  We used data from a magnetometer on board the ISS to simulate the Earth's
magnetic field. For that purpose, we generated two models from the data and
compared them: an off-centered dipole model and a centered multipolar model. We
found out that measuring the magnetic field along only two orbits is not enough
to provide a good estimate of the Earth's magnetic field, as they chart a too
small portion of the Earth's surface. This was our original work within the
"Astro Pi Challenge", a project ran by ESA and the Raspberry Pi Foundation, and
the magnetometer used was the one incorporated in the Raspberry Pi Sense Hat.
Here, we improved by performing the same analysis using data from ten orbits
and learned that the multipolar model already provides a good approximation to
the Earth's magnetic field with this number of orbits. We also noticed a
deviation of the data collected from what would be expected from the IGRF
model, in both sets of data.
