Not exact matches
Observing devices, either within the
region of the dissipative structure or outside of it, may detect regular oscillations caused by variations of components of the structure, or, if their temporal or
spatial resolving power is not high enough for that, they may detect only a new, averaged reading, corresponding to a novel state of affairs brought about by the closure of the set of relationships which
defines the dissipative structure.
We consider the temporal variance to be the statistical variance of the values over intervals of time close to the
defined interval, and the
spatial covariance to be the covariance over
regions close in location, shape, and size to the
defined region.
These subcontinental
spatial units can be chosen to coincide not only with
regions of high observational density but also with
spatial domains
defined by large - scale climate features.
Furthermore, you would also have noticed that by 1500, the
spatial coverage included four of the five
spatial regions defined with the first appearance of data from the fifth
region coming only after 1600.