Voyager 2 solar wind speeds show unusual variations beginning on day 4
0 of 1996. These variations are oscillations of approximately 30 km/s
with periods of about two days and are unlike any variations heretofor
e detected in the outer heliosphere. Several possible sources of this
behavior are examined. First, this speed feature may be due to a Kelvi
n-Helmholtz instability on the boundary between the slow equatorial an
d fast high-latitude flows, although this instability has not been obs
erved at other radial distances and latitudes. A second possibility is
that these waves are due to instabilities associated with interstella
r pick-up ions; at the similar to 48 AU distance where these oscillati
ons are observed, the pick-up pressure far exceeds the pressure of the
thermal solar wind proton population. A third possibility is that the
waves are an upstream signature of the termination shock, similar to
waves observed upstream of planetary bow shocks. Anomalous cosmic ray
protons with 100 MeV energies satisfy the necessary cyclotron resonanc
e conditions and carry sufficient energy density to produce the observ
ed waves. This possibility would require magnetic connection to the sh
ock and the presence of streaming anomalous cosmic ray ions. Plasma da
ta alone cannot determine whether the necessary conditions for any of
these possibilities exist. Further progress requires collaborative stu
dies using all of the available particle and field data from Voyager 2
.