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Chlorophyll a, extracellular polymeric substance concentration and 16S rRNA gene copy numbers in saltmarsh sediments in response to a storm surge

Samples were taken to study the effect of storm surges on ecosystem functioning of salt marsh microbial communities. Sediment samples were collected from experimental salt marsh islands located in the back-barrier tidal flats of Spiekeroog Island, German North Sea (53°45′N, 7°43′E). The islands consist of three elevation zones (0.7 m, 1.0 m, and 1.3 m above mean sea level), corresponding to pioneer zone, lower salt marsh, and upper salt marsh. Six islands were sampled (three initially bare; three transplanted with lower salt marsh sediment and vegetation). Sampling was conducted in September 2022 (pre-disturbance), March 2023 (post-winter storm surges), and August 2023 (recovery phase). Surface sediments (upper 2 cm) were collected using syringe cores. Pooled samples were analyzed for chlorophyll a as a proxy for microphytobenthos biomass using ethanol extraction and spectrophotometric pigment analysis. Extracellular polymeric substances (EPS) were quantified using EDTA extraction followed by phenol–sulfuric acid carbohydrate analysis. DNA was extracted from sediment subsamples using a Qiagen PowerSoil kit. Prokaryotic abundance was estimated by quantitative PCR targeting the 16S rRNA gene (primers 519F/907R), using an Escherichia coli 16S rRNA gene standard curve. The dataset includes chlorophyll a concentrations (µg g⁻¹ dry sediment), EPS carbohydrate concentrations, and prokaryotic 16S rRNA gene copy numbers for all sampling times, elevations, and treatments.

Multibeam bathymetry processed data (Atlas Hydrosweep DS 2 echo sounder entire dataset) of RV POLARSTERN during cruise ANT-XXIII/8 (PS69), Southern Ocean

Multibeam data were collected during RV Polarstern cruise ANT-XXIII/8 (2006-11-23 to 2007-01-30). Multibeam sonar system was Atlas Hydrographic Hydrosweep DS 2 multibeam echo sounder. Data are processed with Caris HIPS, including sound velocity correction with SV data from CTDs and World Ocean Atlas 18 (https://www.ncei.noaa.gov/archive/accession/NCEI-WOA18), tidal correction with TPXO9_atlas_v5 (https://www.tpxo.net), and manual cleaning. The soundings are combined in daily files, the format is XYZ ASCII (<Lon> <Lat> <Depth in meters, positive up, relative to mean sea level>). Additional grids have been computed with depth dependent cell size to visualize the data. These grids are not meant for scientific analysis or navigation, but for overview purposes only.

Multibeam bathymetry processed data (Atlas Hydrosweep DS 3 echo sounder entire dataset) of RV POLARSTERN during cruise PS116, Atlantic Ocean

Multibeam data were collected during RV Polarstern cruise PS116 (2018-11-11 to 2018-12-11). Multibeam sonar system was Atlas Hydrographic Hydrosweep DS 3 multibeam echo sounder. Data are processed with Caris HIPS, including sound velocity correction with SV data from SVPs, UCTDs and World Ocean Atlas 13 (https://doi.org/10.7289/v5f769gt), tidal correction with TPXO9_atlas_v5 (https://www.tpxo.net), and manual cleaning. The soundings are combined in daily files, the format is XYZ ASCII (<Lon> <Lat> <Depth in meters, positive up, relative to mean sea level>). Additional blockmedian grids have been computed with depth dependent cell size to visualize the data. These grids are not meant for scientific analysis or navigation, but for overview purposes only.

Multibeam bathymetry processed data (Atlas Hydrosweep DS 2 echo sounder entire dataset) of RV POLARSTERN during cruise ANT-XVIII/1 (PS58), Atlantic Ocean

Multibeam data were collected during RV Polarstern cruise ANT-XVIII/1 (2000-09-29 to 2000-10-23). Multibeam sonar system was Atlas Hydrographic Hydrosweep DS 2 multibeam echo sounder. Data are processed with Caris HIPS, including sound velocity correction by cross fan calibration, tidal correction with TPXO9_atlas_v5 (https://www.tpxo.net), and manual cleaning. The soundings are combined in daily files, the format is XYZ ASCII (<Lon> <Lat> <Depth in meters, positive up, relative to mean sea level>). Additional grids have been computed with depth dependent cell size to visualize the data. These grids are not meant for scientific analysis or navigation, but for overview purposes only.

Multibeam bathymetry processed data (Atlas Hydrosweep DS 3 echo sounder entire dataset) of RV POLARSTERN during cruise PS98, Atlantic Ocean

Multibeam data were collected during RV Polarstern cruise PS98 (2016-04-10 to 2016-05-11). Multibeam sonar system was Atlas Hydrographic Hydrosweep DS 3 multibeam echo sounder. Data are processed with Caris HIPS, including sound velocity correction with SV data from World Ocean Atlas 13 (https://doi.org/10.7289/v5f769gt), tidal correction with TPXO9_atlas_v5 (https://www.tpxo.net), and manual cleaning. The soundings are combined in daily files, the format is XYZ ASCII (<Lon> <Lat> <Depth in meters, positive up, relative to mean sea level>). Additional blockmedian grids have been computed with depth dependent cell size to visualize the data. These grids are not meant for scientific analysis or navigation, but for overview purposes only.

Multibeam bathymetry processed data (Atlas Hydrosweep DS 3 echo sounder entire dataset) of RV POLARSTERN during cruise PS127, Atlantic Ocean

Multibeam data were collected during RV Polarstern cruise PS127 (2021-12-04 to 2022-01-02). Multibeam sonar system was Atlas Hydrographic Hydrosweep DS 3 multibeam echo sounder. Data are processed with Caris HIPS, including sound velocity correction with SV data from SVPs, CTDs, UCTDs and World Ocean Atlas 13 (https://doi.org/10.7289/v5f769gt), tidal correction with TPXO9_atlas_v5 (https://www.tpxo.net), and manual cleaning. The soundings are combined in daily files, the format is XYZ ASCII (<Lon> <Lat> <Depth in meters, positive up, relative to mean sea level>). Additional blockmedian grids have been computed with depth dependent cell size to visualize the data. These grids are not meant for scientific analysis or navigation, but for overview purposes only.

Multibeam bathymetry processed data (Atlas Hydrosweep DS 2 echo sounder entire dataset) of RV POLARSTERN during cruise ANT-XIX/1 (PS61), Atlantic Ocean

Multibeam data were collected during RV Polarstern cruise ANT-XIX/1 (2001-11-08 to 2001-11-30). Multibeam sonar system was Atlas Hydrographic Hydrosweep DS 2 multibeam echo sounder. Data are processed with Caris HIPS, including sound velocity correction by cross fan calibration, tidal correction with TPXO9_atlas_v5 (https://www.tpxo.net), and manual cleaning. The soundings are combined in daily files, the format is XYZ ASCII (<Lon> <Lat> <Depth in meters, positive up, relative to mean sea level>). Additional grids have been computed with depth dependent cell size to visualize the data. These grids are not meant for scientific analysis or navigation, but for overview purposes only.

Meteogramm bis H+78 LROP Bukarest - Meteogram up to H+78 LROP Bucuresti Ufamati

3 Tage Vorhersage. Wind, Temperatur, Bodendruck, Bedeckung, Konvektionswolken und Niederschlag. - 3 days forecast. Wind, temperature, pressure mean sea level, cloud cover, convective clouds and precipitation.

Meteogramm bis H+78 08536 Lisboa/Portela - Meteogram up to H+78 08536 Lisboa/Portela

3 Tage Vorhersage. Wind, Temperatur, Bodendruck, Bedeckung, Konvektionswolken und Niederschlag. - 3 days forecast. Wind, temperature, pressure mean sea level, cloud cover, convective clouds and precipitation.

Sedimentbewegungen in der Deutschen Bucht

Zur Halbzeit eines BAW-Forschungsprojektes zum 'Aufbau von integrierten Modellsystemen zur Analyse der langfristigen Morphodynamik in der Deutschen Bucht' werden erste Ergebnisse sichtbar. Transportprozesse im Wandel der Zeitläufe: Wie werden sich die Watten und Vorländer der deutschen Nordseeküste anpassen, sollte in Folge des Klimawandels der Meeresspiegel steigen? Eine Antwort auf diese Frage ist nicht nur für die Sicherheit der Seedeiche bedeutsam, sondern auch für die Zufahrten zu den Seehäfen. Einerseits beeinflusst das Flachwasser im Ästuarbereich maßgebend das Tide- und Sedimentregime in den Tideflüssen und hat somit Auswirkungen auf die zukünftige Unterhaltung der Seehafenzufahrten. Zum anderen hat sich gezeigt, dass in einer Betrachtung über Jahrzehnte hinweg die kleinräumigen Transportprozesse in der Deutschen Bucht und in den Außenbereichen der Ästuare auch durch die Transportprozesse, die in der gesamten Nordsee stattfinden, mitgeprägt werden. Die Dimension dieser weiträumigen Transportprozesse in der Nordsee wird in der Satellitenaufnahme der oberflächennahen Ausbreitung der Schwebstofffahnen aus den Ästuarmündungen deutlich (Bild 1). Allerdings entzieht sich dieses Phänomen noch weitgehend der fachwissenschaftlichen Betrachtung, denn über die tatsächlichen Transportprozesse in der Nordsee, zumal in der Deutschen Bucht, ist wenig bekannt: Es fehlen zum Beispiel grundlegende, flächendeckende Informationen über das anstehende Material an der Gewässersohle, über den Bodenaufbau oder über die relevanten Kräfte, die den Transport antreiben, wie Wind und Seegang. Und schließlich fehlen die geeigneten Werkzeuge, um die komplexen Transportprozesse berechnen zu können. BAW hat Federführung bei Forschungsprojekt: Im Rahmen eines im Wettbewerb ausgeschriebenen Forschungsschwerpunktes des Kuratoriums für Forschung im Küsteningenieurwesen (KFKI) konnte sich die BAW mit einem Forschungsantrag zum Thema 'Aufbau von integrierten Modellsystemen zur Analyse der langfristigen Morphodynamik in der deutschen Bucht (AUFMOD)' durchsetzen. An dem Projekt unter Federführung der BAW beteiligen sich weitere neun Kooperationspartner. Gestartet Ende 2009, läuft die Förderung zunächst bis 2012 (siehe: www.kfki.de/prj-aufmod/de).

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