From extensive simulation of simple local fluid models of long wavelen
gth drift wave turbulence in tokamaks, it is found that conventional n
otions concerning directions of cascades, locality and isotropy of spe
ctral transfer, frequencies of fluctuations, and stationarity of satur
ation do not hold for moderate to long wavelengths (kp(s) less-than-or
-equal-to 1). In particular, at long wavelengths, where spectral trans
fer of energy is dominated by the E X B nonlinearity, energy is carrie
d to short scale (even in two dimensions) in a manner that is anisotro
pic and highly nonlocal (energy is efficiently passed between modes se
parated by the entire spectrum range in a correlation time). At short
wavelengths, transfer is dominated by the polarization drift nonlinear
ity. While the standard dual cascade applies in this subrange, it is f
ound that finite spectrum size can produce cascades that are reverse d
irected (i.e., energy to high k) and are nonconservative in enstrophy
and energy similarity ranges (but conservative overall). In regions wh
ere both nonlinearities are important, cross-coupling between the nonl
inearities gives rise to large nonlinear frequency shifts which profou
ndly affect the dynamics of saturation by modifying the growth rate an
d nonlinear transfer rates. These modifications produce a nonstationar
y saturated state with large amplitude, long period relaxation oscilla
tions in the energy, spectrum shape, and transport rates. Methods of o
bserving these effects are presented.