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Continuous meteorological observations at DynaCom automatic weather station, Spiekeroog, Germany, 2025-01 to 2025-12

Data presented here were collected between January 2025 to December 2025 within the research unit DynaCom (Spatial community ecology in highly dynamic landscapes: From island biogeography to metaecosystems, https://uol.de/dynacom/ ) of the Universities of Oldenburg, Göttingen, and Münster, the iDiv Leipzig and the Nationalpark Niedersächsisches Wattenmeer. Experimental islands and saltmarsh enclosed plots were created in the back barrier tidal flat and in the saltmarsh zone of the island of Spiekeroog. Meteorological data were collected near the experimental setup, with a locally installed weather station located approximately 500m north of the southern shoreline. The weather station system used here was a ClimaSensor US 4.920x.00.00x that was pre-calibrated by the manufacturer (Adolf Thies GmbH & Co. KG, D-Göttingen). Data were recorded and saved within the Processcontrol Weather (c) -4H- JENA engineering GmbH (v20.1.0.1 2020) software in a sampling interval of 1 min, with an averaging time of 10 s. Date and time were given in UTC and the position was derived from the internal GPS system. Data handling was performed according to Zielinski et al. (2018): Post-processing of collected data was done using MATLAB (R2024b). Quality control was performed by (a) erasing data covering maintenance activities, (b) removing outliers, defined as data exhibiting changes of more than two standard deviations within one time step, and (c) visually checks.

Tagesberichte zur Luftgütesituation an den Messstationen des Luftmessnetzes in Mecklenburg-Vorpommern

Die Berichte werden in digitaler Form (ASCII-Dateien) erstellt. Die Messergebnisse werden entsprechend des Auswertungsintervalls als Tabellen für die Schadstoffe: Feinstaub (PM10 und PM2,5) Schwefeldioxid Ozon Stickstoffmonoxid Stickstoffdioxid Kohlenstoffmonoxid sowie den meteorologischen Parametern Windrichtung Windgeschwindigkeit Niederschlag und Temperatur bereitgestellt. Die Auswertung erfolgt für die 14 Messstationen des Landes: Rostock-Am Strande Rostock-Holbeinplatz Neubrandenburg Stralsund-Knieperdamm Schwerin-Obotritenring Wolgast-Oberwallstraße Gülzow Löcknitz Rostock-Stuthof Göhlen Leizen Garz Güstrow und Rostock-Warnemünde.

Salzflüsse im Weserästuar 2019/2020

Dieser Datensatz umfasst Monitoringdaten und Modellergebnisse (Hydronumerisches Modell) für das Weserästuar, Nordsee. Die Daten wurden für quantitative Analysen in dem Manuskript „Surges control Salt Flux Variability in a partially-mixed Estuary“ verwendet, das im Journal of Geophysical Research: Oceans zur Veröffentlichung eingereicht wurde. Die Modellergebnisse, wie im Manuskript beschrieben, umfassen Salzflüsse, die aus den simulierten Strömungsgeschwindigkeiten und Salzgehalten abgeleitet wurden. Die vier Salzflusskomponenten [kg s-1] enthalten ein barotrope Komponente (barotropic flux, Fbt), Tidal Pumping (tidal oscillatory salt flux, Fto), den Beitrag durch die ästuarine Austauschströmung (exchange flow contribution, Fex) und eine weitere Komponente, die durch intratidal veränderliche Scherraten (tidal oscillatory shear, Ftos) bestimmt wird. Die Salzflüsse wurden jeweils, entlang der Zeitreihe, für die Dauer eines Tidetages bestimmt. Jeder Schritt beginnt mit einem Stauwasser. Die zeitliche Auflösung beträgt daher eine Halbtide. Die Zeitreihe umfasst ein hydrologisches Jahr. Die Auflösung entlang des Ästuars beträgt 1 km. Zusätzlich zu den Salzflüssen wurden fünf weitere Parameter abgeleitet: die Tideasymmetrie (Strömungsgeschwindigkeit), der gezeitengemittelte Salzgehalt, der Tidenhub [m] sowie die gezeitengemittelte Schichtung (potenzielle Energieanomalie) [J m-3]. Diese Parameter legen auf dem Gitter der Salzflusskomponenten vor. Die Salzintrusion ist in Flusskilometern angegeben und entspricht der Lage der Isohaline der Salinität von 2 PSU (gezeitengemittelt, bestimmt aus Modellergebnissen). Die übrigen Parameter im Datensatz wurden aus Monitoringdaten ermittelt. Hierzu zählen Zeitreihen der Windkomponente des Wasserstands [m], der Windgeschwindigkeit [m s-1] sowie der Windrichtung [°], abgeleitet von Messungen am Leuchtturm Alte Weser. Die spezifischen Methoden für jeden Monitoringparameter sind im Manuskript beschrieben. Dazu kommt noch der Abfluss (Intschede) [m3 s-1]. Alle Daten liegen als selbsterklärende Textdateien mit Kopfzeile vor. This dataset contains monitoring data and numerical model results for the Weser estuary, North Sea, used for quantitative analyses in the paper “Surges control Salt Flux Variability in a partially-mixed Estuary”, which was submitted to the Journal of Geophysical Research: Oceans. Model results comprise salt fluxes, derived from simulated velocity and salinity, as described in the paper. The four salt flux contributions [kg s-1] are the barotropic flux (Fbt), the tidal oscillatory salt flux (Fto), the exchange flow contribution (Fex) and the flux due to tidal oscillatory shear (Ftos). Salt fluxes were determined for the duration of one tidal day, moving stepwise through the timeseries. Each step starts with one slack water. Therefore, the temporal resolution is one value per tidal phase, as described in detail in the manuscript. The time series covers one hydrological year. The along-channel resolution is 1 km. Five additional parameters are derived from model results: the tidal velocity asymmetry, tidally averaged salinity, tidal range [m], and tidally averaged stratification (potential energy anomaly [J m-3]), all stored on the same spatiotemporal grid as the salt flux contributions. The salt intrusion is obtained from subtidal salinity using the location of the isohaline 2 (PSU). The salt intrusion is stored in terms of river km. The remaining parameters in the dataset are derived from monitoring data. These are time series of discharge [m3 s-1], surge [m], tidal range [m], wind speed [m s-1] and wind direction [°], all provided on the same temporal grid as the salt fluxes. The specific methods are described in the paper, for each of the monitoring parameters. All data are stored as self-explanatory, character-delimited text files with header lines.

MOSES Sternfahrt-10, Elbe water distribution and dispersion of pollutants from the Elbe outflow into the Northern Sea (German Bight), in 2023

The Sternfahrt-10 of the MOSES campaign, from 29th August until the 15th of September 2023, had two objectives. One was to follow the dispersion of pollutants, previously observed during the Elbe-Freshwater and Elbe-Tidal cruises, transported by the Elbe water into the North Sea. And second, on this occasion, the distribution of the Elbe water within the German Bight should be followed. To realize this, two drifter groups were deployed in the southern and, respectively, northern branch of the Elbe valley, which were continuously monitored by scientists at the Hereon institute. Further, the drifters were subsequently followed by three ships (RV Ludwig Prandtl, RV Littorina, RV Mya II), for in total three weeks, to measure hydrographic parameters multiple times along their journey. Additionally, to this stationary sampling, basic hydrographic parameters and dissolved methane were measured continuously along the tracks (content of the presented dataset). To ensure the comparability of the data from all three vessels a container was transferred from ship to ship. This "MOSES laboratory-container" was equipped with several sensors, amongst others a pocket FerryBox and a Greenhouse Gas Analyser (Los Gatos). The Ludwig Prandtl started the campaign on August 29th in Cuxhaven and deployed the drifters in the respective areas of the Elbe outflow section of the German Bight. Until the 1st of September the crew followed the drifters to sample this water body. Not all drifters could be reached every day, because it was too shallow, in this case the vessels occupied MOSES hydrographic stations from previous Sternfahrt cruises. On September 4th the vessel Littorina took over and started the second part of the campaign navigating from Cuxhaven to Heligoland covering as many drifter positions as possible. Until the 7th of September the crew sampled in the north eastern part of Heligoland up to Büsum. The handover of the container for the last episode of the cruise took place in Heligoland to the vessel Mya II. From there the crew navigated on September 12th towards west off the island Amrum. In the following days until September 14th, they sampled west off Heligoland to west off St. Peter-Ording. For more details about the exact tracks of the ships, have a look at the added map. More detailed information about the MOSES project and the Sternfahrten, see article cited in references.

Datenarchiv Langzeitmessungen/ kontinuierliche Messungen in Mecklenburg-Vorpommern

Der Datenbestand setzt sich aus kontinuierlichen Messreihen der Hauptluftschadstoffe - Feinstaub/PM10 und PM2,5 (bis 1998 Schwebstaub) - Stickstoffmonoxid (NO) - Stickstoffdioxid (NO2) - Ozon (O3) - Schwefeldioxid (SO2) - Kohlenmonoxid (CO) - Benzol/ Toluol - Ruß und den sie begleitenden meteorologischen Parametern - Windrichtung (WR) - Windgeschwindigkeit (WG) - Luftdruck (Ld) - relative Feuchte (Frel) - Niederschlag (NS) und - Temperatur (Temp) zusammen. Diese Daten werden gegenwärtig in 14 vollautomatisch betriebenen Messcontainern an folgenden Standorten gewonnen: verkehrsnah gelegene Messstationen: Neubrandenburg, Rostock-Am Strande, Rostock-Holbeinplatz, Schwerin-Obotritenring, Stralsund-Knieperdamm, Wolgast-Oberwallstraße; ländlich gelegene Messstationen: Gülzow, Göhlen, Löcknitz, Rostock-Stuthof, Leizen, Garz, Zarrentin (bis 14.6.2010), Selmsdorf (bis 30.11.2000); Messstationen im städtischen Hintergrund: Güstrow, Rostock-Warnemünde. An einigen dieser Messstationen wurden darüber hinaus Geräte zur diskontinuierlichen Feinstaubsammlung installiert, um nach Laboranalysen Kenntnisse über die Inhaltsstoffe des Feinstaubs (PAK, Schwermetalle und ionische Bestandteile) zu gewinnen.

Windgeschwindigkeit und - Richtung (Klimaanalyse)

Windgeschwindigkeit und -richtung. Ähnlich der Fließrichtung der Kaltluft für die Planungshinweiskarte beschreibt dieses Produkt die Windgeschwindigkeit und -richtung der Kaltluft, jedoch für die landesweite Klimaanalysekarte. Mehr dazu: https://pd.lubw.de/10677

Fließrichtung der Kaltluft (Klimaanalyse)

Fließrichtung der Kaltluft. Das Produkt ist Teil der landesweiten Planungshinweiskarte und zeigt als Raster das Windfeld, das sich zur betrachteten Uhrzeit im Klimamodell eingestellt hat. Mehr dazu: https://www.lubw.baden-wuerttemberg.de/klimawandel-und-anpassung

Meteorological data of Time Series Station Spiekeroog for 2018

The Time Series Station Spiekeroog (TSS) was setup in 2002, in the tidal inlet between the East Frisian Islands of Langeoog and Spiekeroog in the Southern German Bight, at position 53°45′01.0″ N, 007°40′16.3″ E. The aim was to ensure the continuous measurement of physical, biological, chemical and meteorological parameters, even under extreme weather conditions such as storms, ice, and storm surges. The TSS was financed as part of the Deutsche Forschungsgemeinschaft (DFG) research unit BioGeoChemistry of Tidal Flats and the Ministry for Science and Culture of the Land of Lower Saxony (MWK). Here, air temperature, air pressure, relative humidity, wind speed and wind direction were measured in the year 2018. All raw data were revised and corrected for steps as range, outliers and stationarity checks. A detailed description of the Time Series Station Spiekeroog, its structure and instrumentation can be found in Zielinski et al. (2022) and in Reuter et al. (2009).

Meteorological data of Time Series Station Spiekeroog for 2008

The Time Series Station Spiekeroog (TSS) was setup in 2002, in the tidal inlet between the East Frisian Islands of Langeoog and Spiekeroog in the Southern German Bight, at position 53°45′01.0″ N, 007°40′16.3″ E. The aim was to ensure the continuous measurement of physical, biological, chemical and meteorological parameters, even under extreme weather conditions such as storms, ice, and storm surges. The TSS was financed as part of the Deutsche Forschungsgemeinschaft (DFG) research unit BioGeoChemistry of Tidal Flats and the Ministry for Science and Culture of the Land of Lower Saxony (MWK). Here, air temperature, air pressure, relative humidity, wind speed and wind direction were measured in the year 2008. All raw data were revised and corrected for steps as range, outliers and stationarity checks. A detailed description of the Time Series Station Spiekeroog, its structure and instrumentation can be found in Zielinski et al. (2022) and in Reuter et al. (2009).

Wetterstation Gewerbegebiet Stadt Ingolstadt

Im Rahmen eines EU-Förderprojekts namens DS4LoReMa wurden Wetterstationen im Untersuchungsgebiet Gewerbegebiet Südost von Ingolstadt aufgestellt, um diese in den Digitalen Zwilling für Energie und Klima zu integrieren und ein Wetter- und Klimadashboard zu erstellen. As part of an EU-funded project called DS4LoReMa, weather stations were set up in the study area of the southeast industrial park in Ingolstadt to integrate them into the digital twin for energy and climate and to create a weather and climate dashboard. Koordinaten: (48.740231N, 11.467381E)

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