Eddies are small features with a large impact. They are where a lot of physical processes takes place in the ocean and are an integral part of our climate system. Coastal eddies have a major role in regulating the weather near the shore and are important for fisheries. In the open ocean, eddies bring nutrient-rich cold water up to the surface and are an important part of the global carbon cycle [1]. These eddies are rotating masses of water that have broken off from a strong front. Eddies are crucial to the transport of Heat, momentum, trace chemicals, biological communities, Oxygen (O2), and nutrients related to sea-life [2]. They are also active in air-sea interaction, both through response to weather and in shaping the patterns of warmth that drive the entire atmospheric circulation. Measurements of ocean colour and the fate of light in the ocean are extremely useful for describing biological dynamics in surface waters [3–5], thus the oceanographic communities has made a substantial commitment to remote sensing of ocean colour from space [6, 7] . Regional scale ocean colour imageries are particularly useful for space-borne studies of ocean margins because of the importance and dominance of Mesoscale features (upwelling plumes, eddies, filaments, and River Plumes) in continental shelf and slope waters [8]. The oceanic and coastal processes rapidly alter the optical properties of water and these effects gets manifested in the colour of the water [9].
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