Atlantic Meridional Overturning Circulation (AMOC)

Syllabus: GS1/ Geography 

Context

  • Recently, a climate study found that if the Atlantic Meridional Overturning Circulation (AMOC) collapses, Europe could face a dramatic and prolonged winter freeze, even in a world warmed by greenhouse gas emissions.

About Atlantic Meridional Overturning Circulation (AMOC)  

  • It is one of the most powerful and complex systems driving Earth’s climate. 
  • It is often likened to a giant conveyor belt that transports warm surface waters from the tropics northward and returns cold, dense water southward at depth.
  • It regulates temperatures across the Atlantic basin and plays a vital role in global climate stability, sea-level patterns, and marine ecosystems.
Atlantic Meridional Overturning Circulation

Working of AMOC

  • The AMOC is a key component of the global thermohaline circulation
  • Warm, salty water flows northward via currents like the Gulf Stream. As it reaches higher latitudes, it cools and becomes denser, sinking into the deep ocean and flowing back south. 
  • It helps distribute heat and nutrients across the globe, influencing weather patterns from the Amazon to the Arctic.

Slowing of AMOC and the Tipping Point

  • Recent studies suggest that the AMOC has weakened significantly since the mid-20th century, and is expected to slow by 18–43% by 2100.
  • It is primarily driven by climate change, particularly the influx of freshwater from melting Greenland ice, which disrupts the salinity and density gradients that power the current.
  • AMOC may be approaching a tipping point, beyond which its collapse could trigger abrupt and irreversible climate shifts.
    • AMOC has two potential tipping points — one linked to salt transport feedback and another to deep ocean convection.
Climate Tipping Points  
– These are critical thresholds in Earth’s systems—once crossed, they can trigger self-reinforcing feedback loops that lead to abrupt, irreversible, and potentially catastrophic changes.
– They occur when a small change in temperature or pressure pushes a system — like an ice sheet, rainforest, or ocean current — into a radically different state.
Key Tipping Elements at Risk
– Recent assessments have identified at least 16 major Earth system components that are vulnerable to tipping, including:
1. Greenland and West Antarctic Ice Sheets;
2. Atlantic Meridional Overturning Circulation (AMOC);
3. Amazon Rainforest Dieback;
4. Arctic Permafrost Thaw;Coral Reef Collapse;

Potential Consequences

  • Europe may face colder winters despite global warming, as warm currents fail to reach its shores.
  • West Africa could see disrupted monsoon patterns, affecting agriculture and water security.
  • Eastern North America might experience accelerated sea-level rise.
  • The Amazon and South Asia could suffer from altered rainfall patterns, increasing drought risk.
Ocean Currents
– Horizontal and vertical components of the circulation system of ocean waters.
Types
Surface Currents: Surface Circulation
Deep Water Currents: Thermohaline Circulation
Forces
Primary: Solar Heating, Winds, Gravity, Coriolis force
Secondary: Temperature, Salinity & Density Difference

Ocean Currents

Source: DTE

 

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