PERIODS OF PLANETARY-WAVES IN GEOMAGNETIC-VARIATIONS

Periods of planetary waves, especially the 10- and 16-day waves, were found in Fourier analyses of 10-year geomagnetic time series from two mid-latitude stations in the northern hemisphere. This suggests that p lanetary waves influence geomagnetic variations. Cross-spectral analys is of magnetic time series from seven stations located at around 50 de grees N at the beginning of 1979, when a 16-day wave occurred in the s tratosphere, also shows a 16-day oscillation. However, study of the ph ases does not reveal the horizontal direction of wave propagation. Fur thermore, the temporal variations of the 16-day oscillation in magneti c time series are presented as dynamic spectra and the results are com pared with global investigations of geopotential height data at 1 hPa (around 48 km) with respect to the 16-day wave for the same time inter val. In some cases this comparison suggests a clear correlation betwee n geomagnetic variations and planetary waves as well as a propagation of the 16-day wave up to the dynamo region (100-170 km).