The team stresses that even a little warming could cause
irreversible melting of ice sheets and turn dense Amazon forests into dry savannah grassland.
Not exact matches
This
ice sheet is losing mass at a rather larger rate (around 220 cubic kilometres per year) and it will take only another 1 - 2 oC world warming to raise the summer
melt zone to the top
of the Greenland
ice pack after which point, in my understanding, the
ice sheet will go into
irreversible melt.
Many important questions
of environmental policy, however, involve inescapably uncertain outcomes... How much global warming will it take to trigger the
irreversible collapse and
melting of the Greenland
ice sheet?»
Will we reach the point where the
melting of the Greenland
ice sheet is
irreversible?
The
melting of Greenland and the retreat
of Antarctic
ice sheets were proceeding faster than experts had expected and now looked
irreversible.
At that level, the world risked initiating feedbacks in the climate system, such as the
melting of ice sheet area, that could trigger
irreversible warming out
of humanity's control.
How such a warming would impact the probability
of irreversible changes to elements
of the climate system (
melting ice sheets, reversal or slowing
of ocean currents, release
of carbon in permafrost) is unknown.
But in Bamber's second calculation the relatively sophisticated energy balance model, which he believes better represents
ice sheet behaviour, gave a threshold
of 8 degrees for
irreversible melting of Greenland — double the previously published threshold.
But in Bamber's second calculation the relatively sophisticated energy balance model, which he believes better represents
ice sheet behaviour, gave a threshold
of 8 degrees for
irreversible melting of Greenland - double the previously published threshold.
So scientists are keen to know at what temperature
melting of the
ice sheet is likely to become
irreversible.
A 550 world dramatically increases the likelihood
of catastrophes and runaway climate change, such as an
irreversible melting of the Greenland
ice sheet resulting in sea - level rise
of 7 metres.
This could prevent catastrophic,
irreversible tipping points such as the
melting of Arctic sea
ice and the Greenland
ice sheet, and buy time for implementation
of critical strategies to cut long - lived greenhouse gas emissions.
For example, the weakening
of the THC under 1 degree
of warming, a risk
of collapse for 3 degrees, risk
of irreversible melting of the Greenland
Ice sheet at 2 degrees warming, sea level changes
of 5 — 12 meters over several centuries, — these eventualities are debatable, and should certainly be viewed as the «adverse tail»
of possible impacts.