 paroxysmal Stromboli eruptions” (Le Pichon et al., 2021, Scientific Reports) provides further details on this data set and its scientific application. Data format: The data are provided as ASCII files (separate file for each infrasound sensor and hour of measurement, plus a README file).
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Friedhöfe im Stadtgebiet der Stadt Göttingen.
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Das Thema stellt die Standorte der Bibliotheken im Landkreis Mecklenburgische Seenplatte dar. Dazu werden Adressdaten und Informationen über die Bibliothek ausgegeben.
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Busliniennetz der Göttinger Verkehrsbetriebe. Dies beinhaltet das Liniennetz im Stadtgebiet der Stadt Göttingen sowie Bovenden und Rosdorf. Das Liniennetz der Überlandbusse sind nicht enthalten.
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Dieser Dienst liefert die Blattschnitteinteilung des (historischen) Topographischen Atlas 1:50000 für das Großherzogtum Baden und das Königreich Württemberg mit den Attributen Blattnummer, Blattnamen sowie Ausgabejahr.
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Modelled temperature and salinity of the operational circulation model of the Federal Maritime and Hydrographic Agency of Germany (BSH), in the North and Baltic Sea (horizontal resolution ca. 5 km). The model (HBM, HIROMB-BOOS-Model) is run four times each day in a configuration with a fine grid in the German Bight and western Baltic Sea (900 m resolution, separate dataset) and a coarser grid which covers the North and Baltic Sea (5 km resolution, this dataset). The model is forced by the weather forecast of the German Weather Service (DWD). More detailed information about the model configuration can be found in Brüning et al. (2021); https://doi.org/10.23784/HN118-01.
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Modelled currents of the operational circulation model of the Federal Maritime and Hydrographic Agency of Germany (BSH), in the German Bight and the western Baltic Sea (horizontal resolution ca. 900 m). The model (HBM, HIROMB-BOOS-Model) is run four times each day in a configuration with a fine grid in the German Bight and western Baltic Sea (900 m resolution, this dataset) and a coarser grid which covers the North and Baltic Sea (5 km resolution, separate dataset). The model is forced by the weather forecast of the German Weather Service (DWD). More detailed information about the model configuration can be found in Brüning et al. (2021); https://doi.org/10.23784/HN118-01. For more information, please visit: https://gdi.bsh.de/en/data/Modelled-currents-of-the-operational-circulation-model-of-BSH-in-the-German-Bight-and-the-western-Baltic-Sea-horizontal-resolution-ca-900-m-2019_FactSheet_HBMnoku_deutsch.pdf https://gdi.bsh.de/en/data/Modelled-currents-of-the-operational-circulation-model-of-BSH-in-the-German-Bight-and-the-western-Baltic-Sea-horizontal-resolution-ca-900-m-2019_FactSheet_HBMnoku_english.pdf
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Layer thickness of the operational circulation model of the Federal Maritime and Hydrographic Agency of Germany (BSH), in the North and Baltic Sea (horizontal resolution ca. 5 km). The model (HBM, HIROMB-BOOS-Model) is run four times each day in a configuration with a fine grid in the German Bight and western Baltic Sea (900 m resolution, separate dataset) and a coarser grid which covers the North and Baltic Sea (5 km resolution, this dataset). The model is forced by the weather forecast of the German Weather Service (DWD). More detailed information about the model configuration can be found in Brüning et al. (2021); https://doi.org/10.23784/HN118-01.
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Modelled sea surface height above mean sea level of the operational circulation model of the Federal Maritime and Hydrographic Agency of Germany (BSH), in the North and Baltic Sea (horizontal resolution ca. 5 km). The model (HBM, HIROMB-BOOS-Model) is run four times each day in a configuration with a fine grid in the German Bight and western Baltic Sea (900 m resolution, separate dataset) and a coarser grid which covers the North and Baltic Sea (5 km resolution, this dataset). The model is forced by the weather forecast of the German Weather Service (DWD). More detailed information about the model configuration can be found in Brüning et al. (2021); https://doi.org/10.23784/HN118-01.