Page 33 - Modern Spatiotemporal Geostatistics
P. 33

14      Modern  Spatiotemporal Geostatistics —  Chapter  1

         •  Spatiotemporal  random  field  modeling:  The natural  variable of  interest  is
         represented  in  terms  of  a  Spatiotemporal  random  field,  which  offers  a  gen-
        eral  framework  for  analyzing  data  distributed  in  space/time.  This  framework
        is especially effective  mathematically;  it  allows us to  grasp difficult  problems,
        improve  our  insight  into the  physical mechanisms and, thus,  enhance our  pre-
        dictive  capabilities.
        •  Physical  knowledge classification:  The two primary physical knowledge bases
        considered  in  Spatiotemporal  analysis  and  mapping  are  general  knowledge
        (obtained  from  theories,  physical  laws,  summary  statistics,  etc.)  and  speci-
        ficatory  knowledge  (obtained  through  experience with the specific situation).
        •  Epistemic  paradigm:  Modern  Spatiotemporal  geostatistics  is underpinned
        by a cogent  epistemic  foundation  which  combines the  world  of  empirical data
        with  the  world  of  theory  and scientific  reasoning.  This is a powerful  combina-
        tion that  leads to  a distinctive  methodology  for the acquisition,  interpretation,
        integration, and  processing of  physical knowledge.
            The  course of  each  one  of  these three  topical  'elements  is  substantially
        influenced  by each  of the  others,  to  the  extent  that  they  form  a net  or  web of
        theoretical  and empirical  support  for  modern geostatistics,  rather  than  simply
        converging  upon  it.

        Why     Modern     Geostatistics?

        The  discussion  of  the  previous section  was partially  motivated  by the  follow-
        ing  question:  Why  should the  data  analysis community  bother  with  modern
        Spatiotemporal  geostatistics  when there  exist  already  other  alternatives  which
        are  fully  developed,  such  as regression  methods,  spline functions,  basis  func-
        tions,  and trend  surface techniques? The  answer  to  this  question  seems to  be
        threefold:
            1.  A  general answer is a matter  of  scientific  progress:  many of  the  above
        techniques—which  have  been  used  for  several  decades—have  reached  their
        limits,  and  it  is time  that  novel  methods  be tried  in  Spatiotemporal  mapping
        applications.  In fact, this development  in the  field  of  geostatistics  is the  nat-
        ural  course  of  all  human constructions:  the time comes when their  limits are
        recognized and  new methods  need to  be devised.  The  latter  is a necessary step
        for  the  continuing vitality  of  a scientific  field,  and geostatistics  should  not  be
        an  exception.
            2.  Another  answer  to  the  above question  is that the  case for  the  existing
        methods  would  be  logically  much  stronger  if  one  could  show  that  all  the
        alternatives  are  less good  or  even inadequate.  This  is an  important  reason  for
        examining  other  possibilities.
            3.  Finally,  a  more specific  answer  is that  many  of  the  existing  methods
        suffer from  a number  of well-documented  limitations  which  modern  geostatis-
        tics  makes a serious effort  to  eliminate.  We  have  already  mentioned  some  of
        these limitations.  Due to its importance, the matter  deserves further discussion,
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