Abstract. Satellite-based Earth observations (EO) are an accurate and
reliable data source for atmospheric and environmental science. Their
increasing spatial and temporal resolutions, as well as the seamless
availability over ungauged regions, make them appealing for hydrological
modeling. This work shows recent advances in the use of high-resolution
satellite-based EO data in hydrological modeling. In a set of six
experiments, the distributed hydrological model Continuum is set up for the
Po River basin (Italy) and forced, in turn, by satellite precipitation and
evaporation, while satellite-derived soil moisture (SM) and snow depths are
ingested into the model structure through a data-assimilation scheme.
Further, satellite-based estimates of precipitation, evaporation, and river
discharge are used for hydrological model calibration, and results are
compared with those based on ground observations. Despite the high density
of conventional ground measurements and the strong human influence in the
focus region, all satellite products show strong potential for operational
hydrological applications, with skillful estimates of river discharge
throughout the model domain. Satellite-based evaporation and snow depths
marginally improve (by 2 % and 4 %) the mean Kling–Gupta efficiency
(KGE) at 27 river gauges, compared to a baseline simulation
(KGEmean= 0.51) forced by high-quality conventional data. Precipitation
has the largest impact on the model output, though the satellite data on
average shows poorer skills compared to conventional data. Interestingly, a
model calibration heavily relying on satellite data, as opposed to
conventional data, provides a skillful reconstruction of river discharges,
paving the way to fully satellite-driven hydrological applications.