1. Introduction
Mesoscale eddies are circular currents of water bodies that widely exist in the global oceans. They play a significant role in the transport of momentum, mass, heat, nutrients, salt, and other seawater chemical elements across the ocean basins. They also impact the global ocean circulation, large-scale water distribution, air-sea coupling, and biological activities [1]–[5]. Cyclonic (anticyclonic) eddies drive local upwelling (downwelling), leading to negative (positive) sea surface height (SSH) and sea surface temperature (SST) anomalies. The satellite-measured SSH and SST images can, therefore, be used to obtain information on the characteristics of oceanic eddies.