But it is becoming increasingly clear that
future changes in the ocean currents will help determine the future survival of the ice sheets.
Not exact matches
[Response: Here's a simple back - of - envelope consideration for the
future: if the Greenland ice sheet melts completely over the next ~ 1,000 years (Jim Hansen argues
in the
current Climatic
Change that the time scale could be centuries), this would contribute an average flux of ~ 0.1 Sv of freshwater to the surrounding
ocean.
The interactions between a recovering ozone hole, increasing greenhouse gases,
ocean currents, and other components of the climate system must still be explored
in order to better understand how the Earth's climate will
change in the
future.