DWD’s fully automatic MOSMIX product optimizes and interprets the forecast calculations of the NWP models ICON (DWD) and IFS (ECMWF), combines these and calculates statistically optimized weather forecasts in terms of point forecasts (PFCs). Thus, statistically corrected, updated forecasts for the next ten days are calculated for about 5400 locations around the world. Most forecasting locations are spread over Germany and Europe. MOSMIX forecasts (PFCs) include nearly all common meteorological parameters measured by weather stations. For further information please refer to: [in German: https://www.dwd.de/DE/leistungen/met_verfahren_mosmix/met_verfahren_mosmix.html ] [in English: https://www.dwd.de/EN/ourservices/met_application_mosmix/met_application_mosmix.html ]
DWD’s fully automatic MOSMIX product optimizes and interprets the forecast calculations of the NWP models ICON (DWD) and IFS (ECMWF), combines these and calculates statistically optimized weather forecasts in terms of point forecasts (PFCs). Thus, statistically corrected, updated forecasts for the next ten days are calculated for about 5400 locations around the world. Most forecasting locations are spread over Germany and Europe. MOSMIX forecasts (PFCs) include nearly all common meteorological parameters measured by weather stations. For further information please refer to: [in German: https://www.dwd.de/DE/leistungen/met_verfahren_mosmix/met_verfahren_mosmix.html ] [in English: https://www.dwd.de/EN/ourservices/met_application_mosmix/met_application_mosmix.html ]
The dataset is an extended and updated version of the homogenized regional earthquake catalogue of the Marmara region, north-western Turkey, presented in Bohnhof et al. (2017) and Wollin et al. (2018). It is built on the regional Turkish seismicity catalogues provided by AFAD (Disaster and Emergency Management Presidency of Turkey) and KOERI (Kandilli Observatory and Earthquake Research Institute) and spans the time interval 2006-2020. All events available in these two catalogues in the wider Marmara region were combined and dublicate events removed. A total of 13812 events having at least 6 P- and/or S-picks were located using the NLLoc software (Lomax et al., 2000, 2009) in Octtree mode utilizing automatic picks (see Wollin et al., 2018 for details) for all available waveforms. The magnitude range is between M0.3 and M5.7 with time-variable magnitude of completeness and covers the area 39.70S-41.50S and 26.0E-30.65E. The full description of the data and methods is provided in the data description file.
This dataset presents the raw data from two experimental series of analogue models and four numerical models performed to investigate Rift-Rift-Rift triple junction dynamics, supporting the modelling results described in the submitted paper. Numerical models were run in order to support the outcomes obtained from the analogue models. Our experimental series tested the case of a totally symmetric RRR junction (with rift branch angles trending at 120° and direction of stretching similarly trending at 120°; SY Series) or a less symmetric triple junction (with rift branches trending at 120° but with one of these experiencing orthogonal extension; OR Series), and testing the role of a single or two phases of extension coupled with effect of differential velocities between the three moving plates. An overview of the performed analogue and numerical models is provided in Table 1. Analogue models have been analysed quantitatively by means of photogrammetric reconstruction of Digital Elevation Model (DEM) used for 3D quantification of the deformation, and top-view photo analysis for qualitative descriptions. The analogue materials used in the setup of these models are described in Montanari et al. (2017), Del Ventisette et al. (2019) and Maestrelli et al. (2020). Numerical models were run with the finite element software ASPECT (e.g., Kronbichler et al., 2012; Heister et al., 2017; Rose et al., 2017).
The Ethiopian rift is a unique natural environment to study the different stages of evolution from initial continental rifting to embryonic sea-floor spreading. We study the crust and uppermost mantle of the Afar, Main Ethiopian Rift and the adjoining plateaus using hierarchical Bayesian ambient seismic noise tomography. A shear wave velocity model of the crust is produced based on the point-wise linearized inversion of the dispersion curves extracted from the group velocity maps. This dataset provides 3-D shear velocity results from Eshetu et al. (2021). The file “3dmod.dat” contains the shear wave velocity model for the Ethiopian rift, sampled onto a regular grid. Poorly imaged cells are set to “nan”, see the main text for details. Note that the model primarly resolves S wave structure (Vs). P wave velocity (Vp) is not independently constrained but, during the inversion, calculated from Vs using empirical relations (Brocher, 2005).
Der Echte Mehltau (Sphaerotheca humuli) ist in den letzten Jahren im Hopfenanbau in Europa und den USA zu einem schwerwiegenden Problem geworden. So sind anscheinend die meisten Resistenzen im gegenwaertigen Sortenspektrum durch neu entstandene Pathotypen zumindest teilweise ueberwunden. Um die Pathotypenvielfalt in den verschiedenen Hopfenanbaugebieten zu erfassen, werden Mehltauisolate aus Deutschland, USA, aus Frankreich und England auf ihr Infektionsvermoegen (Virulenz) gegenueber Hopfensorten und Staemmen mit unterschiedlichsten Resistenzen (R-Genen) getestet. Um die relativ hohe Anzahl an Analysen mit einem vertretbaren Aufwand durchfuehren zu koennen, wird in einem ersten Schritt ein miniaturisiertes Testverfahren mit Blattscheiben auf Agar etabliert. Letztlich sind durch diese Virulenzanalysen mit den verschiedenen Mehltauisolaten Aussagen moeglich, welche Resistenzgene noch einen effektiven Schutz darstellen und daher noch sinnvoll in der Hopfenzuechtung einzusetzen sind.
Ziel des Teilprojektes A2 des SFB 299 ist die Entwicklung einer Methode zur Modellierung des Landschaftswasser- und Stoffhaushaltes im meso- bis makroskaligen Bereich. Die Wirkung von Landnutzungsoptionen auf Komponenten des Wasser- und Stofftransportes soll hoch aufgeloest und flaechenhaft quantifiziert werden. Das physikalisch basierte Kontinuumsmodell SWAT (Arnold et al., 1993; 1995) wird in der ersten Projektphase in den Einzugsgebieten der Dietzhoelze (81,3 km2) und der Aar (61,1 km2) kalibriert und validiert. Im Modell implementierte Datenbanken werden durch lokale Datenbestaende ersetzt. Die Eingabe von flaechenhaften Eingabedaten erfolgt ueber ein Schnittstellenprogramm (SWATGRASS; Srinivasan, 1994) zum Raster-GIS GRASS. Nach der erfolgreichen Ueberpruefung des Modells anhand der aktuellen Landnutzungsdaten, die aus Landsat TM 5-Szenen stammen, werden Nutzungsvorschlaege vom oekonomischen Modell ProLand (TP A1) hinsichtlich ihrer hydrologischen Auswirkungen ueberprueft. Zur Bewertung einzelner Landnutzungkonzepte werden Indikatoren, die die hydrologischen Konsequenzen der veraenderten Nutzung charakterisieren, an Teilprojekt A4 geliefert.
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