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This analysis evaluated the skill of the ERIC flash flood products when compared against flash flood observations, the results are used to decide the criteria for issuing flash flood notifications. It was necessary to perform a new skill assessment for EFAS v5.0 to decide these criteria, rather than using the criteria from EFAS v4.1 because of the following changes:

  • The new calibration of the LISFLOOD hydrological model which is used within the generation of the ERIC flash flood products
  • The ERIC products are now calculated directly from the surface runoff predictions from LISFLOOD, previously precipitation was combined with LISFLOOD predictions of soil moisture to estimate surface runoff

The evaluation was performed for ERIC flash flood predictions between 1st January 2022 - 31st December 2022

Flash Flood Observations

Observations of flash floods during the evaluation period were obtained from three sources:

  • EFAS partner feedback
  • FloodList.com
  • EFAS long term run (river discharge re-analysis)
EFAS Partner Feedback

EFAS partners are able to provide feedback in response to each flash flood notification email they receive, they can inform if the flash flood event did or did not occur. Therefore the feedback received during the evaluation period was selected and events where a flash flood did occur were chosen. 42 flash flood events were reported by EFAS partners during the evaluation period

FloodList.com

Flash flood events were obtained from an API collated by FloodList.com. The API was queried to return events which matched the following criteria:

  • Occurred during the evaluation period
  • Occurred within the EFAS domain
  • Flood event type was recorded as either 'flash flood' or 'minor flood', the latter was included as this refers to flooding with a small spatial and temporal scale which is similar to flash flooding

Some of the extracted flash flood events were recorded as having a duration of several days, whereas normally flash flooding occurs within a 24 hour timescale. This longer duration could be because other types of flooding were recorded during the same event, for example longer lasting riverine flooding may have occurred later on further downstream. Uncertainty in the timing of the reported flash flood event could also explain the longer duration. In these cases it was decided to only record the first date on which the flash flooding was reported as this would coincide with the initial heavy rainfall which is often associated with most flash flooding impacts.

  

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