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Raumordnung der Küstenländer in Meeres- und Küstenzone (WFS)

Die deutschen Anteile an Nord- und Ostsee sind in die Territorial- und Küstengewässer der Küstenbundesländer sowie die Ausschließliche Wirtschaftszone unterteilt. Jedes Küstenbundesland und der Bund für die AWZ sind für die Aufstellung von Raumordnungsplänen (-programmen, -konzepten) zuständig. Da allerdings die Nutzung des Meeres grenzüberschreitend erfolgt, besteht der Bedarf für ein harmonisiertes Produkt das das gesamte deutsche Meeresgebiet abdeckt. Dieser Download-Dienst (WFS) der Marinen Dateninfrastruktur Deutschland (MDI-DE) stellt unterschiedliche Nutzungen aus den Raumordnungsplänen der Küstenländer harmonisiert zur Verfügung. Die Daten schließen nahtlos and den Raumordnungsplan AWZ des BSH an und enthalten die Nutzungen Schifffahrt, Windenergie, Leitungen, Natur und Landschaft, Fischerei, Tourismus sowie Rohstoffe und Küstenschutz. Datenquellen: Landesraumordnungsprogramme und -entwicklungspläne sowie Flächennutzungspläne der Küstenländer. Harmonisierte Attribute: Nutzung, Vorrang- / Vorbehaltsgebiet, Gültigkeit, Lizenz, Planungsdokument sowie an die EU Raumordnung angeglichene fachliche Typisierung.

Umweltgerechtigkeit 2023/2024 (Umweltatlas)

Darstellung der Umweltgerechtigkeit in Berlin 2023/24 durch die Bewertung der Kernindikatoren Lärmbelastung, Luftbelastung, Grünversorgung, Thermische Belastung, Soziale Benachteiligung sowie der Darstellung der Integrierten Mehrfachbelastung, Integrierten Mehrfachbelastung einschließlich des Kernindikators Soziale Benachteiligung sowie der Integrierten Mehrfachbelastung einschließlich des Kernindikators Soziale Benachteiligung und weiterer Ergänzungsindikatoren als "Berliner Umweltgerechtigkeitskarte".

Processed seismic data of Cruise BGR 1977

A geophysical reconnaissance survey was carried out in the Labrador Sea and Davis Strait between July and September 1977 by BGR. The data format is Society of Exploration Geophysicists SEG Y. The survey was executed on the research vessel MS Explora. The seismic, magnetic and gravity data from 5931 line-kilometers on 21 lines were recorded on magnetic tape. A 24-fold coverage technique was used with 48 seismic channels (traces), with a 2400m streamer cable, and 23.45 l airgun array. A full integrated computerized satellite navigation system (INDAS III) served as positioning system. Based on a preliminary interpretation of the seismograms, the Labrador Sea was devided into an eastern (Greenland) and western (Canadian) area, seperated by the Mid Labrador Ridge. Within the eastern part of the Labrador Sea the Pre-Cenozoic sediments show three distinct layers, traceable over the entire Greenland area of the sea. In the Cenozoic layer olisthostromes occur. The highest apparent velocity determined from sonobuoy data was 9.26 km/sec. The calculated refractor lies at a depth of approximately 13 km. The seismic section from the sediments on the Canadian side of the Labrador Sea show a uniform series of thick sediments below the Cenozoic cover. The highly disturbed basement is often masked by the multiple reflections from the seafloor. Statements about the nature and structure of the basement can only be made after processing data.

Processed seismic data of Cruise HE242

The previous BGR-cruises with RV AURELIA in 2003 and 2004 were designed to collect a grid of seismic MCS-data which should enable us to get a high-resolution overview over the upper 1 s TWT of the sediments of the German North Sea sector. The data format is Society of Exploration Geophysicists SEG Y. Together with the previously acquired data these new data should help to extend our knowledge of the Late Tertiary and Quaternary evolution of the German North Sea Sector. For the current measurements under the scope of the DFG-funded project RE2424/1-1 ‚Nordsee’ the research vessel RV HEINCKE was made available by the ‘Senatskommission für Ozeanographie’ of the DFG. During the cruise a total ca. 1400 km of high quality MCS lines were surveyed and simultaneously measured by a sediment echosounder system that enabled additional profiles during transits with speeds > 5 kn. The BGR high-resolution multichannel seismic reflection system consisting of a GI-Gun (0.8 l) and a 300 m streamer with 24 channels and a sediment echosounder type SES 2000 standard by Innomar, Rostock. While the BGR-seismic system was used to observe the shallow subsurface down to 2 s TWT penetration depth, the sediment echosounder with a penetration depth of several meters was primarily intended to identify sampling positions for the deployment of the BGR vibration corer during the succeeding Leg 2. Additionally, the echosounder system enables the relationship to the highest-resolution multichannel seismic measurements of the group of the University of Bremen on FK SENCKENBERG. All seismic records were processed onboard for the quality control and for a first interpretation.

Raumordnung der Küstenländer in Meeres- und Küstenzone (WMS)

Die deutschen Anteile an Nord- und Ostsee sind in die Territorial- und Küstengewässer der Küstenbundesländer sowie die Ausschließliche Wirtschaftszone unterteilt. Jedes Küstenbundesland und der Bund für die AWZ sind für die Aufstellung von Raumordnungsplänen (-programmen, -konzepten) zuständig. Da allerdings die Nutzung des Meeres grenzüberschreitend erfolgt, besteht der Bedarf für ein harmonisiertes Produkt das das gesamte deutsche Meeresgebiet abdeckt. Dieser Darstellungs-Dienst (WMS) der Marinen Dateninfrastruktur Deutschland (MDI-DE) stellt unterschiedliche Nutzungen aus den Raumordnungsplänen der Küstenländer harmonisiert zur Verfügung. Die Daten schließen nahtlos and den Raumordnungsplan AWZ des BSH an und enthalten die Nutzungen Schifffahrt, Windenergie, Leitungen, Natur und Landschaft, Fischerei, Tourismus sowie Rohstoffe und Küstenschutz. Datenquellen: Landesraumordnungsprogramme und -entwicklungspläne sowie Flächennutzungspläne der Küstenländer. Harmonisierte Attribute: Nutzung, Vorrang- / Vorbehaltsgebiet, Gültigkeit, Lizenz, Planungsdokument sowie an die EU Raumordnung angeglichene fachliche Typisierung.

Processed seismic data of Cruise Nares 2001

The Scientific staff and crew onboard CCGS Louis S. St. Laurent (LSL) returned September the 10th, 2001 from a scientific expedition to the Nares Strait, the northernmost waterway connecting the Arctic and Atlantic oceans. The data format is Society of Exploration Geophysicists SEG Y. The ice conditions in the strait required the support of Canada's largest ice breaker. The ship was a versatile platform for 34 scientists to accomplish their marine investigation. The LSL has a history of supporting international scientific expeditions including an oceanographic transect of the Arctic Ocean in 1994 and a biological study of the Canadian Arctic Islands in 1999. Germany (Bundesanstalt für Geowissenschaften und Rohstoffe, BGR) and Canada (Geological Survey of Canada) undertook a 5-week scientific cruise to study and explore the geological structure and evolution of the Nares Strait. The primary objective was the study of structural features relating to the formation of the Arctic Ocean and, in particular, the study of the Wegener Fault. This fault is a linear boundary between Greenland and Ellesmere Island which was noted by the German scientist Alfred Wegener in 1915 and later became the subject of a major scientific controversy. The co-operative cruise, which was planned over a period of 2 years, provided the basis for a wide range of scientific investigations, from marine seismic work and climate change studies through airborne magnetic investigations to geodetic survey measurements and geological sampling onshore. Systematic geophysical offshore studies in this key area had not been undertaken before. Where towing of seismic equipment was not possible because of ice coverage, magnetic maps were made using a helicopter-borne magnetic sensor system. Sediment and water samples taken during the cruise provide information on changes in climate and sea ice cover from the last ice-age to the present. An 11 m-long sediment core from outer Jones Sound is the longest core ever taken in the Canadian Arctic channels and holds clues to the detailed climate history of northern Baffin Bay.

ICON-EPS GRIB data

ICON-EPS 0.5º x 0.5º regular lat/lon grid, up to +180h every 6h, runs 00/12 UTC varios parameter, varios level, varios threshold

Processed seismic data of Cruise PQ2

Processed seismic data from Baltic Sea with research ship M/V Polar Queen.The data format is Society of Exploration Geophysicists SEG Y. During the period from 14th to 28th of April 1996 BGR and GFZ chartered the Norwegian vessel M/V POLAR QUEEN for testing the new and updated marine seismic equipment of the BGR and for acquiring seismic lines. The operating area was the North Sea and Baltic Sea. The geophysical lines in the Baltic Sea were chosen as extended onshore DEKORP lines to evaluate the deep structure of the south western part of the Baltic Sea. For the seismic profiles a tuned source array consisting of 20 air guns in two linear strings with a total volume of 52 l was used. The recording length was 26 s, the sample rate 4 ms and the shot interval 30 s. This time triggering for the shot release was chosen, because all shots were also recorded onshore by seismic stations for wide angle/refraction acquisition (GFZ). During this leg 810 km reflection lines and additional 230 km pure shooting could be surveyed. The preliminary interpretation of the seismic single traces was restricted on the ship to the upper time range. The main structures in the southern Baltic Sea could be evaluated. A full interpretation especially of the deeper part is only possible after a processing due to the nature of the single traces and the S/N ratio.

Processed seismic data of Cruise AUR 2003

The late Tertiary and Quaternary development of the German EEZ was systematically inverstigated by seismic profiling. The data format is Society of Exploration Geophysicists SEG Y. For that survey the privately owned motor vessel AURELIA was chartered for a period of 24 days from the 16th of September to 10th of October 2003. A more or less equidistant E-W and N-S grid of profiles with a length of 2500 km was surveyed by high-resolution multichannel seismic system. A 0.82 litre GI-Gun was employed every 12.5 m and the reflected signals were recorded by a 300 m long streamer. Simultaneously a deep-towed HUNTEC-Boomer or a GEO-Sparker was run (150km/620km). All seismic records were processed onboard for the quality control and for a first interpretation.

Marine Seismic Survey Profiles (MSSP) (WMS)

During the period from 1974 to 2018 various cruises from BGR acquired seismic lines worldwide. The aim of these marine expeditions was a detailed survey of the geological structure.

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