North Atlantic Ocean
Quick Summary
The North Atlantic is a vast body of saltwater, second in size only to the Pacific Ocean, separating Europe and Africa from the Americas. It is characterized by prevailing westerly winds, influenced by large-scale air currents and pressure systems like the Azores high and Icelandic low.12
A significant feature is the Gulf Stream, a warm and swift current originating from the Gulf of Mexico. This current flows northeastward, becoming the North Atlantic Current, which significantly moderates the climate of northwestern Europe. The North Atlantic is also a crucial oceanic highway, historically vital for trade and transportation between continents, with major ports in North America and Europe.345
Ask Britannica AI about this topic
Britannica doesn't have a full article on this topic, so we've curated a list of our relevant coverage.
ocean currentThermohaline circulation…regions, chiefly in the northern North Atlantic and near Antarctica. These dense water masses spread into the full extent of the ocean and gradually upwell to feed a slow return flow to the sinking regions. A theory for the thermohaline circulation pattern was proposed by Stommel and Arnold Arons in…
Read More…regions, chiefly in the northern North Atlantic and near Antarctica. These dense water masses spread into the full extent of the ocean and gradually upwell to feed a slow return flow to the sinking regions. A theory for the thermohaline circulation pattern was proposed by Stommel and Arnold Arons in…
Read More- climateThe ocean surface and climate anomalies
The circulation over the North Atlantic and northern Europe during early winter has been found to be sensitive to large ocean surface temperature anomalies south of Newfoundland. When a warm positive anomaly exists in this region, an anomalous surface anticyclone occurs in the atmosphere above the central Atlantic at…
Read MoreThe circulation over the North Atlantic and northern Europe during early winter has been found to be sensitive to large ocean surface temperature anomalies south of Newfoundland. When a warm positive anomaly exists in this region, an anomalous surface anticyclone occurs in the atmosphere above the central Atlantic at…
Read More

