Ice mass loss from Antarctica and Greenland contributes
about 20% to the current rate of global sea level rise. This ice loss is
projected to increase over the coming century.
A recent article on The
Conversation raised the concept of “climate tipping points”: thresholds in
the climate system that, once breached, lead to substantial and irreversible
change.
Such a climate tipping point may occur as a result of the
increasingly rapid decline of the Antarctic ice sheets, leading to a rapid rise
in sea levels. But what is this threshold? And when will we reach it?
Read the story on The
Conversation - “Tipping point: how we predict when Antarctica’s melting ice sheets will flood the seas.”

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