Versions Compared

Key

  • This line was added.
  • This line was removed.
  • Formatting was changed.

...

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 area areas are also excluded by excluding filtering the rivers with a 1.5-year return period below < 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 equal 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):

  • Inside COSMO-LEPS domain: (25%, 25%, 25%, 25%)
  • Outside COSMO-LEPS domain: (25%, 25%, 50%, 0%)

The persistence probability is then calculated by averaging the total probabilities from the current and the previous forecast. Dynamic reporting Reporting points are finally created (and their alert levels are computed) based on the following rules:

  • 20-year return period: persistence probability > 30% and upstream area > 1000 km2km2.
  • 5-year return period: persistence probability > 30% and upstream area > 1000 km2km2.
  • 2-year return period: persistence probability > 50% and upstream area > 1000 km2

Alert levels are also computed for static reporting points where hydrological metadata information is available. The rules are different for these points:

  • 5-year return period: persistence probability > 10% or at least 3 COSMO-LEPS members exceeding the 5-year return period threshold, and upstream area > 1000 km2

  • 2-year return period: persistence probability > 10% and upstream area > 2000 km2

...

  • .

In regions where no static points (hydrological stations) are available, an algorithm is used to generate dynamic points. The algorithm is based on the following properties:

  • A dynamic point will be created at the most downstream location and at the peak signal location of a flood signal of at least 5 pixels.
  • Once a dynamic point is created, it stays on the map as long as a flood signal exceeding at least the 2-year return period is detected.
  • Points to close to each other are removed (points from previous forecasts will remain).
  • If two points are close to each other but are on different rivers (based on the upstream area > 1000 km2 network), the two points are kept.

Pop-out windows

Additional local information associated with each flood forecast layer (except for the ‘Flood Probability’ layers) the reporting points layers is available from the mapviewer as pop-up plots. They display information such as:

...

Below are some graphical aids to help to interpret and use reporting points' feature information products (these can be found under the Flood Summary layer group - Reporting Points layer, when clicking on a point on the EFAS-IS mapviewer).


...



...

 

...



...


...

Image Modified


...

Restrictions

...