A spatial-temporal model of the daily mean values of the geomagnetic total
force field was constructed for Japan for the time interval from 1997 to 19
99. The daily mean data of six geomagnetic observatories and nine continuou
s geomagnetic stations in Japan were used for the model. Temporal functions
of the model were constructed using the Natural Orthogonal Components meth
od, and the spatial functions are polynomial functions of the horizontal po
sitions. The accuracy of the model is within approximately a few nT, and it
can be used for eliminating external fields for geomagnetic surveys or det
ecting local geomagnetic changes for monitoring crustal activities. Each fu
nction, which is calculated using the mathematical (statistical) method, ha
s physical meaning, such as the intensity of the globally symmetrical equat
orial ring current and secular changes in the main field. The temporal and
spatial functions can be then used for geophysical study of the Earth.