Learn about the ground-based, ship-borne, balloon-borne, and airborne campaigns and small satellite field experiments that validate orbiting ESA EO satellites and support future mission development.
The CReSIS radar is a classic nadir-looking altimeter, i.e. the current system configuration does not support acquisition
However, the phases seem to be anti-correlated, which is currently being investigated.
parameterizations of the dependencies between sea surface emissivity at L-band and surface roughness, and perform validation of currently