The interplanetary magnetic field (IMF) orientation controls foreshock
densities and modulates the fraction of the solar wind dynamic pressu
re applied to the magnetosphere. Such pressure variations produce bow
shock and magnetopause motion and cause the radial. profiles for vario
us magnetosheath parameters to sweep inward and outward past nearly st
ationary satellites. We report ISEE 2 observations of correlated densi
ty and speed fluctuations, and anticorrelated density and temperature
fluctuations, on an outbound pass through the northern dawnside magnet
osheath. Densities decreased when the magnetic field rotated southward
and draped about the magnetopause. In the absence of any significant
solar wind density or dynamic pressure variations, we interpret the ma
gnetosheath fluctuations as evidence for radial magnetosheath motion i
nduced by variations in the IMF orientation.