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The figures below explain the Reporting Points map layer.
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The reporting points are created using the following process. For each NWP-driven forecast, a flood probability is computed for each return period flood threshold (2-year, 5-year and 20-year) using the maximum forecast discharge value over the 10-day forecast horizon. This flood probability is only computed on the large rivers with an upstream area > 250 km2. Very dry areas are also excluded by filtering the rivers with a 1.5-year return period < 1 m3/s. A total probability of exceedance is computed from these maximum forecast probabilities (from DWD-HRES, ECMWF-HRES, ECMWF-ENS and COSMO-LEPS). The weights of the forecasts in the total probability are equals but, in order to avoid the predominance of deterministic forecasts in the region where COSMO-LEPS is not available, we impose a ratio of 50% deterministic, 50% probabilistic in the computation of the total probability. This gives the two cases (DWD-HRES, ECMWF-HRES,ECMWF-ENS, COSMO-LEPS):
The persistence probability is then calculated by averaging the total probabilities from the current and the previous forecast. Reporting points are finally created (and their alert levels are computed) based on the following rules:
In regions where no static points (hydrological stations) are available from the EFAS hydrological database, an algorithm is used to generate dynamic points. The algorithm is based on the following properties:
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Pop-out windows
Additional local information associated with the reporting points layers is available from the mapviewer as pop-up plots. They display information such as:
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