Scientists have detected a 30% slowdown of the deep ocean currents that form in Antarctica, with profound consequences for Earth’s climate, sea level and marine life.
The Drake Passage, seen from Antarctica, is one of the most turbulent ocean regions on Earth.
Lilian Dove
Working with underwater robots, scientists show how deep sea mountains and fast currents between Antarctica and South America play a crucial role in stabilizing the climate.
In a plot reminiscent of the 2004 movie The Day After Tomorrow?, Australian scientists are warning that the Southern Ocean’s deep “overturning” circulation is slowing and headed for collapse.
A green turtle on Aldabra entangled in abandoned fishing gear.
Rich Baxter
Studying these deposits gives scientists information about how past environments change. That, in turn, gives us informed estimates on how climates and environments will change in the near future.
A computer animation reflects the temperature change as eddies spin off from the Loop Current and Gulf Stream along the U.S. Coast.
Ida exploded from a weak hurricane to a powerful Category 4 storm in less than 24 hours, thanks to heat from an ocean eddy. An oceanographer explains its rapid intensification.
Plastic fragments washed onto Schiavonea beach in Calabria, Italy, in a 2019 storm.
Alfonso Di Vincenzo/KONTROLAB /LightRocket via Getty Images
The grisly discovery of a disembodied foot on a NSW beach was a tragic twist in the mystery of missing woman Melissa Caddick. Such tragedies can also reveal hidden currents connecting the planet.
The Atlantic Ocean is still growing physically, but humans are over-harvesting its rich fisheries. The most famous one – North Atlantic cod – has become a textbook example of harmful overfishing.
A rockfish hides in a red tree coral in the deep sea.
Geofflos
Fish can’t read maps, and their eggs and larvae drift across national boundaries. Recent research shows that local problems in one fishery can affect others across wide areas.
Great areas of rubbish – known as ‘garbage patches’ – are known to form in the Pacific and Atlantic oceans, but not the southern Indian Ocean. Why is that?