Gbm. Heuvelink, UNCERTAINTY ANALYSIS IN ENVIRONMENTAL MODELING UNDER A CHANGE OF SPATIAL SCALE, Nutrient cycling in agroecosystems, 50(1-3), 1998, pp. 255-264
Although environmental processes at large scales are to a great degree
the resultant of processes at smaller scales, models representing the
se processes can vary considerably from scale to scale. There are thre
e main reasons for this. Firstly, different processes dominate at diff
erent scales, and so different processes are ignored in the simplifica
tion step of the model development. Secondly, input data are often abs
ent or of a much lower quality at larger scales, which results in a te
ndency to use simpler, empirical models at the larger scale. Third, th
e support of the inputs and outputs of a model changes with change of
scale, and this affects the relationships between them. Given these re
asons for using different models at different scales, application of a
model developed at a specific scale to a larger scale should be treat
ed with care. Instead, models should be modified to suit the larger sc
ale, and for this purpose uncertainty analyses can be extremely helpfu
l. If upscaling disturbed the balance between the contributions of inp
ut and model error to the output error, then an uncertainty analysis w
ill show this. Uncertainty analysis will also show how to restore the
balance. In practice, application of uncertainty analysis is severely
hampered by difficulties in the assessment of input and model error. K
nowledge of the short distance spatial variability is of paramount imp
ortance to input error assessment with a change of support, but curren
t geographical databases rarely convey this type of information. Model
error can only be estimated reliably by validation, but this is not e
asy because the support of model predictions and validation measuremen
ts is usually not the same.