The Equator-S satellite was ideally positioned to make magnetic field obser
vations in the dawn-side magnetosheath, relatively close to the magnetopaus
e. The magnetosheath data were particularly rich in compressional signature
s, consistent with mirror mode structures, which occurred during similar to
30% of orbits crossing into the magnetosheath. In most, although not all c
ases, strongly compressive signatures extended up to the magnetopause bound
ary, with no increase in the underlying magnetic field magnitude on the tim
e scale of ten to thirty minutes. The proximity and character of mirror-lik
e fluctuations near the magnetopause suggest that in the dawn-side magnetos
heath the plasma depletion layer (PDL) is of narrower extent than is genera
lly observed closer to the subsolar point, or is absent.