My question is whether this number is substantially different when arrived at by
averaging climate sensitivity over a 3D surface or calculating climate sensitivity for a 1D average surface.
So again, we see that there is no way to assign
an average climate sensitivity.
As a result,
the average climate sensitivity rises.
The overall results of these calcs gives
an average climate sensitivity of about 2 degrees.
Most of these sensitivities are a good 40 % below
the average climate sensitivity of the models used by the U.N.'s Intergovernmental Panel on Climate Change (IPCC).
Not exact matches
This new research takes away the lower end of
climate sensitivity estimates, meaning that global
average temperatures will increase by 3 °C to 5 °C with a doubling of carbon dioxide.»
The metric they have developed, the Vegetation
Sensitivity Index (VSI), allows a more quantifiable response to
climate change challenges and how sensitive different ecosystems are to short - term
climate anomalies; e.g. a warmer June than on
average, a cold December, a cloudy September, etc..
Where «dT» is the change in the Earth's
average surface temperature, «λ» is the
climate sensitivity, usually with units in Kelvin or degrees Celsius per Watts per square meter (°C / [W - m - 2]-RRB-, and «dF» is the radiative forcing.
Where «dT» is the change in the Earth's
average surface temperature, «λ» is the
climate sensitivity, usually with units in Kelvin or degrees Celsius per Watts per square meter (°C / [W m - 2]-RRB-, and «dF» is the radiative forcing, which is discussed in further detail in the Advanced rebuttal to the «CO2 effect is weak» argument.
Climate sensitivity, in the context of this post, refers to a globally
averaged quantity.
With an
average body temperature of 102 degrees Fahrenheit, cats living in cooler
climates must compensate for their temperature -
sensitivity.
The addition says many
climate models typically look at short term, rapid factors when calculating the Earth's
climate sensitivity, which is defined as the
average global temperature increase brought about by a doubling of CO2 in the atmosphere.
The 100 % anthropogenic attribution from
climate models is derived from
climate models that have an
average equilibrium
climate sensitivity (ECS) around 3C.
CONCLUSION The values for the global
climate sensitivity published by the IPCC cover a range from 2.1 ̊C — 4.4 ̊C with an
average value of 3.2 ̊C, which is seven times larger than that predicted here.
Nonetheless, there is a tendency for similar equilibrium
climate sensitivity ECS, especially using a Charney ECS defined as equilibrium global time
average surface temperature change per unit tropopause - level forcing with stratospheric adjustment, for different types of forcings (CO2, CH4, solar) if the forcings are not too idiosyncratic.
The efficacy of a forcing is the
climate sensitivity (in terms of global
average surface temperature change per unit global
average RF) of that forcing relative to a standard type of forcing.
(PS we are considering the
climate sensitivity to be in terms of changes in global - time
average surface temperature per unit global - time
average radiative forcing, though one could also define other
sensitivities for other measures of
climate).
There, they define
climate sensitivity as how strong an effect doubling CO2 will have on
average global temperature.
That would be the General Fluid Dynamics Laboratory which produced the lower «
climate sensitivity» range, (Manabe) which was «
averaged» with the much higher GISS estimate to produce a high end estimate that was assumed to be real science, when it was actually an
average of WAGs.
Figure 1: If
climate skeptics are right about
climate sensitivity (green), then global
average temperature increases will be more moderate this century, shown here for RCP6 (left) and RCP8.5 (right).
For present
climate to show a Gavin / Hansen / IPCC
sensitivity of 0.75 C / Wm ^ -2, an increase of 3.5-fold over the net
average, one must infer that
climate became increasingly sensitive to forcing as «G» has increased.
(ppm) Year of Peak Emissions Percent Change in global emissions Global
average temperature increase above pre-industrial at equilibrium, using «best estimate»
climate sensitivity CO 2 concentration at stabilization (2010 = 388 ppm) CO 2 - eq.
The equilibrium
climate sensitivity refers to the equilibrium change in
average global surface air temperature following a unit change in the radiative forcing.
If
climate skeptics are right about
climate sensitivity (green), then global
average temperature increases will be more moderate this century, shown here for RCP6 (left) and RCP8.5 (right).
The right - hand panel shows ranges of global
average temperature change above pre-industrial, using (i) «best estimate»
climate sensitivity of 3 °C (black line in middle of shaded area), (ii) upper bound of likely range of
climate sensitivity of 4.5 °C (red line at top of shaded area)(iii) lower bound of likely range of
climate sensitivity of 2 °C (blue line at bottom of shaded area).
As it happens, for any value of time constant /
sensitivity value for the «
climate lump» there is a specific phase lag that I will expect between the time of maximum
average solar radiance for the planet to the time of minimum.
Figure 3 shows the same records, with the addition of the results from the
average models from the Forster study, the results that the models were calculated to have on
average, and the results if we assume a
climate sensitivity of 3.0 W / m2 per doubling of CO2.
Each SCC estimate is the
average of numerous iterations (10,000 in the EPA's assessment, which we reproduce here) of the model using different potential values for
climate sensitivity (how much warming a doubling of CO2 will generate).
In other words, these are 3D global simulations from which globally
averaged TOA fluxes and temperatures are determined, which are then used to determine the
climate sensitivity.
So what happens if we calculate dT, dN, and dF at every gridpoint of the model, use that to solve for
climate sensitivity and then take the
average to have a global
climate sensitivity number?
So
climate sensitivity varies... which means, of course, that the constant «temperature
sensitivity» that they claim exists must be an
average temperature
sensitivity.
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).
Where «dT» is the change in the Earth's
average surface temperature, «λ» is the
climate sensitivity, usually with units in Kelvin or degrees Celsius per Watts per square meter (°C / [W / m2]-RRB-, and «dF» is the radiative forcing.
Climate sensitivity is defined in terms of global
averages (there is only one number) but a GCM is fully time - dependent, three - dimensional simulation that typically includes atmospheric and ocean processes.
If the two methods do lead to different estimates of
climate sensitivity, I find it difficult to believe that the 1D model is more appropriate than 3D to making claims about how much the real
average temperature will rise due to a given influence.
In that paper they use the 1D model to calculate
climate sensitivity from
averages of CIMP5 output.
If
climate sensitivity is a variable and not a constant what can we really learn from paleo data other than what the
climate sensitivity was, on
average, over an extended period of time?
In the same way,
climate sensitivity is a long - term measure... but it is the
average of the short term measurements.
«all of the coupled
climate models used in the IPCC AR4 reproduce the time series for the 20th century of globally
averaged surface temperature anomalies; yet they have different feedbacks and
sensitivities and produce markedly different simulations of the 21st century
climate.»
Judith How will we handle «
climate sensitivity» to «global warming» when global
average temperatures start coolingwhile CO2 continues to increase?
If you set goals in terms of global
average temperature, then you need to feed that through the uncertainty of
climate sensitivity to get the concentration of greenhouse gases — not just carbon dioxide, but the whole range of greenhouse gases.
On current trends, the IPCC finds, emissions will continue to soar and global
average temperatures will rise between 2.5 and 7.8 degrees Celsius before the century is out, depending on the pace of economic growth and the
sensitivity of the
climate system to CO2.
That's right, the latest
climate science (some 10 studies published in just the past 3 years) indicates that the earth's
climate sensitivity — that is, how much the global
average surface temperature will rise as a result of greenhouse gases emitted from human activities — is some 33 percent less than scientists thought at the time of the last IPCC Assessment, published in 2007.
The United Nations» Intergovernmental Panel on
Climate Change, a global effort involving hundreds of climate scientists and the governments of 100 nations, projected in 2001 that, depending on the rate of greenhouse gas emissions and general climate sensitivities, the global average temperature would rise 2.5 to 10.4 degrees Fahrenheit between 1990 an
Climate Change, a global effort involving hundreds of
climate scientists and the governments of 100 nations, projected in 2001 that, depending on the rate of greenhouse gas emissions and general climate sensitivities, the global average temperature would rise 2.5 to 10.4 degrees Fahrenheit between 1990 an
climate scientists and the governments of 100 nations, projected in 2001 that, depending on the rate of greenhouse gas emissions and general
climate sensitivities, the global average temperature would rise 2.5 to 10.4 degrees Fahrenheit between 1990 an
climate sensitivities, the global
average temperature would rise 2.5 to 10.4 degrees Fahrenheit between 1990 and 2100.
If we have the
climate sensitivity right and
AVERAGE temperatures increase by the amount predicted it is not a case of your temperatures going up by that much.
The fact that the CMIP simulations ensemble mean can reproduce the 1970 — 2010 US SW temperature increase without inclusion of the AMO (the AMO is treated as an intrinsic natural
climate vari - ability that is
averaged out by taking an ensemble mean of individual simulations) suggests that the CMIP5 models» predicted US SW temperature
sensitivity to the GHG has been significantly (by about a factor of two) overestimated.
Also, perhaps a more open - ended question would be what does he think the
average sceptic MEANS when they say «I am sceptical about AGW, or CAGW, or the consensus position on
climate sensitivity, or IPCC statements, or the possibility of mitigation...»
Our DOE Comment focuses entirely on the new science concerning the equilibrium
climate sensitivity, that is, how much the earth's
average surface temperature will increase from a doubling of the atmospheric carbon dioxide content.
«The fact that the CMIP simulations ensemble mean can reproduce the 1970 — 2010 US SW temperature increase without inclusion of the AMO (the AMO is treated as an intrinsic natural
climate variability that is
averaged out by taking an ensemble mean of individual simulations) suggests that the CMIP5 models» predicted US SW temperature
sensitivity to the GHG has been significantly (by about a factor of two) overestimated.»
By the way Kramm has recently shown that if the
climate sensitivity to 2x CO2 is as small as your value then it can not be discerned within the error of calculating any
average annual temperature and if something can't be observed then I wonder about its existence