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1. KINEMATICS OF MATERIAL POINT

                                                  1.1. Frame of Reference


                            To  determine  of the location of a body in the space  at any time
                  it is necessary to choose frame of reference.
                           Frame of reference is usually understood as body of reference,

                  system of axes closely connected with it and clock (time device).
                         Body of reference is a body referring to which positions of other
                                                                 objects  are  determined.  Any  body
                                                                 can  be  chosen  as  the  body  of

                                                                 reference.  For  example  the  Earth
                                                                 can be the body of reference, where
                                                                 system  of  coordinates  (system  of
                                                          а      axes) are parallels-meridians system

                                                                 (fig.1.1 a)
                                                                    The           meridian            through

                                                                 Greenwich, England (fig.1.1b), also
                                                                 called  the  Prime  Meridian,  was  set
                                                                 at  zero  degrees  of  longitude,  with

                                                          b      other  meridians  being  defined  by
                                                                 the angle at the centre of the Earth
                                                                 between  where  it  and  the  Prime
                                                                 Meridian cross the equator. As there

                                                                 are  360  degrees  in  a  circle,  the
                                                                 meridian on the opposite side of the
                                                                 Earth from Greenwich, forming the

                                                                 other  half  of  a  circle  with  the  one
                                                                 through       Greenwich,          is    180°
                                                                 longitude,  and  the  others  lie

                                                          c      between  0°  and  180°  of  West
                                                                 longitude         in      the       Western
                                   Figure 1.1
                                                                 Hemisphere  (West  of  Greenwich)
                                                                 and  between  0°  and  180°  of  East
                                                                 longitude         in       the       Eastern
                  Hemisphere    (East  of  Greenwich).  Most  maps  show  the  lines  of
                  longitude. So, if you are in Greenwich you can be at the very same time

                  in Western Hemisphere and Eastern Hemisphere as shown in fig.1.1 c.





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