THE QUIET DAILY VARIATION IN THE TOTAL MAGNETIC-FIELD - GLOBAL CURVES

Most magnetic mapping exercises involve measuring the amplitude, or to tal-field component, of Earth's magnetic field. Removing the time-vary ing part of the field is a task of data reduction, and the most common time variation is the quiet daily variation, S-q. It is thus valuable to have for reference type curves of the quiet daily variation in the total field. To meet this need, global data obtained during the 1965 International Year of the Quiet Sun have been used to derive type curv es describing the S-q variation of the total magnetic field, in additi on to the traditional field components. As for the traditional compone nts, the total-field curves show significant seasonal and latitudinal variability in amplitude and phase. The effect of the equatorial elect rojet is clearly evident. In both hemispheres of the globe there are b ands of reduced amplitude in total-field signal between the equator an d the path of the S-q focus. These bands, here termed the total-field ''doldrums'', persist throughout the year.