Thanks Ron,
This paper is one of the most realistic and down-to-earth I have read recently. It is a step in the right direction. It argues that we need to get the global temperature back below 1.0C, or possibly lower, if we are to prevent catastrophic sea level rise from the polar ice sheets. Our group, PRAG, goes further and argues that the most urgent action is preventing the partial collapse of the Greenland Ice Sheet (GIS), which is in accelerated decline. We want both the Arctic and global temperatures to be brought back to what they were around 1980 or earlier. The abstract of the paper, see below, points out this acceleration: a quadrupling of ice mass loss since the 90s. Though the paper argues for more research, what they are saying seems a very good argument for cooling intervention to lower temperatures. We add specific urgency: the GIS intervention needs to be before things get much worse and the point of no return is reached when even the most powerful cooling intervention is unable to prevent the slide towards collapse and metres of sea level rise. The urgency would justify the ambitious target of five years to ramp up SAI to full strength: where "full strength" means enough cooling power to start lowering the Arctic temperature and reversing the mass loss of the GIS.
BTW, the other four tipping processes in the Arctic might be saved from becoming irreversible by lowering the Arctic temperature; see the Arctic Emergency Report Card in draft.
Cheers, John
Abstract
Mass loss from ice sheets in Greenland and Antarctica has quadrupled
since the 1990s and now represents the dominant source of global mean
sea-level rise from the cryosphere. This has raised concerns about their
future stability and focussed attention on the global mean temperature
thresholds that might trigger more rapid retreat or even collapse, with
renewed calls to meet the more ambitious target of the Paris Climate
Agreement and limit warming to +1.5 °C above pre-industrial. Here we
synthesise multiple lines of evidence to show that +1.5 °C is too high
and that even current climate forcing (+1.2 °C), if sustained, is likely
to generate several metres of sea-level rise over the coming centuries,
causing extensive loss and damage to coastal populations and
challenging the implementation of adaptation measures. To avoid this
requires a global mean temperature that is cooler than present and which
we hypothesise to be closer to +1 °C above pre-industrial, possibly
even lower, but further work is urgently required to more precisely
determine a ‘safe limit’ for ice sheets.