geo.be Metadata Catalog
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The ceilometer CL51 employs a pulsed diode laser LIDAR technology, where short, powerful laser pulses are sent out in a vertical or near-vertical direction. The reflection of light (backscatter) caused by clouds, precipitation or other obscuration is analysed and used to determine the cloud base height, the cloud layer height and the amount of clouds (in octas) in different layers.
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Points Of Interest - Economy interest contains point elements indicating the location of an economic activity, such as a brewery, wholesale market, (commercial, industrial) building, cooling tower, gas processing/disposal, slagheap, telecommunications, wind turbine, solar panel park in Belgium.
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RADCLIM is a historical dataset based on weather radar observations that provides gridded accumulated precipitation composites over Belgium and surrounding regions. The data are distributed in ODIM_H5 version 2.2 format. The reported quantity is accumulated precipitation (ACRR) for 5-minute and 1-hour accumulation periods. UTC is used as the time reference, and the timestamp in the filename corresponds to the end of the accumulation period. The dataset is produced on a 700 × 700 grid with 1 km spatial resolution in the Belgian Lambert 2008 projection (Lambert Conformal Conic).
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The DSM 1m, digital surface model at 1m-resolution, is a homogeneous and regular point grid indicating the height of the Earth’s surface level in order to model its landscape, also including objects on the surface such as vegetation and buildings. The DSM 1m is achieved by interpolating in Lambert 2008 source data in Lambert 72 and at a 1m-resolution from the Flemish (2013-2015) and Brussels (2021) Regions, and by adding Lambert 2008 data at 1m-resolution from the Walloon Region (2021-2022).
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UV Index derived from spectral measurements with a Brewer UV spectrophotometer. This product is not publically available yet.
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The Belgian seismic network of the Royal Observatory of Belgium (ROB), with about 45 permanent stations, is mainly dedicated to the monitoring and the scientific study of the seismic activity in Belgium. The ROB is also managing 3 stations in the Grand-Duchy of Luxemburg (in cooperation with the European Center for Geodynamics and Seismology). Earthquakes worldwide with magnitude greater than 4.5 – 5.0 are routinely recorded by the Belgian seismic network. The measurements on these recordings are sent to international seismological centers (EMSC and ISC) where data from stations worldwide are analyzed to furnish a global catalogue of earthquakes and phase arrival time models. We also provide real-time seismic signals from some Belgian stations to data exchange centers like ORFEUS (Observatories and Research Facilities for European Seismology) and IRIS (Incorporated Research Institutions for Seismology).To complement the seismic network, the Belgian accelerometric network was installed early in the 2000ies to furnish reliable data when strong ground motions saturate traditional seismometers. This network consists of 19 stations, is sensitive to accelerations of 1E-5 g (g is gravity at the Earth’s surface) and is an important tool for professionals in the field of earthquake engineering and engineering seismology (seismic hazard assessment). Currently, since 2014 the service is installing another network (“AcceleROB“) of 90 low-cost accelerometers. These sensors are calibrated to be sensitive to accelerations of 1E-3 g, which should be observed during any earthquake of local magnitude ML=3 or larger.
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The Royal Decree of 20 March 2026 establishing the marine spatial plan for the period 2026 to 2034 in the Belgian marine areas defines 20 shipping and ports zones: IMO shipping zones (Art. 14§2), Traffic separation schemes (Art. 14§2), IMO traffic separation scheme "Noordhinder South" (Art. 14§2.1°), IMO precautionary area "in the vicinity of Thornton and Blighbank" (Art. 14§2.10°), Other routes and traffic flows (Royal Decree) (Art. 14§2.11°-19°), IMO traffic separation scheme "Off Noordhinder" (Art. 14§2.2°), IMO precautionary area "Noordhinder Junction" (Art. 14§2.3°), IMO traffic separation scheme "At Westhinder" (Art. 14§2.4°), Separation line "At West Hinder" (Art. 14§2.4°), IMO precautionary area "At Westhinder" (Art. 14§2.5°), IMO area to be avoided "At Westhinder" (Art. 14§2.6°), IMO deep-water route "Approach to the Scheldt" (Art. 14§2.7°), IMO two-way route "Westpit" (Art. 14§2.8°), IMO precautionary area "At Gootebank" (Art. 14§2.9°), Anchorage area "Oostdyck" (Art. 14§3.1°), IMO anchorage area "At Westhinder" (Art. 14§3.2°), Maritime safety research zone: Zone 1 (Art. 14§5.1°), Maritime safety research zone: Zone 2 (Art. 14§5.2°), Maritime safety research zone: Zone 3 (Art. 14§5.3°). It replaces the 2020 Marine Spatial Plan. Please refer to the Belgian official gazette ("Moniteur belgeBelgisch Staatsblad") for official reference information.
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The Royal Decree of 20 March 2026 establishing the marine spatial plan for the period 2026 to 2034 in the Belgian marine areas defines 7 energy, cable and pipeline zones: Renewable energy zone: Zone 1, Eastern Zone (Art. 12§1), Princess Elisabeth renewable energy zone: Zone 2a, Noordhinder North (Art. 12§2.2a°), Princess Elisabeth renewable energy zone: Zone 2b, Noordhinder South (Art. 12§2.2b°), Princess Elisabeth renewable energy zone: Zone 2c, Fairybank (Art. 12§2.3°), Modular offshore grid for electricity transmission (Art. 12§4), Safeguard zone of the Eastern Zone (Art. 12§5), Pipeline and cable corridor (Art. 13§1). It replaces the 2020 Marine Spatial Plan. Please refer to the Belgian official gazette ("Moniteur belgeBelgisch Staatsblad") for official reference information.
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The Royal Decree of 20 March 2026 establishing the marine spatial plan for the period 2026 to 2034 in the Belgian marine areas defines 1 coastal protection experiments zone: Coastal protection belt (Art. 20§2). It replaces the 2020 Marine Spatial Plan. Please refer to the Belgian official gazette ("Moniteur belgeBelgisch Staatsblad") for official reference information.
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The law of 13 June 1969 defines “Belgian Continental Shelf” as follows: the seabed and the subsoil of the marine areas adjacent to the Belgian coast but beyond the Belgian territorial sea.