Belgian risk of hail composite
Hail products are derived from the observed vertical profiles of radar reflectivity and the NWP vertical profiles of temperature. Three types of products are generated. poh : probability of hail of any size (larger than 0.5 cm diameter)expressed in %. posh : probability of severe hail(larger than 2cm)expressed in %. mesh : maximum expected size of hailexpressed in mm of hailstone diameter. All products are generated every 5 minutes. This product is not publically available yet.
Simple
- Date (Revision)
- 2024-10-01
- Identifier
- RMI-be / belgian_composite_hail
- Status
- On going
- Maintenance and update frequency
- Continual
- GEMET - INSPIRE themes, version 1.0
-
- Atmospheric conditions
- Keywords
-
- federal government
- hail
- observation
- Spatial scope
- Access constraints
- Other restrictions
- Other constraints
- No limitations on public access
- Use constraints
- Intellectual property rights
- Classification
- Unclassified
- Spatial representation type
- Grid
- Distance
- 500 http://standards.iso.org/ittf/PubliclyAvailableStandards/ISO_19139_Schemas/resources /uom/ML_gmxUom.xml#m
- Metadata language
- English
- Topic category
-
- Climatology, meteorology, atmosphere
N
S
E
W
- Begin date
- 2016-04-01T00:00:00
- Unique resource identifier
- EPSG:4258
- Distribution format
-
-
HDF
(
5
)
-
HDF
(
5
)
- OnLine resource
-
RMI opendata portal
(
WWW:LINK-1.0-http--link
)
RMI opendata portal
- Hierarchy level
- Dataset
- Other
- dataset
Domain consistency
- Name of measure
- INSPIRE Conformity
Conformance result
- Date (Publication)
- 2010-12-08
- Explanation
- See the referenced specification
- Pass
- No
- Statement
- Hail detection module is an implementation of two hail detection algorithms: of Witt and of Waldvogel (Waldvogelet al., 1979). The module takes radar observations and temperature information and estimates probability of hail (POH, %), probability of severe hail (POSH, %) and maximum expected size of hail (MESH, mm). The implementation of the Waldvogel algorithm is based on the Holleman s equation (I. Holleman, 2001), which was verified for Belgium by Delobbe et al. (2003). The POH is derived in the algorithm from the presence of a substantial updraft detected above the freezing level (0º-isoterm). The implementation of the Witt algorithm is based on the weighted integration of the reflectivity values between the heights of 0º-isoterm and -20º-isotherm (Witt et al., 1998). This algorithm provides POSH and MESH estimates.
- File identifier
- RMI_DATASET_BELGIAN_COMPOSITE_HAIL XML
- Metadata language
- English
- Hierarchy level
- Dataset
- Date stamp
- 2024-10-01
Overviews
Spatial extent
N
S
E
W
Provided by
Associated resources
Not available