Summary: Surface ocean velocities estimated from HF-Radar are representative of the upper 0.3 - 2.5 meters of the ocean. The main objective of the near-real time processing is to produce the best product from available data at the time of processing.
Keywords:
HF Radar, Galicia, surface sea water velocity, near-real time
HF Radar, Galicia, surface sea water velocity, near-real time