Coronal holes produce high-speed, low-density, and high-temperature st
reams that propagate into the interplanetary space. These streams inte
ract with the slow-speed, high-density, and low-temperature stream of
the ambient solar wind. We investigate this problem using the time-dep
endent, two-dimensional hydrodynamic model in the spherical-equatorial
coordinate system. More accurate numerical methods and finer differen
ce meshes used enable us to track the evolution of detailed features o
f the fast and slow stream interaction. An analysis of formation of sh
ock pairs (forward and reverse shocks) is presented for both erupting
and corotating parts of fast streams. Further, it is shown that the pr
ocess of interaction of fast and slow solar wind streams may contain r
icher structures. Such structures may originate during the reconfineme
nt process (internal shocks), spatial substructures (flux tubes), and
small temporal modulations (shock wings). They may influence the globa
l shape of stream interfaces and heating of the plasma. Finally, concl
usion can be made that boundaries between the fast and slow coronal st
reams seem to be stable against small random fluctuations and against
small-introduced disturbances and the Kelvin-Helmholtz instability is
not initiated.