is convection
is convection
Warm ocean currents cool as they flow along a coastline away from the equator because sand and minerals are transported by ocean currents away from the equator.
Ocean floor.
Deep currents flow along the ocean floor, primarily in the abyssal plains and deep-sea trenches. These currents are driven by differences in water density, temperature, and salinity. They play a crucial role in distributing heat, nutrients, and dissolved gases around the world's ocean.
Along warm water currents from the equator to the poles.
Along cold water currents from the poles to the equator.
deep currents streamlike movement of water that flow very slowly along the ocean floor. surface current can influence the climate of land are they flow past.
As water is on top of the ocean, wind pushes it along, creating a current. As it warms, it interacts with lower colder waters, pulling them along with it. As water cools, it rises and this interaction creates ocean currents.
Cold ocean currents sink under warm ocean currents to form deep ocean currents.
The shape of a continent can influence ocean currents by directing their flow. For example, a narrow passage between two landmasses can funnel and accelerate ocean currents, while a broad continental shelf can slow down and disperse currents. Additionally, the presence of peninsulas, bays, and capes can create eddies and turbulence in ocean currents.
An Antarctic density current is a flow of cold, dense water that moves along the ocean floor in the Southern Ocean. These currents are important for the transport of nutrients and influence the climate by helping to regulate heat distribution in the ocean. They can also play a role in the movement of marine life and the cycling of nutrients in the ocean.
Ocean currents is what forms surface currents. This starts deep in the ocean.