Not exact matches
Just for the sake of illustration, though, here's one
scenario where
higher Holocene variability could go along with lower
climate sensitivity: Suppose that some unknown stabilizing mechanism makes the real world less sensitive to radiative forcing than our current models.
Note that the old GISS model had a
climate sensitivity that was a little
higher (4.2 ºC for a doubling of CO2) than the best estimate (~ 3ºC) and as stated in previous years, the actual forcings that occurred are not the same as those used in the different
scenarios.
My complaint concerns the putative conclusions that the narrator makes concerning
climate sensitivity and the implications for the
high end IPCC
scenarios.
This is presented as a worst - case
scenario — what might be expected to happen if a) nothing is done to curb GHG emissions and b) the
climate sensitivity is in the
higher range Peter Cox and other leading scientists now believe possible.
As stated last year, the
Scenario B in that paper is running a little
high compared with the actual forcings growth (by about 10 %)(and
high compared to A1B), and the old GISS model had a
climate sensitivity that was a little
higher (4.2 ºC for a doubling of CO2) than the best estimate (~ 3ºC).
Just for the sake of illustration, though, here's one
scenario where
higher Holocene variability could go along with lower
climate sensitivity: Suppose that some unknown stabilizing mechanism makes the real world less sensitive to radiative forcing than our current models.
Since 1990, observed sea level has followed the uppermost uncertainty limit of the Intergovernmental Panel on
Climate Change (IPCC) Third Assessment Report (TAR), which was constructed by assuming the highest emission scenario combined with the highest climate sensitivity and adding an ad hoc amount of sea - level rise for «ice sheet uncertainty&raqu
Climate Change (IPCC) Third Assessment Report (TAR), which was constructed by assuming the
highest emission
scenario combined with the
highest climate sensitivity and adding an ad hoc amount of sea - level rise for «ice sheet uncertainty&raqu
climate sensitivity and adding an ad hoc amount of sea - level rise for «ice sheet uncertainty» (1).
Even with a low
climate sensitivity,
high emissions
scenarios will lead to warming exceeding the nominal 2 °C target.
If observations eliminate the possibility that
climate sensitivity is 4 or greater, the low probability /
high damage
scenarios that inflate the societal cost of carbon emissions disappear.
Using the IPCC
climate sensitivity of 3.2 C, the CO2 level by 2100 would need to double by 2100, from today's 392 to 784 ppmv, to reach this warming (the
high side IPCC «
scenario and storyline» A2 is at this level, with estimated warming of 3.4 C above the 1980 - 1999 average, or ~ 3.2 C above today's temperature).
it looks to me from the temperature data that is now in that
Climate sensitivity can not be
higher than the no feedback
scenario, and it could well be less than that.
It appears that the Hansen
Scenario B performed fairly well, with an overestimated trend consistent with its estimate of
climate sensitivity at what is now considered to be toward the
high end of the likely range (although of course, Hansen continues to estimate
climate sensitivity at
higher levels than most other observers).
The «flaw» of low - ECS
climate model studies may not be so much in aerosols, the NASA study suggests, as the effective radiative forcing
scenario (with
high climate sensitivity) is accompanied with relatively low value for aerosol efficacy:
However, from a purely policy standpoint, it is important to consider all possible
scenarios, and a very
high climate sensitivity can not yet be ruled out, as Chris Colose explains (via personal communication):
Figure 3: Global mean temperature measurements (black) and projections based on an IPCC
scenario with
high emissions (A2) for a
climate sensitivity parameter of 5 °C (upper red) and 2 °C (upper blue).