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                9.2    The shape of the Earth and the grid



                The Earth is shaped like a sphere (although it is slightly flattened at the poles).


                The  Earth  moves  around  the  sun

                once a year.




                In one day, the Earth rotates  once

                around itself.

                The rotation goes from west to east.




                                                                         o
                In relation to the sun, the Earth's axis is tilted 23½ .

                This tilt is the cause of the seasonal climatic changes.


                Across the earth, from magnetic pole to magnetic pole, a magnetic field runs.

                This field works broadly like an ordinary bar magnet.

                Note  that  there  are  2  axes,  a  magnetic  and  a  geographic,  and  they  do  not

                coincide.


                We will come back to this.




                9.2.1    Longitude and latitude


                Longitude and latitude are a coordinate system used to determine positions on

                Earth.


                Latitude (north-south) is measured from the equator (0°) up to 90° north or

                south.

                Longitude (east-west) is measured from the prime meridian (0°), which passes

                through Greenwich, and extends up to 180° east or west.


                Together they form a network that makes it possible to find precise geographical

                locations.


             Flyveteori PPL(A)(UL)/LAPL             Henning Andersen, Midtjysk Flyveskole© 2025               803
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