The LISFLOOD static and parameter maps for Europe contain
all gridded input maps (except for the meteorological forcings that can be found here https://data.jrc.ec.europa.eu/dataset/0bd84be4-cec8-4180-97a6-8b3adaac4d26) that are required to run the spatially distributed hydrological model LISFLOOD for Europe. Details on the open-source hydrological model LISFLOOD can be found here: https://ec-jrc.github.io/lisflood/ . The LISFLOOD static maps have been derived using a variety of different data sources and have a spatial resolution of 1 arc min (approx. 1.5km). A detailed description of how the maps have been derived can be found here: https://ec-jrc.github.io/lisflood-code/4_Static-Maps-introduction/. The LISFLOOD parameter maps have been derived using model calibration and a parameter regionalization technique.
Christel Prudhomme; Cinzia Mazzetti
; Francesca Moschini
; Hylke Beck
; Juliana Disperati; Margarita Choulga
; Peter Salamon
; Stefania Grimaldi
Choulga, Margarita; Moschini, Francesca; Mazzetti, Cinzia; Grimaldi, Stefania; Disperati, Juliana; Beck, Hylke; Salamon, Peter; Prudhomme, Christel (2026): LISFLOOD static and parameter maps for Europe. European Commission, Joint Research Centre [Dataset] doi: 10.2905/JRC.1YHPHC8 PID: http://data.europa.eu/89h/f572c443-7466-4adf-87aa-c0847a169f23
droughtsfloodshydrologymodeling
The LISFLOOD static maps have been derived using a variety of different data sources and have a spatial resolution of 1 arc min (approx. 1.5km). A detailed description of how the maps have been derived can be found here: https://ec-jrc.github.io/lisflood-code/4_Static-Maps-introduction/. The LISFLOOD parameter maps have been derived using model calibration and a parameter regionalization technique.