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Multibeam bathymetry processed data (EM 1002 echosounder entire dataset) of RV MARIA S. MERIAN during cruise MSM62/2

Swath sonar bathymetry data used for that dataset was recorded during RV MARIA S. MERIAN cruise MSM62/2 using Kongsberg EM1002 multibeam echosounder. The cruise took place between 23.03.2017 and 27.03.2017 in the Baltic Sea. The cruise aimed to investigate the impact of the Littorina transgression on the inflow of saline waters into the western Baltic and assessed the potential for future diminution of ventilation in the central and northern deeper basins due to isostatic uplift [CSR]. CI Citation: Paul Wintersteller (seafloor-imaging@marum.de) as responsible party for bathymetry raw data ingest and approval. During the MSM62/2 cruise, the moonpooled KONGSBERG EM1002 multibeam echosounder (MBES) was utilized to perform bathymetric mapping in shallow depths. The echosounder has a curved transducer in which 111 beams are formed for each ping while the seafloor is detected using amplitude and phase information for each beam sounding. For further information on the system, consult https://www.km.kongsberg.com/. Postprocessing and products were conducted by the Seafloor-Imaging & Mapping group of MARUM/FB5, responsible person Paul Wintersteller (seafloor-imaging@marum.de). The open source software MB-System (Caress, D. W., and D. N. Chayes, MB-System: Mapping the Seafloor, https://www.mbari.org/products/research-software/mb-system, 2017) was utilized for this purpose. A sound velocity correction profile was applied to the MSM62/2 data; there were no further corrections for roll, pitch and heave applied during postprocessing. A tide correction was applied, based on the Oregon State University (OSU) tidal prediction software (OTPS) that is retrievable through MB-System. CTD measurements during the cruise were sufficient to represent the changes in the sound velocity throughout the study area. Using Mbeditviz, artefacts were cleaned manually. NetCDF (GMT) grids of the edited data as well as statistics were created with mbgrid. The published bathymetric EM1002 grid of the cruise MSM62/2 has a resolution of 15 m. No total propagated uncertainty (TPU) has been calculated to gather vertical or horizontal accuracy. A higher resolution is, at least partly, achievable. The grid extended with _num represents a raster dataset with the statistical number of beams/depths taken into account to create the depth of the cell. The extended _sd -grid contains the standard deviation for each cell. The DTMs projections are given in Geographic coordinate system Lat/Lon; Geodetic Datum: WGS84.

Kartenlayer Dachflächenphotovoltaikanlagen

Die Karte zeigt die Standorte von DachflächenFotovoltaikanlagen in NRW Im Download wird ebenfalls ein Datensatz für die gesamten Fotovoltaikanlagen (Dach- und Freifläache) angeboten.

Multibeam bathymetry processed data (EM 1002 echosounder entire dataset) of RV MARIA S. MERIAN during cruise MSM52

Swath sonar bathymetry data used for that dataset was recorded during RV MARIA S. MERIAN cruise MSM52 using Kongsberg EM1002 multibeam echosounder. The cruise took place between 01.03.2016 and 28.03.2016 in the Baltic Sea. The cruise aimed gapless imagining of the major pre-alpine tectonic lineaments due to the fact that the Glückstadt Graben and the Avalonia-Baltica suture zone run across the southern Baltic [DOI: 10.2312/cr_msm52]. CI Citation: Paul Wintersteller (seafloor-imaging@marum.de) as responsible party for bathymetry raw data ingest and approval. During the MSM52 cruise, the moonpooled KONGSBERG EM1002 multibeam echosounder (MBES) was utilized to perform bathymetric mapping in shallow depths. It has a curved transducer of which 111 beams are formed for each ping while the seafloor is detected using amplitude and phase information for each beam sounding. For further information on the system, consult https://www.km.kongsberg.com/. Generally, the system was acquiring data throughout the entire cruise. Responsible person during this cruise / PI: Laura Frahm. Postprocessing and products were conducted by the Seafloor-Imaging & Mapping group of MARUM/FB5, responsible person Paul Wintersteller (seafloor-imaging@marum.de). The open source software MB-System (Caress, D. W., and D. N. Chayes, MB-System: Mapping the Seafloor, https://www.mbari.org/products/research-software/mb-system, 2017) was utilized for this purpose. A sound velocity correction profile was applied to the MSM52 data; there were no further corrections for roll, pitch and heave applied during postprocessing. A tide correction was applied, based on the Oregon State University (OSU) tidal prediction software (OTPS) that is retrievable through MB-System. CTD measurements during the cruise were sufficient to represent the changes in the sound velocity throughout the study area. Using Mbeditviz, artefacts were cleaned manually. NetCDF (GMT) grids of the edited data as well as statistics were created with mbgrid. The published bathymetric EM1002 grid of the cruise MSM52 has a resolution of 35 m. No total propagated uncertainty (TPU) has been calculated to gather vertical or horizontal accuracy. A higher resolution is, at least partly, achievable. The grid extended with _num represents a raster dataset with the statistical number of beams/depths taken into account to create the depth of the cell. The extended _sd -grid contains the standard deviation for each cell. The DTMs projections are given in Geographic coordinate system Lat/Lon; Geodetic Datum: WGS84.

GTS Bulletin: ISND40 UMRR - Observational data (Binary coded) - BUFR (details are described in the abstract)

The ISND40 TTAAii Data Designators decode as: T1 (I): Observational data (Binary coded) - BUFR T1T2 (IS): Surface/sea level T1T2A1 (ISN): Synoptic observations from fixed land stations at non-standard time (i.e. 0100, 0200, 0400, 0500, ... UTC) A2 (D): 90°E - 0° northern hemisphere (Remarks from Volume-C: NilReason)

GTS Bulletin: SNAA21 EDZW - Surface data (details are described in the abstract)

The SNAA21 TTAAii Data Designators decode as: T1 (S): Surface data T1T2 (SN): Non-standard synoptic hour A1A2 (AA): Antarctic(The bulletin collects reports from stations: 89011;89047;)

GTS Bulletin: ISID08 EDZW - Observational data (Binary coded) - BUFR (details are described in the abstract)

The ISID08 TTAAii Data Designators decode as: T1 (I): Observational data (Binary coded) - BUFR T1T2 (IS): Surface/sea level T1T2A1 (ISI): Intermediate synoptic observations from fixed land stations A2 (D): 90°E - 0° northern hemisphere(The bulletin collects reports from stations: 10564;Schleiz;10565;Osterfeld;10569;Plauen;10574;Carlsfeld;10577;Chemnitz;10579;Marienberg;10582;Zinnwald-Georgenfeld;10591;Lichtenhain-Mittelndorf;10615;Deuselbach;10628;Geisenheim;10635;Kleiner Feldberg/Taunus;10646;Neuhütten/Spessart;10648;Michelstadt-Vielbrunn;10658;Kissingen, Bad;10671;Lautertal-Oberlauter;10686;Wunsiedel-Schönbrunn;10704;Berus;10706;Tholey;10724;Weinbiet;10733;Waibstadt;10736;Mühlacker;10739;Stuttgart (Schnarrenberg);10747;Kaisersbach-Cronhütte;) (Remarks from Volume-C: SYNOP)

Multibeam bathymetry processed data (EM 1002 echosounder entire dataset) of RV MARIA S. MERIAN during cruise MSM51/1

Swath sonar bathymetry data used for that dataset was recorded during RV MARIA S. MERIAN cruise MSM51/1 using Kongsberg EM1002 multibeam echosounder. The cruise took place between 01.02.2016 and 27.02.2016 in the Baltic Sea. The cruise aimed to perform seismo- and hydroacoustic surveys, sampling of Holocene sediments and to investigate the water column wintertime mixing close to sea-ice limits. These surveys improved the understanding of variations in the ventilation of the deeper Baltic, considering not only external climate forcing but also the effects of postglacial sealevel rise and isostatic uplift [CSR]. CI Citation: Paul Wintersteller (seafloor-imaging@marum.de) as responsible party for bathymetry raw data ingest and approval. During the MSM51-1 cruise, the moonpooled KONGSBERG EM1002 multibeam echosounder (MBES) was utilized to perform bathymetric mapping in shallow depths. 111 beams are formed for each ping while the seafloor is detected using amplitude and phase information for each beam sounding. For further information on the system, consult https://www.km.kongsberg.com/. Postprocessing and products were conducted by the Seafloor-Imaging & Mapping group of MARUM/FB5, responsible person Paul Wintersteller (seafloor-imaging@marum.de). The open source software MB-System (Caress, D. W., and D. N. Chayes, MB-System: Mapping the Seafloor, https://www.mbari.org/products/research-software/mb-system, 2017) was utilized for this purpose. A sound velocity correction profile was applied to the MSM51-1 data; there were no further corrections for roll, pitch and heave applied during postprocessing. A tide correction was applied, based on the Oregon State University (OSU) tidal prediction software (OTPS) that is retrievable through MB-System. CTD measurements during the cruise were sufficient to represent the changes in the sound velocity throughout the study area. Using Mbeditviz, artefacts were cleaned manually. NetCDF (GMT) grids of the edited data as well as statistics were created with mbgrid. The published bathymetric EM1002 grid of the cruise MSM51-1 has a resolution of 15 m. No total propagated uncertainty (TPU) has been calculated to gather vertical or horizontal accuracy. A higher resolution is, at least partly, achievable. The grid extended with _num represents a raster dataset with the statistical number of beams/depths taken into account to create the depth of the cell. The extended _sd -grid contains the standard deviation for each cell. The DTMs projections are given in Geographic coordinate system Lat/Lon; Geodetic Datum: WGS84.

Strom aus Photovoltaik - Installierte Leistung (Plan.-Reg.)

Die Karte zeigt die Summe der installierten elektrischen Leistung der Photovoltaikanlagen für die Planungsregionen (Plan.-Reg.) in Bayern - unterteilt nach Gebäude- und Freiflächenanlagen.

Multibeam bathymetry raw data (Kongsberg EM712 entire dataset) of RV HEINCKE during cruise HE659

Raw multibeam bathymetry data from the Kongsberg EM712 was acquired during the RV Heincke cruise HE659 in the German Bight in April 2025. The data was generally acquired during calm seas in water depths between 20 and 50 m. Primarily three different regions were surveyed (Borkumer Reef Ground, Sylt Outer Reef, and Helgoland). Generally the data is comprehensive and overlapping swaths creating a continuous bathymetry were archived. In some areas the data was acquired complementary to sidescan sonar surveys and individual tracks do not overlap. Data are unprocessed and therefore may contain some incorrect depth measurements (artifacts) without further processing. No tide variations are applied. Sound velocity profiles were acquired regularly. Overall, it appears that the data quality is rather good. The gridded data showed relatively few obstacles.

Biotopkartierung (SH4) Marine Daten

Der vorliegende Geodatensatz umfasst alle bis zum angegebenen Stand kartierten bzw. abgegrenzten FFH-Lebensraumtypen (= LRT) der Meeresgewässer und Gezeitenzonen (1110, 1130. 1140, 1160, 1170) ohne die LRT 1110 und 1170 der Ostsee, für die ein separater Datensatz bereitgestellt wird. Die Abgernzungen in der Nordsee wurden durch die zuständige Nationalparkverwaltung durchgeführt bzw. mit ihr abgestimmt und spiegeln den aktuellen Kenntnisstand wieder. Die Abgrenzungen in der Ostsee wurden in Abstimmung mit der Abteilung Wasserwirtschaft, Dezernat Küstengewässer z. T. anhand von Tiefenlinien und Exposition durchgeführt. Die Abgrenzungen erfolgten i. d. R. nicht durch tatsächliche Kartierung im klassischen Sinne durch Inaugenscheinnahme, sondern durch Detektion (z.B. Sonar) und dient in erster Linie der Abgrenzung LRT zur Erfüllung europarechtlicher Berichtspflichten. Die Anspache der z.T. flächenidentischen gesetzlichen Biotope sowie die Bewertung des Erhaltungsgrades der LRT wird in diesem Datensatz nicht abgebildet. Weitergehende Erläuterung zum Begriff "Wertbiotop": Im Rahmen der BK gehören zu den Wertbiotopen grundsätzlich alle Flächen, die entweder als gesetzlich geschützte Biotope gemäß § 30 BNatSchG i. V. m. § 21 LNatSchG gelten und/oder als Lebensraumtyp (LRT) gemäß Anhang I der FFH-Richtlinie (92/43/EWG, 21.05.1992) anzusprechen sind. Hinsichtlich des gesetzlichen Biotopschutzes ist der Stand nach der Novellierung des Landesnaturschutzgesetzes (LNatSchG) in 2016 (Veröffentlichung in dem GVO Nr. 7 vom 23.06.2016, Seite 162) berücksichtigt und schließt das „arten-und strukturreiche Dauergrünland“ mit ein. Auch die Änderungen aufgrund des § 21 Absatz 7 des Landesnaturschutzgesetzes (LNatSchG), zuletzt geändert durch Verordnung vom 27. März 2019 (GVOBl. Schl.-H. S. 85), sind berücksichtigt sowie - soweit bereits erhoben bzw. in Schleswig-Holstein überhaupt v.h. - auch die seit dem 1. März 2022 gem. § 30 Absatz 1 Nummer 7 BNatSchG neu erfassten gesetzlich geschützten Biotope. Zu den Wertbiotopen gehören im vorliegenden Geodatensatz sämtliche Flächen/ Geometrien, die in den Tabellenspalten „BTSCHUTZ_1“ und/oder „BTSCHUTZ_2“ der Attributtabelle einen Eintrag einer Biotopverordnungsnummer (VO) oder die in den Tabellenspalten „LRT_TYP_1“ und/oder „LRT_TYP_2“ einen Eintrag eines Natura 2000- bzw. EU-LRT-Codes aufweisen. Nachrichtlich weist das LfU darauf hin, dass der Schutz des § 30 BNatSchG i. V. m. § 21 LNatSchG aktiviert wird, wenn und sobald eine Fläche die charakteristischen Merkmale eines gesetzlich geschützten Biotopes erfüllt. Der in § 30 Abs. 7 thematisierten Registrierung, die sich nach Landesrecht richtet und zumeist in Biotopkartierungen, Listen oder Biotopverzeichnissen ihren Niederschlag findet, kommt daher eine lediglich deklaratorische Bedeutung zu. D.h. nicht erst durch die Kartierung bzw. Erfassung und Registrierung werden Flächen zum geschützten Biotop, sondern der Charakter als gesetzlich geschütztes Biotop ergibt sich unmittelbar aus dem Gesetz. Bei Fragen und in Zweifelsfällen ist mit der fachlich zuständigen Person im LfU Rücksprache zu halten. Hinweis: Daten der maritimen LRT 1110 und 1170 in der Ostsee, befinden sich in dem separaten Geodatensatz "Maritim_Daten_Ostsee_LRT_1110_und_1170".

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