Coldcall said:
Vanesch,
"I would hope they know what they've put in their computer model. They have not been typing random lines of code, right ?"
Good question. Considering some of the comments in the harry_readme file of the CRU emails one wonders about the quality and validation of the input data for Jones's models. Though no I am not saying their inputs were just random code :-)
Reconstruction of indicators of past climate have nothing to do with climate models.
"So it is not possible that actually used models over the time scale and in the parameter zone they are used, exhibit chaotic behaviour"
I respectfully disagree. The timeframe involved may be arbritray depending on ones definition of a full climate cycle. I believe they speak of 30 years usually (correct me if I am wrong). But even if one uses a shorter timeframe such as 10 years the system will exhibit chaotic behaviour within the first few seconds (depending on how accurately you are measuring the initial conditions and then comparing them to what actually transpired in the real world).
I have no idea what that might mean. A "full climate cycle" must be something that is way longer than the defining time of over how long we have to average weather to even define climate. If that period is 30 years, then 30 years is just ONE single "climate point". The next single point is then 60 years later. In a century, we have about 3 "climate state points" (of course, we will work with moving averages, and we can then interpolate between them to have a continuous curve).
Climate dynamics - strictly speaking - is then the dynamical equation which will have us the first climate point (right now) evolve in the second one (30 years from now) and which will have the second one evolve in the third one (60 years from now).
By definition, you cannot have better time resolution in climate dynamics. A climate cycle must contain many "climate points" and hence must have a period that is several hundreds of years, at least.
Its that difference to reality (unpredictability) which is a symptom of the chaotic behaviour.
Imagine that you have a weather forcast program. You introduce into it, actual initial conditions. You let it compute the weather for the next 20 years. Of course, it will not predict the day-to-day weather accurately after a few days, because of, exactly, that chaotic behaviour of weather. But if you take the
average of that weather over your computed time series, you will find certain average evolutions for temperature, precipitation etc... over the year.
Now, do the same, but start out from different (randomly generated) initial conditions. You will have 20 years of imaginary weather (again). Take the average. Chances are, your average is not very different from your first run.
Do this 1000 times (that is, do 1000 times a 20 - year weather forecast), each time with different initial conditions. Calculate averages each time.
If those "time averages" are more or less comparable, you can say that you have a rather robust climate estimate, independent of the exact initial conditions, right ? So although the exact succession of rain, sunshine, wind and so on will be totally different for those 1000 runs, the averages calculated will maybe be rather comparable. And probably also comparable to the real climate if the weather forecasting program is any good.
Mind you, it could be that each time you get wildly different averages. In that case, your weather forecasting engine doesn't allow you to estimate climate. But if the averages are more or less the same, it does.
This allows you already to estimate (static) climate from a weather forecasting program - even though the weather forecasting itself is chaotic, the statistical properties (the averages) can be well-defined (or not).