Page 137 - Modern Spatiotemporal Geostatistics
P. 137

118      Modern Spatiotemporal Geostatistics  —  Chapter  5


             In view  of  the  preceding analysis,  an essential difference between classical
        and  modern  geostatistics  could  be described  as follows:  Unlike  classical  geo-
        statistics  which  essentially capitalized  on  the  techniques of  spatial  statistics,
        the  emphasis of  modern  spatiotemporal  geostatistics  is on  the  powerful  the-
        ories  and  laws  of  natural  sciences.  The  implication  of  this  difference is that
         modern  geostatisticians,  rather than  being  misled by the  numerous  statistical
        models  and  hypotheses compatible with the  data set available, should be able
        to  weed out  the  physically incorrect  models and  hypotheses quickly,  and  get
        on to  the  next  problem with a great  deal  more confidence about  the  maps and
        conclusions  they  have drawn.  This  important  feature of  modern  geostatistics
        is  usually called  strong  inference  in  scientific  reasoning theory.
        EXAMPLE 5.7:  The strong inference situation  described above is a familiar  one
        in science.  Molecular biology,  e.g., was able to  make spectacular progress in a
        rather  short  period of time.  As Platt  (1964) explained in an article published in
        the journal  Science, this extraordinary success was due to  the fact that,  unlike
        traditional  biology  which  was relying  primarily  on taxonomy  (i.e.,  collecting,
        describing,  and  tabulating  observational facts),  molecular  biology  capitalized
        on  the  powerful  theories  of chemistry and the  mathematical modeling  tools  of
        theoretical  physics.

            The  BME  approach aims  at  contributing to  the  continuing  dialogue  be-
        tween  scientific  theories  and  experimental  results.  In  this  sense,  the  BME
        space/time  maps  could  offer valuable  evidence that  a theory  may  need  to  be
        revised  or  reassessed.

        Possible   modifications and    generalizations
        of  the  prior  stage

        The  epistemic  framework of  modern spatiotemporal  geostatistics  is very  gen-
        eral,  thus  allowing  various modifications of  the  BME  approach.  Let  us briefly
        discuss  a few  possibilities.
            The  (p a  functions  of  Equation  5.4  were  assumed  to  be  of  the  form
                                   Otner Vet forms may also be considered, thus
        broadening  the  range of  applicability  of  the  BME  analysis  (the  issue  was al-
        ready  raised in  Chapter 3,  "A  mathematical formulation  of  the  general knowl-
        edge  base,"  p. 74).  In cases where the  general  knowledge consists of  statistical
        moments  (Example  5.1  above),  several  methods  can  be  used  in  place of  en-
        tropy  maximization,  including  series  truncation  and  orthogonal  polynomial
        expansion  (Christakos,  1992).
            When the  univariate prior  pdf is available (considered to  be the same at  all
        points  in space/time),  it  may be assumed that a transformation  of the  original
        random  field  into  a  Gaussian one exists.  Using  the  derived  statistics  of  the
        Gaussian field,  the  approach of  Example 5.1 can then  be applied to  define the
        9^-operator.  Finally, the  operator associated with the  original  field  is obtained
        by the  inverse transformation (Bogaert  et al.,  1999).
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