Two large depressions in the magnitude of the interplanetary magnetic field
, lasting similar to 10-20 min, have been observed in the solar wind just u
pstream of the Earth's bow shock by three spacecraft (Active Magnetospheric
Particle Tracer Explorer UK Subsatellite (AMPTE UKS), AMPTE Ion Release Mo
dule (IRM), and ISEE 1). The multiple satellite observations show that the
depressions are convecting with the ambient solar wind. Analysis of the dep
ression boundaries shows that they are tangential discontinuities with norm
als aligned approximately parallel to the GSE x direction. The electron dis
tributions measured within the structures are remarkably isotropic when com
pared to the more anisotropic distributions found in the ambient solar wind
. There is also a reduction in plasma wave activity during the depressions.
The depressions exhibit characteristics similar to those of solar wind mag
netic holes but are much larger than has been typically observed. The depre
ssions also display similarities with encounters of the heliospheric plasma
sheet and heat flux dropouts, both of which are typically observed near se
ctor boundaries, close to the heliospheric current sheet. The nature of the
se depressions is discussed in the context of magnetic hole and heliospheri
c plasma sheet observations. A large magnetic hole structure formed from a
conglomeration of small holes appears the more likely scenario for the obse
rved depressions.