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In fluid dynamics, an eddy is the swirling of a fluid and the reverse current created when the fluid is in a turbulent flow regime. The moving fluid creates a space devoid of downstream-flowing fluid on the downstream side of the object. Fluid behind the obstacle flows into the void creating a swirl of fluid on each edge of the obstacle, followed by a short reverse flow of fluid behind the obstacle flowing upstream, toward the back of the obstacle.
The swirling water of an eddy can be more than 100 km (60 miles) in diameter. The center of some eddies is cool while the center of others is warm. Marine life is sparse in warm water eddies, where the water does not have many nutrients. Cold water eddies are usually full of nutrients and marine life. Eddies form when a bend in a surface ocean current lengthens and eventually makes a loop, which separates from the main current.
In that sense, ocean eddies are analogous to atmospheric weather-although their spatial scales are smaller and temporal scales longer because of differences between air and water. Currents, gyres and eddies transport water and heat long distances and help promote large-scale mixing of the ocean. In the process they also transport nutrients, salt and other chemicals and help regulate the planet’s weather, climate and marine ecosystems. Strong currents and eddies also influence shipping routes and have been known to damage oil platforms.
The water properties of eddies are also important in supplying nutrients to coastal zones and the surface ocean where plankton blooms may result. More than half of the kinetic energy of the ocean circulation is contained in the mesoscale eddy field, with the remainder largely contained in the large-scale circulation
In April, mesoscale eddies are observed along the western boundary of the. Sea of Okhotsk. It was established that seasonal variability of turbulent wind stress. and the baroclinic instability of the East-Sakhalin Current are major reasons of. mesoscale variability along the western boundary of the Sea of Okhotsk. Keywords mesoscale eddies ·Sea of Okhotsk ·eddy kinetic energy ·baroclinic. instability ·barotropic instability. The Sea of Okhotsk is one of the marginal seas in the north-western Paciﬁc Ocean . Initial potential temperature and salinity are extracted from the datasets. On the sea surface, potential temperature and salinity are corrected by adding.
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Ocean eddies are abundant in the Caribbean Sea. They are predominantly anti-cyclonic, have a warm core, and can be long-lived. They are thought to impact the local ecosystem by mixing low-salinity river waters with the nutrient-rich waters that upwell along the Venezuelan and Colombian coast. Since these eddies have the potential to store heat below the surface, they may influence the evolution of passing hurricanes. Modelling the lifecycle of Caribbean eddies. Survey of a Caribbean anticyclone. In February 2018, we performed a combined hydrographic and biological survey of a Caribbean anti-cyclone.
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