Kuriosho current el nino current
The western side of continents tends to have cooler ocean temperatures because of cold ocean currents flowing towards the equator from the poles. These currents bring colder water to the western coasts, influencing the climate of the adjacent land areas.
Cold currents near coastlines often indicate the presence of upwelling. This is because upwelling brings cold, nutrient-rich waters from the ocean depths to the surface, leading to colder surface currents. Some examples of cold currents near coastlines that are associated with upwelling include the California Current, the Benguela Current, and the Canary Current.
Along cold water currents from the poles to the equator.
Ocean currents can transport warm or cold water from one region to another, affecting the temperature of nearby land. For example, warm currents can bring milder temperatures to coastal areas, while cold currents can result in cooler temperatures. Ocean currents also influence weather patterns by transferring heat, moisture, and nutrients, which can in turn impact climate.
Ocean currents are responsible for mixing heat evenly throughout the ocean. These currents transport warm water from the equator towards the poles and bring cold water from the poles towards the equator, helping to regulate global temperature. Winds also play a role in driving ocean currents and redistributing heat.
Both: Tidal currents that flow from the tropics will be warm, and if they flow from the poles will be cool.
Gulf Stream - warm ocean current Labrador - cold ocean current
makes a ksunami.
The Alaska, Northern Pacific, and California currents carry cold water in the Eastern Pacific ocean in the Northern Hemisphere.
Cold ocean currents sink under warm ocean currents to form deep ocean currents.
Deep ocean currents are predominantly cold.
Africa
No
The rising of the deep cold currents to the ocean surface is called
Cold ocean currents are not found in the northern part of Indian ocean due to excess heat from sun.
Cold ocean currents are not found in the northern part of Indian ocean due to excess heat from sun.
Currents