Dear Sir David,
The threat of DJT taking over Greenland is a wake-up call for those of us who understand the precarious Arctic situation.
There is a very powerful lobby of businesses and politicians who want the land and sea ice to melt away so that they can exploit resources more easily. They seem wilfully blind (a legal term) to the implications of unabated Arctic meltdown: extremely high risk of catastrophic sea level rise this century.
I drafted an Arctic Emergency Report Card last October, and spent some time investigating the AI response to the text. The AI response was positive but it turns out that AI cannot easily be used as a publicity tool, especially if there's nothing in the public domain. So I have continued waiting for a means of publicising the report.
Now, with a world focus on Greenland, I think there is a window of opportunity, but I would appreciate your support for publication. I've cut my original draft text to focus on Greenland; see below. I could get AI to present a nice executive summary. It needs to be made clear that letting the Greenland Ice Sheet melt continue is risking accelerated disintegration and metres of sea level rise this century
Should we reframe this message as a Greenland Emergency Report Card, and confront those who wish to exploit Greenland regardless of the future? How should we best confront them?
Cheers, John
ARCTIC EMERGENCY REPORT CARD
Draft of 2025/10/26
Introduction
The
Arctic is in a meltdown, which threatens to take at least five tipping
elements beyond their point of no return. Continued meltdown would have
catastrophic consequences which we examine below. Emergency cooling
intervention is vital to prevent any of the tipping elements reaching a point of no return.
The
original cause of this meltdown was global warming caused by an excess
of greenhouse gases in the atmosphere. Global temperature rise has been
amplified in the Arctic, mainly by albedo positive feedback, such that,
since 1980, the mean Arctic temperature has been rising at about four
times the global average. The retreat of sea ice started to accelerate
around 1980, as shown by a comparison with the linear models used by the
IPCC. Satellite images show a corresponding retreat of snow in the
Arctic region. Retreat exposes open water and open ground
respectively. This lowers the albedo causing more heat to be absorbed
and more retreat in a vicious cycle known as albedo positive feedback.
Thus Arctic meltdown is accelerating.
[Snip]
Arctic tipping elements
Since 1980 the Arctic has been warming around four times faster
than the global average. Five elements of the Arctic have been
categorised as tipping elements in the Earth System; see [3] Figure 3:
- the Arctic sea ice;
- the Greenland Ice Sheet;
- the Arctic permafrost, both on land and under the seabed;
- the polar jet stream;
- the Atlantic Meridional Overturning Circulation (AMOC).
The
Arctic sea ice exhibits a switch behaviour. From an initial state of
perennial sea ice, there is accelerated retreat followed by decline
towards a state where there is only seasonal sea ice. This final state
will be reached when all the multiyear ice has gone. This departure
could happen quite suddenly and be a point of no return, meaning the sea
ice cover could not be restored to the perennial sea ice state with
multiyear ice. The Arctic sea ice acts as a vast mirror of many square
kilometres. Complete loss of Arctic ice would contribute 3.3 W/m2 to
global warming besides triggering the other Arctic tipping elements to the point of
no return: a tipping point cascade.
The Greenland Ice Sheet is already
disintegrating. The number of moulins has grown exponentially over the
past 20 years or more. The great glaciers with terminations in the sea
are accelerating towards the sea, as their terminations are warmed from
Atlantic water, derived from the Gulf Stream. Their descent is being
lubricated by the meltwater which flows through the increasing numbers
of moulins. At some point a great glacier is liable to collapse, with
an avalanche of ice blocks racing towards the sea and creating a
megatsunami. Such an avalanche has already occurred for an inland
glacier, causing a 200 metre tsunami oscillating between shores of an
inland lake. There is evidence of past collapses when significant parts
of Greenland suddenly became free of ice, e.g. in the early Holocene. A
complete collapse of the Greenland Ice Sheet would produce enough
meltwater to raise sea level by over 7 metres, risking an even greater
contribution from West Antarctic glaciers, already in a critical state.
[Snip]
Refreezing the Arctic
This is an unprecedented
emergency. Tipping processes are taking the planet towards irreversible
and catastrophic climate change and sea level rise. The Arctic
temperature has to be brought down, long before 4C is reached,
for there to be any chance to prevent the Arctic tipping elements
reaching their "points of no return". In effect the Arctic has to be
refrozen back to some maintainable state, e.g. its state in 1980 before
accelerated meltdown got underway.
Help is at
hand. With powerful cooling intervention using Stratospheric Aerosol
Injection (SAI) it may be possible, not only to lower the Arctic
temperature to around its 1980 temperature but also to reverse climate
change and bring the global temperature back to its 1980 value. The
amount of Arctic warming power is estimated at approximately 2.0 W/m2:
half coming from albedo loss and half from Atlantification. Thus the
cooling power has to be significantly greater than 2.0 W/m2 which
equates to 1.0 petawatt. This has to be directed into the Arctic.
Because most surface water north of 50N flows towards the Arctic,
injection of the aerosol or its precursor can be effective at a latitude
of 50N. The bulk of the aerosol will drift towards the pole, taken by
the Brewer-Dobson circulation, and descend harmlessly into the
troposphere before it reaches the pole. At the megaton injection level,
SO2 is capable of lowering the Arctic temperature, at a cost of a few
tens of thousands of dollars per year [6]. Researchers have been unable
to identify any unmanageable untoward effects; but deployment can be
modelled to anticipate problems even during deployment. The deployment
can be monitored and tuned to avoid any foreseen or unforeseen problems,
thus maximising safety, while maintaining effectiveness.
[snip]
References
[3] Will Steffen et al (2018)
Trajectories of the Earth System in the Anthropocene
[6] Wake Smith et al.
A sub-polar focussed stratospheric aerosol injection deployment scenario