The ocean surface current, a key variable for many scientific and operational applications, is only partially and indirectly observed from space. Altimetry provides the geostrophic component of the current (Fu et al., 1988), which is a dominant contribution to surface transport in most of the oceans, effectively resolving wavelengths larger than about 200 km wavelength (Ballarotta et al., 2019). The ageostrophic component, not synoptically observed yet, is locally sampled from drifting buoys (Elipot et al., 2016) or high-frequency radars near the coasts (Kim et al., 2008). If model estimates for ageostrophic current are available, in particular for the low-frequency part (Rio et al., 2014) the uncertainties are still high. Filling this gap with satellite measurements of the total surface current is the topic of active research, with several emerging concepts of spaceborne Doppler radar for either 1 km resolution local studies such as SEASTAR (Gommengin