The IPCC defines climate feedback in their glossary as,
Because for Human type CO2 emissions, maximum warming is reached in about 10 years,(
Maximum warming occurs about one decade after a carbon dioxide emission),
I thought it might be possible to evaluate the instrument temperature record to see if the levels of climate feedback exists to meet the requirement for 3°C of warming in response to a doubling of the CO2 level.
For an ECS of 3°C the forcing perturbation of doubling the CO2 level (1.1°C), would require a climate feedback (feedback factor) of 2.72 Times the input perturbation, (1.1 X 2.72 =2.992).
To evaluate this for the entire record, I have the starting date (DATE), The DATE minus 10 years(T1), and the DATE minus 20 years (T2).
I also included the forcing between T1 and the DATE, as 74% of the
NOAA AGGI forcing, using the IPCC's ratio of forcing warming less aerosol cooling.
Output is the DATE -(T1 less forcing)
Input is T1 - T2
Climate feedback is the Output/Input
The average Climate feedback for the years 1880 to 2020 was -.2222,
The average Climate feedback since 1978 was -1.98
The average Climate feedback since 2000 was -5.78
For the forcing I used 5.35 X ln( CO2-eq DATE/CO2-eq T1) X .3 X .74,
The bottom line is that the climate feedback to warming perturbations is mostly negative, and so cannot produce the require long term +2.72 Climate feedback needed for a doubling of the CO2 level
to become a 3°C output. If anything the feedbacks are negative, meaning the warming from the initial warming perturbation is weakened!
Thoughts on improving the evaluation?