Page 61 - Modern Spatiotemporal Geostatistics
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42       Modern  Spatiotemporal  Geostatistics  —  Chapter  2














        Figure  2.10.  An  illustration  of the  geodesies coordinate system.

        (e.g.,  toroidal  coordinates  are such that  the  equation  of  a  magnetic-field  line
        is that  of  a straight  line  in  these  coordinates).  This  section  concludes with a
        postulate  that  summarizes  an  important  conclusion  from  our  examination  of
        spatiotemporal  analysis thus  far  and foreshadows results to  be obtained  in  the
        following sections.
        POSTULATE     2.6:  The  geostatistician  should  choose a  coordinate  sys-
        tem  (Euclidean  or non-Euclidean)  that  provides a  physically  meaningful
        representation  of  the  situation  and  works as simply  as  possible.
            In  other  words,  in  many geostatistical  applications, the  physical  interpre-
        tation of the subject  matter  (i.e.,  "In what  physical situations  do we use which
        system  of  coordinates?")  may  be equally as important  as the  computational
        convenience  resulting  from  a  particular  choice of the  coordinate  system.

        Metrical     Structure

        Central  among  the  quantitative  features  of  a  spatiotemporal  geometry  is  its
        metrical  structure,  that  is, a set of  mathematical  expressions that  define dis-
        tances.  Metrical  properties  (or  distance  relations)  must  be  "added"  once we
        have  a set  of  points  in  space/time;  the  same  set of  points  may be  compatible
        with  many metrical  properties.
        DEFINITION   2.5:  A  spatiotemporal  metric  is a  function  defined  for a
        coordinate  system  such  that  the  spatiotemporal  distance  between  any
        two  points  in that  system  is determined  from  their  coordinates.

            Distance  expressions cannot  always  be  defined  unambiguously.  The  ex-
        pression for  the  metric  of any continuum  is dependent  on two  entirely  different
        factors:  (i.)  a  "relative"  factor—the particular  coordinate  system;  and (ii.) an
         "absolute"  factor—the  nature  of  the  continuum  itself  (whether  it  forms  a
        plane,  a  sphere,  or  an  ellipsoid;  the  physical  laws  governing  the  natural  vari-
        ables occurring  within the continuum,  etc.).
            In  modern  spatiotemporal  geostatistics,  it  is  usually convenient  to  con-
        sider  two  prime  metrical  structures:  one is the  separate metrical  structure  and
        the  other  is  the  composite  metrical  structure.  Both  metrical  structures  are
        discussed  below  in considerable detail.
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