Large fluctuations of plasma densities in the earth's flank-side magnetoshe
ath (local times 1500-1700) are examined. The characteristics of the fluctu
ations are large amplitudes (Delta N/N similar to 1), long oscillation peri
ods (T similar to 30 m) and anti- correlation between the plasma densities
and magnetic field strengths. The variations of the solar wind plasma densi
ties are negligible, whereas considerable fluctuations are found for the so
lar wind magnetic fields. Two possibilities are considered for the density
fluctuations: 1) repeated traversals of the plasma depletion layer and the
standing slow-mode waves near the magnetopause and 2) convected slow-mode w
aves generated at the earth's bow shock. Temperature anisotropy and density
profile as expected from the repeated traversals are not confirmed with th
e observations. Based on the consideration that the present observations oc
cur in the flanks where plasma flows are largely tangential to the magnetop
ause, we propose that the convected slow-mode waves play a role in the gene
ration of the density fluctuations.