The Greenland ice sheet is melting. At our current rate of increasing carbon emissions, we are
on track for it all to disappear. If that happens, mean sea-level (MSL) will rise by about
7 metres23 feet
(due to the Greenland ice sheet alone).
According to modelling and to historical data, there is a threshold beyond which
self-sustained melting will continue. This threshold has been modelled to occur at a global
mean temperature (GMT) between
above preindustrial
temperatures so we are, potentially, very close to that tipping point.
If/when we overshoot that threshold, but then manage to get GMT back to
1.5C 2.7F
above preindustrial temperatures, melting would slow and eventually stop. But by then MSL will
have risen several metres.
If GMT rises enough for the Greenland ice sheet to melt, then we shall have to contend with
the extra sea-level rise (SLR) due to melting occurring in Antarctica.
Greenland's ice sheet produces 1 billion (1x109) tonnes of 'rock flour' each year
which could be utilised for (limited) carbon capture. [2]