Die Ergebnisse der Landtagswahl vom 15.10.2017 für die Stadt Göttingen. Dabei können die Ergebnisse für die Stadt Göttingen als Gesamtergebnis sowie für die einzelnen Ortsteile, die Wahlbereiche und Wahlbezirke abgerufen werden. In der Ergebnisdarstellung nach Ortsteilen werden aufgrund der Struktur der Briefwahlbezirke nicht alle Briefwahlergebnisse einberechnet. Einige Briefwahlbezirke in der Stadt Göttingen liegen nur ortsteilübergreifend vor (bspw. EIN Briefwahlbezirk für Elliehausen, Esebeck, Groß Ellershausen, Hetjershausen und Knutbühren). Weiterhin sind einige Briefwahlbezirke von Ortsteilen gleichzeitig auch anderen Bezirken zugeorndet, die nicht zu Ortsteilen gehören. (Bspw. BW-Bezirk 155 Oststadt+Herberhausen). Diese o.g. Ergebnisse werden in den Ergebnissen nach Ortsteilen nicht berücksichtigt. Davon betroffen sind die Ortsteile Elliehausen, Esebeck, Groß Ellershausen, Hetjershausen, Knutbühren, Holtensen, Nikolausberg, Roringen, Herberhausen. In den Ergebnisansichten der Wahlkreise und Wahlbereiche werden die Briefwahlergebnisse natürlich komplett berücksichtigt Die Dateien enthalten folgende Felder: Landtagswahl (17 Göttingen-Stadt) datum : Datum des Wahltermins wahl : Name der Wahl ags : AGS der Behörde gebiet-nr : Nummer des Wahlgebiets gebiet-name : Name des Wahlgebiets max-schnellmeldungen : Anzahl an insgesamt erwarteten Schnellmeldungen im Wahlgebiet anz-schnellmeldungen : Anzahl an bisher eingegangenen Schnellmeldungen im Wahlgebiet A1 : Wahlberechtigte ohne Sperrvermerk 'W' A2 : Wahlberechtigte mit Sperrvermerk 'W' A3 : Wahlberechtigte nicht im Wählerverzeichnis A : Wahlberechtigte insgesamt B : Wähler B1 : Wähler mit Wahlschein C : Ungültige Erststimmen D : Gültige Erststimmen E : Ungültige Zweitstimmen F : Gültige Zweitstimmen D1 : Erststimmen für Partei 1 ... : ... D99 : Erststimmen für Partei 99 F1 : Zweitstimmen für Partei 1 ... : ... F99 : Zweitstimmen für Partei 99 Bei der aktuellen Landtagswahl (17 Göttingen-Stadt) treten folgende Parteien an: D1 / F1 : Christlich Demokratische Union Deutschlands in Niedersachsen D2 / F2 : Sozialdemokratische Partei Deutschlands D3 / F3 : BÜNDNIS 90/DIE GRÜNEN D4 / F4 : Freie Demokratische Partei D5 / F5 : DIE LINKE. Niedersachsen D6 / F6 : Alternative für Deutschland (AfD) Niedersachsen D9 / F9 : Bündnis Grundeinkommen - Die Grundeinkommenspartei D13 / F13 : Deutsche Mitte - Politik geht anders... D16 / F16 : FREIE WÄHLER Niedersachsen D17 / F17 : Liberal-Konservative Reformer Niedersachsen D18 / F18 : Ökologisch-Demokratische Partei, Landesverband Niedersachsen D19 / F19 : Partei für Arbeit, Rechtsstaat, Tierschutz, Elitenförderung und basisdemokratische Initiative D20 / F20 : PARTEI MENSCH UMWELT TIERSCHUTZ Landesverband Niedersachsen D21 / F21 : Piratenpartei Niedersachsen D22 / F22 : V-Partei³ - Partei für Veränderung, Vegetarier und Veganer D23 : Einzelbewerber Yusuf Demirbag

Layer thickness 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/Layer-thickness-of-the-operational-circulation-model-of-BSH-in-the-German-Bight-and-the-western-Baltic-Sea-horizontal-resolution-ca-900-m-2017_FactSheet_HBMnoku_deutsch.pdf https://gdi.bsh.de/en/data/Layer-thickness-of-the-operational-circulation-model-of-BSH-in-the-German-Bight-and-the-western-Baltic-Sea-horizontal-resolution-ca-900-m-2017_FactSheet_HBMnoku_english.pdf

Modelled temperature and salinity 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-temperature-and-salinity-of-the-operational-circulation-model-of-BSH-in-the-German-Bight-and-the-western-Baltic-Sea-horizontal-resolution-ca-900-m-2017_FactSheet_HBMnoku_english.pdf https://gdi.bsh.de/en/data/Modelled-temperature-and-salinity-of-the-operational-circulation-model-of-BSH-in-the-German-Bight-and-the-western-Baltic-Sea-horizontal-resolution-ca-900-m-2017_FactSheet_HBMnoku_deutsch.pdf

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.

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-2017_FactSheet_HBMnoku_english.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-2017_FactSheet_HBMnoku_deutsch.pdf

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.

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.

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-2017_FactSheet_HBMnoku_english.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-2017_FactSheet_HBMnoku_deutsch.pdf

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.

Layer thickness 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/Layer-thickness-of-the-operational-circulation-model-of-BSH-in-the-German-Bight-and-the-western-Baltic-Sea-horizontal-resolution-ca-900-m-2017_FactSheet_HBMnoku_deutsch.pdf https://gdi.bsh.de/en/data/Layer-thickness-of-the-operational-circulation-model-of-BSH-in-the-German-Bight-and-the-western-Baltic-Sea-horizontal-resolution-ca-900-m-2017_FactSheet_HBMnoku_english.pdf