Ice Sheet (WAIS), representing 3 - 4 m of potential sea - level rise, is capable of flowing rapidly
into deep ocean basins.
Not exact matches
At high latitudes, they sink
deep into the
ocean basins.
Most of the
deep ocean warming is occurring in the subtropical
ocean gyres - vast rotating masses of water in each
ocean basin where near - surface currents converge and are forced downward
into the
ocean interior.