Constancy of parametervalues in high aggegated sys tems
Posted: Sat Apr 22, 1995 4:12 pm
About constancy of parameters in high aggregated system-models.
I would like to have the opinion of other system-dynamicist about the
following problem:
Let in an economic dynamic feed-back model the relationship between demand
and price for one individual be:
demand=constant*(price**pelasticity)*(income**ielasticity) [1]
in which pelasticity has a negative and ielasticity a positive value
The relation for a population of 1000 individuals then will be:
demand=1000*constant*(price**pelasticity)*(income**ielasticity) [2]
This however is only true if all 1000 individuals react in the same way.
If their income is different (may be they are distributed log-normal over
income, are there any arguments for particular types of distribution and for
constancy of a particular type?), then the magnitude of the dependency of
demand on price is smaller than the parameter pelasticity in relation [2]
suggests. For a "same" price works out differently for individuals with a low
and for individuals with a high income. Actually the parameter "eplasticity"
is dependent on the income-distribution of the population. However as the
income-distribution itself is dependent on the demand (because of self-
selection processes within the population), the parameter "pelasticity" must
be a variable. (And the same will be true for all the other parameters which
are dependent on distributions of variables around their mean values. The
question is: are there any general laws (a priori principles) describing the
relations between the "dynamics over time" and the "distribution around the
mean" in a dynamic system, or are those relations different and unique for
all different systems and is the only option to simulate the relation between
diachronic and synchronic variation by means of models at the lowest levels
of aggregation? Can high aggregated models of complex systems theoretically,
empirically or pragmatically be valid?
To make a reliable model of (a problem in) a system the suggestion is that
one has two options:
1. Make a very big detailed model at the lowest possible aggregation-level
(individual level)
2. Make a smaller summary-model for aggregated individuals in which the
constant parametervalues are replaced by variables. These "variable
parameters" are dependent on the over time changing distributions of
variables. Those distributions have to be included as "level-variables"
(state variables) into the model. However to determine the changing
magnitudes of relationships over time in model [2] one needs the simulation-
results of model [1]. How to get confidence in a high aggregated model
without the help of a low aggregated model ?
Are summary models only valid for physical and chemical systems, a little bit
for population-dynamical systems, still less for ecological systems and not
at all for social systems ?
Geert Nijland, Wageningen University, Dep. Ecological Agriculture.
Mail: Geert Nijland@users@ECO.WAU.NL
I would like to have the opinion of other system-dynamicist about the
following problem:
Let in an economic dynamic feed-back model the relationship between demand
and price for one individual be:
demand=constant*(price**pelasticity)*(income**ielasticity) [1]
in which pelasticity has a negative and ielasticity a positive value
The relation for a population of 1000 individuals then will be:
demand=1000*constant*(price**pelasticity)*(income**ielasticity) [2]
This however is only true if all 1000 individuals react in the same way.
If their income is different (may be they are distributed log-normal over
income, are there any arguments for particular types of distribution and for
constancy of a particular type?), then the magnitude of the dependency of
demand on price is smaller than the parameter pelasticity in relation [2]
suggests. For a "same" price works out differently for individuals with a low
and for individuals with a high income. Actually the parameter "eplasticity"
is dependent on the income-distribution of the population. However as the
income-distribution itself is dependent on the demand (because of self-
selection processes within the population), the parameter "pelasticity" must
be a variable. (And the same will be true for all the other parameters which
are dependent on distributions of variables around their mean values. The
question is: are there any general laws (a priori principles) describing the
relations between the "dynamics over time" and the "distribution around the
mean" in a dynamic system, or are those relations different and unique for
all different systems and is the only option to simulate the relation between
diachronic and synchronic variation by means of models at the lowest levels
of aggregation? Can high aggregated models of complex systems theoretically,
empirically or pragmatically be valid?
To make a reliable model of (a problem in) a system the suggestion is that
one has two options:
1. Make a very big detailed model at the lowest possible aggregation-level
(individual level)
2. Make a smaller summary-model for aggregated individuals in which the
constant parametervalues are replaced by variables. These "variable
parameters" are dependent on the over time changing distributions of
variables. Those distributions have to be included as "level-variables"
(state variables) into the model. However to determine the changing
magnitudes of relationships over time in model [2] one needs the simulation-
results of model [1]. How to get confidence in a high aggregated model
without the help of a low aggregated model ?
Are summary models only valid for physical and chemical systems, a little bit
for population-dynamical systems, still less for ecological systems and not
at all for social systems ?
Geert Nijland, Wageningen University, Dep. Ecological Agriculture.
Mail: Geert Nijland@users@ECO.WAU.NL