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How to Discretize, Disaggregate and … Complexity 27<br />

von der Regendauer", (Berichte aus de Institut für Wasserwirtschaft und<br />

Gesundheits-ingenieurwesen Technische Hochschule München Nr. 2, 1969, ca<br />

200pp.). What conclusion can be drawn from Figure 2.2, other than that c varies<br />

widely and unpredictably with duration? Surely, that the given relationship is<br />

poorly structured, or fuzzy, perhaps even a mess, since, in the absence of a<br />

better explanation of the processes involved, evidently any value is as good as<br />

any other.<br />

Reporting this variance of c in those models that use it has to my knowledge<br />

never been done. It seems to be virtually unknown in the English literature on<br />

the subject. In this sense a simplistic sub-model increases a difficulty when<br />

using the model, because its mathematical formulation is likely incorrect<br />

physically, and evidently meaningful values of the empirical coefficient c<br />

cannot be acceptably fudged. Ideally, the inherent scatter in all sub-models<br />

should be incorporated in the computations in the model, and reported (the<br />

uncertainty can probably be uncovered in the original publications).<br />

Complexity arises when there is a large number of processes, when the<br />

relationships are non-linear, and where there are nonholonomic constraints (e.g.<br />

if a pump station in a drainage system switches on or off without regard to the<br />

system as a whole).<br />

We may think of model complexity C as the sum<br />

where:<br />

C<br />

N<br />

N<br />

N<br />

∑∑ ∑<br />

≡ M S pr<br />

m= 1 s= 1 p = 1<br />

r<br />

Np a<br />

p,<br />

s , m<br />

N m = the number of modules active in the model,<br />

N s = no. of sub-spaces modeled in each module,<br />

N pr = no. of processes modeled in each sub-space,<br />

Np a = no. of input parameters required for each process.<br />

Model complexity is related to the total number of uncertain<br />

input parameters.<br />

C is independent of the number of time steps in the input time series (e.g.<br />

rainfall or inflows) that drives the system model. For instance, a rain time series<br />

may be 100 y long at 1 minute time steps, comprising about 3.15x10 9 time<br />

steps, while the system model itself may have just six elements each requiring<br />

(say) ten parameters to describe their geometry. Such a system model may be<br />

said to have a complexity of 60, a relatively small number, even though the<br />

driving input function is extremely large.<br />

There is another hierarchy of complexity that depends upon how wellknown<br />

the processes are, and how they depend upon earlier levels of<br />

understanding. In this approach, physical systems are the simplest. SWMM

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