Atlantic Meridional Overturning Circulation
SEO Title: Atlantic Meridional Overturning Circulation (AMOC): Ocean Currents, Climate and Global Impact
Category: Environment & Ecology | Climate Change | Oceanography
UPSC Notes
The Atlantic Meridional Overturning Circulation (AMOC) is a large-scale system of ocean circulation in the Atlantic Ocean that transports heat northward and cold, dense water southward.
Key Pointers
Major component of the global ocean circulation system.
Moves warm surface waters northward.
Cold, dense waters sink at high latitudes and return southward at depth.
Closely linked with the Atlantic Ocean's climate system.
Influences:
European climate
Tropical rainfall
Sea level patterns
Marine ecosystems
Climate change can affect ocean temperature, salinity and freshwater input, potentially influencing AMOC strength.
AMOC is different from a single surface current; it is a large-scale overturning circulation.
Prelims Focus: AMOC → Atlantic Ocean → heat transport → sinking cold water → climate regulation.
Share this article