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EU27_2020 basemap for EEA internal use

This Discomap web map service provides an EU-27 (2020) basemap for internal EEA use as a background layer in viewers or any other web application. It is provided as REST and as OGC WMS services, dynamic and cached. The cached service has a custom cache at the following scales: 1/50.000.000 1/42.000.000 1/36.000.000 (Europe's size) 1/30.000.000 1/20.000.000 1/10.000.000 1/5.000.000 1/2.500.000 1/1.000.000.

HW-gefährdeter Bereich Tidegebiet Elbe Hamburg

Hochwasser gefährdeter Bereich Tidegebiet Elbe Hamburg Fachliche Beschreibung: „Der durch Tidehochwasser, insbesondere Sturmfluten, gefährdete Bereich im Tidegebiet der Elbe besteht aus den Landflächen zwischen der Gewässerlinie der Elbe (§ 3) und der Linie der öffentlichen Hochwasserschutzanlagen oder, sofern öffentliche Hochwasserschutzanlagen nicht bestehen, der Linie des amtlich bekannt gemachten Bemessungswasserstands für öffentliche Hochwasserschutzanlagen zuzüglich eines Sicherheitszuschlags von 0,50 m." Auszug aus § 53 HWaG Rechtlicher Hintergrund: § 53 des Hamburgischen Wassergesetzes (HWaG) in der Fassung vom 29.05.2005 über "Hochwassergefährdeter Bereich im Tidegebiet der Elbe"

NECPR: Additional Reporting Obligations in the area of Renewable Energy (Annex XVI) dataset, 2023

Additional reporting in the area of renewable energy is a dataset under the National Energy and Climate Progress Reports (NECPRs), which is reported every second year (starting in 2023) by EU Member States. The dataset provides information regarding Member States functioning system for guarantees of origin (GO), renewable energy surplus/deficits, biomass use and impacts, and renewable energy usage in buildings. The EEA collects and quality checks this data. The dataset links to data from Eurostat. This reporting obligation comes from the Governance Regulation 2018/1999, Implementing Regulation (EU) 2022/2299 (Annex XVI).

Late-Glacial and Holocene vegetational stability of southern South America

This project focuses on the long-term stability (or otherwise) of vegetation, based on a series of multi-proxy records in southern South America. We will build a network of sites suitable for high-resolution reconstructions of changes in vegetation since the Last Glacial Maximum, and use these to test a null hypothesis that changes in vegetation over the past 14,000 years are driven by internal dynamics rather than external forcing factors. The extent to which the null hypothesis can be falsified will reveal the degree to which we can expect to be able to predict how vegetation is affected by external events, including future climate change. The southern fringes of the South American landmass provide a rare opportunity to examine the development of moorland vegetation with sparse tree cover in a wet, cool temperate climate of the Southern Hemisphere. We present a record of changes in vegetation over the past 17,000 years, from a lake in extreme southern Chile (Isla Santa Inés, Magallanes region, 53°38.97S; 72°25.24W; Fontana, Bennett 2012: The Holocene), where human influence on vegetation is negligible. The western archipelago of Tierra del Fuego remained treeless for most of the Lateglacial period. Nothofagus may have survived the last glacial maximum at the eastern edge of the Magellan glaciers from where it spread southwestwards and established in the region at around 10,500 cal. yr BP. Nothofagus antarctica was likely the earlier colonizing tree in the western islands, followed shortly after by Nothofagus betuloides. At 9000 cal. yr BP moorland communities expanded at the expense of Nothofagus woodland. Simultaneously, Nothofagus species shifted to dominance of the evergreen Nothofagus betuloides and the Magellanic rain forest established in the region. Rapid and drastic vegetation changes occurred at 5200 cal. yr BP, after the Mt Burney MB2 eruption, including the expansion and establishment of Pilgerodendron uviferum and the development of mixed Nothofagus-Pilgerodendron-Drimys woodland. Scattered populations of Nothofagus, as they occur today in westernmost Tierra del Fuego may be a good analogue for Nothofagus populations during the Lateglacial in eastern sites. Climate, dispersal barriers and/or fire disturbance may have played a role controlling the postglacial spread of Nothofagus. Climate change during the Lateglacial and early Holocene was a prerequisite for the expansion of Nothofagus populations and may have controlled it at many sites in Tierra del Fuego. The delayed arrival at the site, with respect to the Holocene warming, may be due to dispersal barriers and/or fire disturbance at eastern sites, reducing the size of the source populations. The retreat of Nothofagus woodland after 9000 cal. yr BP may be due to competitive interactions with bog communities. Volcanic disturbance had a positive influence on the expansion of Pilgerodendron uviferum and facilitated the development of mixed Nothofagus-Pilgerodendron-Drimys woodland.

GreenCompas - Grüne Werkstoffe und energieeffiziente Prozesse für kreislauffähige Verbundprodukte durch Nutzung regionaler Potenziale und paneuropäischer Partnerschaften

Quarzsandabbau Sommerach

Die Heidelberg Materials Mineralik DE GmbH (ehem. Heidelberger Sand und Kies GmbH) plant, die Kiessandgewinnung Sommerach in dem Markt Schwarzach am Main und der Gemeinde Sommerach, Landkreis Kitzingen ausgehend vom aktuellen Gewinnungsfeld („Bestandsgenehmigung“) nach Süden zu erweitern („Erweiterungsfeld“). Auf der Grundlage der Lagerstättenerkundung und der Einstufung als grundeigener Rohstoff durch das Bayerische Landesamt für Umwelt ist hierzu ein bergrechtliches Planfeststellungsverfahren mit integrierter Umweltverträglichkeitsprüfung beim Bergamt Nordbayern zu führen. Der Abbau der Kiessande erfolgt insgesamt auf einer Fläche von 12 ha, die Gewinnung soll mittels Eimerkettenbagger erfolgen. Der geplante Abbauzeitraum beträgt etwa 6 Jahre. Daran schließen sich etwa 5 Jahre für die Weiterführung der Verfüllung nach Abbauende und etwa 2 weitere Jahre für vollständige Wiedernutzbarmachung des Standorts an. Die Aufbereitung der geförderten Kiessande findet im etwa 2,5 km südwestlich gelegenen Kieswerk Dettelbach statt. Nach Abschluss der Kiessandgewinnung verbleibt ein etwa 4 ha großer Restsee mit umgebenden wiederverfüllten Landflächen zurück. Für die Verfüllung wird extern angelieferter Fremdboden verwendet. Für den Restsee ist ggf. eine Nachnutzung als Beregnungsspeicher für den umliegenden Weinbau vorgesehen.

Floods Reference Spatial Datasets reported under Floods Directive - version 3.0, Mar. 2025

The Floods Directive (FD) was adopted in 2007 (https://eur-lex.europa.eu/legal-content/EN/TXT/?uri=celex:32007L0060). The purpose of the FD is to establish a framework for the assessment and management of flood risks, aiming at the reduction of the adverse consequences for human health, the environment, cultural heritage and economic activity associated with floods in the European Union. ‘Flood’ means the temporary covering by water of land not normally covered by water. This shall include floods from rivers, mountain torrents, Mediterranean ephemeral water courses, and floods from the sea in coastal areas, and may exclude floods from sewerage systems. This reference spatial dataset, reported under the Floods Directive, includes the areas of potential significant flood risk (APSFR), as they were lastly reported by the Member States to the European Commission, and the Units of Management (UoM).

Estimates of land surface air temperature changes homogenised using sparse input 20th Century reanalysis product 20CRv3

The data consist of 4 frozen gridded estimates as described in Gillespie et al, 2022. The data are presented as 5 degree resolution global fields over 1850-2014. Station data arising from the International Surface Temperature Initiative (ISTI) global databank of monthly holdings have been homogenised using 20CRv3 to identify breakpoints. Four distinct approaches to adjustment have been undertaken resulting in 4 separate estimates of the resulting series. The gridding is a simple gridbox average of any observations available within each 5 degree gridbox. Data is available for those global land areas for which underlying station data are available in teh ISTI holdings.

Flurstücke WBV

Die Gebiete der Wasser- und Bodenverbände in M-V sind über die Anlage 1 des Gesetzes über die Bildung von Gewässerunterhaltungsverbänden (GUVG) in der jeweils gültigen Fassung festgelegt. Sie basieren auf den oberirdischen Einzugsgebieten (EZG). Die Verbandskulissen enthalten alle Flurstücke in MV. Innerhalb der Landfläche MV werden die Flurstücke mit den EZG-Grenzen aufgeschnitten. Die Flurstücke bzw. Flurstücksteile erhalten eine Kennung, zu welchem Verbandsgebiet sie gehören.

Waterbase - UWWTD: Urban Waste Water Treatment Directive – reported data

The Urban Waste Water Treatment Directive concerns the collection, treatment and discharge of urban waste water and the treatment and discharge of waste water from certain industrial sectors. The objective of the Directive is to protect the environment from the adverse effects of the above mentioned waste water discharges. This series contains time series of spatial and tabular data covering Agglomerations, Discharge Points, and Treatment Plants.

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