Beam-driven Langmuir turbulence is studied in two moderately moderatel
y magnetized (OMEGA(e) almost-equal-to omega(e)) space-plasma regimes:
regions of the lower solar corona and the Earth's auroral ionosphere.
The turbulence is modeled using modified Zakharov equations, which ar
e employed in two-dimensional numerical simulations. For coronal param
eters, highly anisotropic coherent wave packets form and collapse when
OMEGA(e) < omega(e). By contrast, the turbulence is phase incoherent
when OMEGA(e) > omega(e), as a result of change in the topology of the
Langmuir dispersion relation. In the auroral ionosphere, intense Lang
muir waves (up to 500 mV/m) have been measured, in conjunction with fi
eld-aligned electron streams and nonthermal electron tails. Approximat
e agreement with high-time-resolution electric-field measurements, is
found in the simulations. However, because of strong damping on nonthe
rmal electrons, wave collapse is inhibited, irrespective of the orderi
ng of OMEGA(e) and omega(e).