The gravest threat we foresee starts with surface melt on West
Antarctica and interaction among positive feedbacks leading to
catastrophic ice loss...
West Antarctica seems to be moving into a mode of significant mass loss (Thomas et al. 2004). ...We find it
implausible that BAU [business as usual] scenarios, with climate forcing and global warming
exceeding those of the Pliocene, would permit a West Antarctic ice
sheet of present size to survive even for a century.
Our concern that BAU GHG [greenhouse gas] scenarios would cause large sea-level rise this century (Hansen 2005) differs from estimates of IPCC (2001, 2007),
which foresees little or no contribution to twenty-first century
sea-level rise from Greenland and Antarctica. However, the IPCC
analyses and projections do not well account for the nonlinear physics
of wet ice sheet disintegration, ice streams and eroding ice shelves,
nor are they consistent with the palaeoclimate evidence we have
presented for the absence of discernable lag between ice sheet forcing
and sea-level rise.
The best chance for averting ice sheet disintegration seems to be intense simultaneous efforts to reduce both CO2 emissions and non-CO2
climate forcings. As mentioned above, there are multiple benefits from
such actions. However, even with such actions, it is probable that the
dangerous level of atmospheric GHGs will be passed, at least
temporarily. We have presented evidence (Hansen et al. 2006b) that the dangerous level of CO2
can be no more than approximately 450ppm. Our present discussion,
including the conclusion that slow feedbacks (ice, vegetation and GHG)
can come into play on century time-scales or sooner, makes it probable
that the dangerous level is even lower.
Present knowledge does not permit accurate
specification of the dangerous level of human-made GHGs. However, it is
much lower than has commonly been assumed. If we have not already
passed the dangerous level, the energy infrastructure in place ensures
that we will pass it within several decades.
We conclude that a feasible strategy for planetary rescue almost surely requires a means of extracting GHGs from the air.
Development of CO2 capture at power plants, with below-ground CO2 sequestration, may be a critical element. Injection of the CO2 well beneath the ocean floor assures its stability (House et al. 2006). If the power plant fuel is derived from biomass, such as cellulosic fibres5 grown without excessive fertilization that produces N2O or other offsetting GHG emissions, it will provide continuing drawdown of atmospheric CO2.