Research Highlight: Climate Model Predicts Faster Warming for the North Atlantic Ocean

As aerosol emissions decline, heat uptake in the North Atlantic could increase dramatically.

Researchers at Scripps Institution of Oceanography at UC San Diego have predicted faster rates of warming than previously predicted for the North Atlantic Ocean in a recent paper published in the Journal of Climate.  This warming could disrupt major oceanic cycles and have worldwide impacts on climate systems.

The researchers modeled scenarios based on possible future greenhouse gas and aerosol emission rates.  One likely scenario focuses on future decline in aerosols and continued increase of greenhouse gases in the atmosphere.  Aerosols are minute particles suspended in the atmosphere.  Some scatter sunlight, thereby actually acting as cooling agents.

The aerosol cooling effect is about 50 percent of the warming effect of anthropogenic carbon dioxide at present.  Aerosols released from human activities are pollutants, however, and their health concerns have triggered worldwide efforts to curb emissions.  An aerosol decline could spark an interesting catch-22:  Because of their cooling effect, this decline would accelerate ocean warming that is already being caused by increasing carbon dioxide emissions–most notably initiating major warming in the North Atlantic.
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Increased rates of warming in the North Atlantic could impact a key oceanic cycle, the Atlantic Meridional Overturning Circulation, or AMOC.  An important part of the Earth’s climate system, the AMOC is a large system of ocean currents – such as the Gulf Stream – that pulls warmer water from the tropics toward the North Atlantic where it cools, sinks into the deep ocean, and flows southward again.  Eventually the water is pulled back to the surface, where it warms and completes the circulation.  Because it distributes heat and energy, the AMOC plays a major role in sustaining worldwide climate patterns, and is especially important in regulating climate in northern Europe and coastal North America. 

A warmer North Atlantic could significantly weaken the AMOC.  The system is driven by changes in salinity and temperature; as the warm water moves north, it evaporates to become saltier and gets cooler in the northern latitudes, making it denser so it sinks.  Changes in water temperature in the North Atlantic could throw a wrench into this whole process.  In fact recent studies have shown that the AMOC may have started weakening over the past decade.  Greater weakening could have widespread impacts on climate and weather patterns.  While all of the exact consequences are still unknown, for instance, warmer water on the surface could fuel stronger hurricanes.

Read more at Research Highlight:  Climate Model Predicts Faster Warming for the North Atlantic Ocean