Not exact matches
These scaling factors
compensate for under - or overestimates of the amplitude of the model
response to forcing that may result from factors such as errors in the model's climate sensitivity, ocean heat uptake efficiency or errors in the imposed external
forcing.
Using this estimate, the value of needed
to produce near zero heat uptake by the oceans is, so internal variability need only contribute about 25 % of the total warming
to fully
compensate for the heat uptake due
to the
forced response.
It seems
to me that depending on the parameters — specifically whether you are beyond the threshold point at which your boy can no longer sufficiently
compensate and maintain homesostasis — there actually is a linear relationship between the
forcing (external temperature) and
response (core body temperature) in humans.
I have, incidentally, found using a multilayer diffusive ocean model that there is a near complete identity in the path of the model surface temperature
response to a step
forcing, for the better part of a century, over a wide range of equilibrium climate sensitivities if effective ocean diffusivity is varied
to compensate.