ANTARCTIC CIRCULATION - GEOGRAPHY

News: Will climate change result in slowing down Antarctic circulation?

 

What's in the news?

       Antarctic circulation could slow by more than 40% over the next three decades, with significant implications for the oceans and climate.

       Such decline of the ocean circulation will stagnate the bottom of the oceans and generate further impacts, affecting climate and marine ecosystems for centuries to come.

 

Key takeaways:

       Cold water that sinks near Antarctica drives the deepest flow of the overturning circulation - a network of currents that spans the world's oceans. The overturning carries heat, carbon, oxygen and nutrients around the globe.

       This influences climate, sea level and the productivity of marine ecosystems.

 

Overturning Circulations:

       The “overturning circulation” of the oceans, driven by the movement of denser water towards the sea floor, helps deliver heat, carbon, oxygen and vital nutrients around the globe.

       Ocean overturning allows nutrients to rise up from the bottom, with the Southern Ocean supporting about three-quarters of global phytoplankton production, the base of the food chain.

 

Study:

       According to a release, Matthew England, Deputy Director of the ARC Centre for Excellence in Antarctic Science (ACEAS) at the University of New South Wales, Sydney, says the modeling shows that global carbon emissions continue at the current rate, then the Antarctic overturning will slow by more than 40% in the next 30 years and on a trajectory that looks headed towards collapse.

       As temperatures rise, freshwater from Antarctica’s melting ice enters the ocean, reducing the salinity and density of the surface water and diminishing that downward flow to the sea’s bottom.

       The study’s findings also suggest the ocean would not be able to absorb as much carbon dioxide as its upper layers become more stratified, leaving more CO2 in the atmosphere.