ON THE EQUIVALENCE OF THE COKRIGING AND KRIGING SYSTEMS

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dc.contributor.author Subramanyam A.
dc.contributor.author Pandalai H.S.
dc.date.accessioned 2022-09-23T00:35:23Z
dc.date.available 2022-09-23T00:35:23Z
dc.date.issued 2004
dc.identifier https://elibrary.ru/item.asp?id=6617790
dc.identifier.citation Mathematical Geology, 2004, 36, 4, 507-523
dc.identifier.issn 0882-8121
dc.identifier.uri https://repository.geologyscience.ru/handle/123456789/38702
dc.description.abstract Simple cokriging of components of a p-dimensional second-order stationary random process is considered. Necessary and sufficient conditions under which simple cokriging is equivalent to simple kriging are given. Essentially this condition requires that it should be possible to express the cross-covariance at any lag series h using the cross-covariance at |h|=0 and the auto-covariance at lag series h. The mosaic model, multicolocated kriging and the linear model of coregionalization are examined in this context. A data analytic method to examine whether simple kriging of components of a multivariate random process is equivalent to its cokriging is given
dc.subject COKRIGING
dc.subject KRIGING
dc.subject INTRINSIC COREGIONALIZATION
dc.subject SPATIAL ORTHOGONALITY
dc.subject MOSAIC MODEL
dc.title ON THE EQUIVALENCE OF THE COKRIGING AND KRIGING SYSTEMS
dc.type Статья


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