A team of researchers investigate why the ocean has been absorbing more carbon from the atmosphere in recent decades, and find ocean circulation could be responsible.
A team of researchers went back to the same part of Antarctic after a decade to see how the deep ocean had changed, and were surprised to find the deep ocean was fresher than they expected.
The Antarctic Circumpolar current, which wraps around Antarctica and connects the Atlantic, Indian and Pacific Oceans, is notoriously difficult to measure. Recently a group of researchers tackled the wild current, and found it was 30% stronger than scientists previously thought.
The first things we learn about the ocean are that it’s big and salty. We know that its bigness is an important factor for earth’s climate; the authors of this paper demonstrate that its saltiness is too, and that this can affect whether other earth-like planets are truly habitable.
A group of scientists have delved deeper to solve the puzzle of why the ocean around Antarctica has been cooling, while the rest of the ocean is rapidly warming.
A pair of scientists have figured out how to track deep ocean currents using gravity measurements from space.
Sluggish ocean circulation can’t keep up with global climate change and this has caused the North Atlantic to cool.