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Stephen Tashi said:How are the data points measured? Do you have separate instruments to measure \frac{dC(t)}{dt} and C(t)? Or are you computing \frac{dC(t)}{dt} from differences in the C(t) data?
(I'm wondering why you chose to use regression instead of fitting a curve to the C(t) data.)
First, thanks for all the responses to my original question.
I agree completely that, if one had observations of C(t), where C(t) satisfies dC(t)/dt = -λ C(t), starting from C(0), then you'd simply find the exponential that fitted the observed points.
I tried to include sufficient information to ask my question but I tried to avoid including a load of detail that I thought would simply be tedious and irrelevant to readers.
I am trying to understand a very simple model representing the dynamics of atmospheric concentration of CO2 that someone sent me in a paper they had written. I am trying as a first step to reproduce their work. I think that they have greatly over-estimated the accuracy of the estimate for 1/λ, so I want to be doubly careful with this aspect.
I'm still simplifying things here but I hope this won't result in confusion.
Here are my symbols:
t = time after 1960 (yr)
C(t) = excess atmospheric CO2 over the equilbrium level, at time t (Gt).
Fa(t) = rate of emission of anthropogenic CO2 (Gt/yr)
λ = coefficient relating C(t) and the resulting additional absorption rate over the equilibrium absorption rate. (This assumes linearity and only one sink for CO2, hence a 1st order diff eqtn.)
So I have an equation dC(t)/dt = -λ C(t) + Fa(t) .. .. .. .. (1)
As data, I have:
Values of C(0), C(1),... observed values for excess CO2, derived from data published by the Mauna Loa observatory.
Values of Fa(0),Fa(1),... from published estimates of annual CO2 release from fossil fuel burning and land use change.
If I change equation (1) around, I have dC(t)/dt - Fa(t) = -λ C(t). .. .. .. (2)
Using the approximation dC(t)/dt = [C(t) - C(t-1)]/1 and the estimates for Fa(t), I get 50 (rather scattered) points on the left of (2) and I have 50 points on the right. This gives me my scatter plot. A regression analysis gives me an estimate for λ.
From the estimate for λ, I can compute various things of interest, including T = 1/λ, the time to reach equilibrium, in the hypothetical case of anthopogenic CO2 releases ceasing.
I hope this gives the background and explains why I could not just fit a curve to C(t). If there is a better way of doing things, I'd like to know about it.
Thank you again to all for the comments.