Near-surface ocean currents are a critical component of the Earth system, mediating the transfer of heat, momentum, and trace gasses between ocean and atmosphere (Cronin et al., 2019;Elipot & Wenegrat, 2021). These currents regulate marine ecosystems by transporting nutrients and phytoplankton laterally within the eutrophic zone (Barton et al., 2010;Resplandy et al., 2011), and they transport marine debris and plastic pollution around the globe (Van Sebille et al., 2020). Observed ocean surface currents are also used to evaluate the accuracy and biases of numerical ocean models. As a result, the oceanographic community requires accurate and detailed knowledge of the state of ocean surface currents.Satellite-based observations of sea-surface height (SSH), which is directly proportional to surface pressure, can be used to infer surface velocities via geostrophic balance. Modern ocean altimetry products like Archiving, Validation, and Interpretation of Satellite Oceanographic data (Ducet et al., 2000) typically have grid resolution of around 0.25° and an effective resolution of approximately 200 km. At this scale, geostrophic balance holds well, and altimetry-derived near-surface geostrophic velocities are used in many studies of ocean currents (e.g.,