De gebeurtenissen langs de bevaarbare waterlopen waren niet uitzonderlijk, maar eerder een typisch winterfenomeen, waarbij voor de traag reagerende waterlopen na verloop van tijd de verzadigde bodem een duidelijke rol speelt. In de periode 9-11 februari 2016 waren de afvoeren het hoogst. De retourperiodes waren niet extreem- ongeveer 2 jaar. In die periode werd ook de stormtijprocedure voor het Zeescheldebekken afgekondigd.
De hele periode was er een verhoogde waakzaamheid bij de permanentie van het Hydrologisch InformatieCentrum. Een constante opvolging van neerslag- en windverwachtingen en de gemeten peilen en afvoeren resulteerde in 67 actieve berichten voor de beheerders van de bevaarbare waterlopen. 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