Climate Sensitivity
​Fast and slow feedback sensitivity
​​There is slow responding sensitivity as well as the fast responding 

The 3C metric ​​is based only on fast feedbacks

​​The fast onset feedbacks are the ones that immediately act in response to an increase in atmospheric greenhouse gases (GHGs). They are mainly atmospheric feedbacks in the air, like water vapor, clouds and minute suspended particles (aerosols). Some albedo cooling effect of snow and ice is included. ​

​Water vapor is actually the main GHG because it is so abundant but its global warming effect is mainly a feedback response. Warm air holds more water vapor and that about doubles the warming caused just by a GHG increase.

Slow onset feedbacks are planetary responses to global warming like melting ice sheets and thawing ​​permafrost. Warming wetland peat is a slow feedbacks and melting sub seafloor methane hydrate is considered a very slow feedback.

​​The fast feedback CS is taken to be 3 by the scientists and the slow feedback sensitivity is not used in the assessments- a huge error in underestimating the actual warming that will occur over the long term future. 

​​It was James Hansen who pointed out in a 2008 paper that the true climate sensitivity for the very long term is (6°C), which is double the immediate fast feedback sensitivity (3C) that has been applied by the science since the first IPCC assessment in 1990.

It is the 'true' CS because it is protective of all future generations and life. The fast CS that does not include the large slow feedbacks is not protective. The slow FS is therefore by far the most policy relevant. ​

​​Slow feedbacks take a long time (hence 'slow') in  response to global warming, but they greatly increase over time and are irreversible. They are loss of albedo cooling from ice melting and Arctic carbon feedbacks from warming wetlands and thawing permafrost, that release methane and carbon dioxide.  

There is little point in debating the precise number of the fast CS that is the only CS being used, when we are ignoring all important slow CS. ​​

The debate is because the climate sensitivity fast feedback being used has a very large range, that has actually not changed significantly since 1990.​​​​

"The long term change in surface air temperature following a doubling of carbon dioxide (referred to as the climate sensitivity) is generally used as a benchmark to compare models. The range of results from model studies is 1.9 to 5.2°C... the models results do not justify altering the previously accepted range of 1.5 to 4.5°C. (IPCC WG 1 1990)

​It is likely to be in the range 2°C to 4.5°C with a best estimate of about 3°C, (IPCC WG1 AR4 2007)"

The single fast feedback CS metric(3C) as defined and applied by climate change science ignores the greatest global warming risk which is superheating hothouse Earth  climate change from large Arctic +ve (amplifying) slow feedbacks. 

The metric was originally  fixed to allow for climate change modelling.However in the real world the climate sensitivity is dynamic - with warming it increases as does the risk of abrupt warming.

​​There are wide ranges of uncertainty for all aspects of climate change modeling
(IPCC 2007)​​, and there is a wide range of uncertainty for the fast climate sensitivity that determines the entire assessment of climate change.

.. climate sensitivity only considers the surface mean temperature and gives no indication of the occurrence of abrupt changes or extreme events. Despite its limitations, however, the climate sensitivity remains a useful concept​​..  IPCC AR4 2007 Definition of Climate Sensitivity"

The fact is climate sensitivity is not a linear constant factor (as is assumed in the science), it is dynamic increasing with time and temperature of warming. This is because of the many positive (bad) feedbacks that increase with warming.

    Time-dependent climate sensitivity and the legacy of anthropogenic greenhouse gas emissions, Richard E. Zeebe, August 2013 
    Fast feedbacks
    • water vapour, 
    • surface albedo
    • clouds, ​​
    • aerosols

    NAP 2011 Earth's deep paleo past shows a very high climate sensitivity - up to 7 to 9.6C  3 M years ago (Pliocene).
    July 2019
    ​​​Most complete list. 
    ​Climate feedbacks in the Earth system and prospects for their evaluation

    ​​​​​​The IPCC has always used only a rough mean. For the IPCC AR6 the IPCC rejected the latest model results that put the sensitivity higher, and downgraded it to 3°C again. 

    ​​Here we provide evidence that under higher degrees of warming it will be higher than 3°C (3.8°C), and in any case for consideration of risk a value above 3°C (at least 4°C) has to be used.  

    ​2021 IPCC AR6 ​sensitivity models 
    result is 3.8°C​, but IPCC improperly
    ​pegged it at 3°C, rejecting risk in the entire 
    Double click here to edit this text.
    IPCC AR6 climate sensitivity
    Climate sensitivity is the fundamental single fixed metric determining all projections in the IPCC assessments. It is defined as the equilibrium warming resulting from a doubling of atmospheric CO2. There has always been a wide range of estimates for the value, but the IPCC has only used a single fixed metric, which for long term equilibrium warming runs contrary to climate system science and to risk assessment. The science agrees that higher climate sensitivity (than 3C) is possible. If it is, all the global warming impacts will be earlier and larger (we are already finding this) than projected at 3°C. That risk must be excluded using a higher sensitivity. This was explained by in 2009 by economist Martin Weitzman his paper On modeling and interpreting catastrophic climate change. Catastrophic impacts were mentioned in IPCC 2021 TAR and 2007 AR4, but not since. The IPCC in effect has excluded catastrophic climate change impacts.

    ​​​In addition, the sensitivity will increase with temperature, because of the many amplifying feedback responses to warming. As the planet surface warms large feedbacks come into play. which are all positive (amplifying) the global temperature increase. We already have methane and nitrous oxide that will increase with further warming, making the climate more sensitive. The IPCC excludes these from the projections by not adding extra feedback warming to climate sensitivity based on its warming projections. We know these feedbacks will happen and indeed they have started, but the IPCC acts as if they don't exist. 

    Immediate Emissions Decline
    ​However practically speaking today (2013) the risk of a higher climate sensitivity is just one other reason why global emissions must be put into decline
    immediately and rapidly as IPCC AR6 WG3
    Climate sensitivity in the Anthropocene, M Previdi et al, 2011
    Evidence from Earth's history suggests that slower surface albedo feedbacks due to vegetation change and melting of Greenland and Antarctica can come into play on the timescales of interest to humans, which could increase the sensitivity to significantly higher values, as much as 6 °C. Even higher sensitivity may result as present-day land and ocean carbon sinks begin to lose their ability to sequester anthropogenic CO2 in the coming decades. The evolving view of climate sensitivity in the Anthropocene is therefore one in which a wider array of Earth system feedbacks are recognized as important. Since these feedbacks are overwhelmingly positive, the sensitivity is likely to be higher than has traditionally been assumed.
    There is no one number that is climate sensitivity