Abstract. It is known that at some critical amplitude both periodic flows in fluids and the drift waves in magnetized plasma become unstable with respect to long-wavelength perturbations. Such secondary instabilities result in the generation of large-scale structures which play a significant role in such important physical phenomena as an enhanced transport and self-organization. In z-pinches, plasma erosion switches, and possibly in tokamaks with an intensive ECR heating the phenomena on small time and space scales when only the electron motions play a role and the ions form an immobile background could be important. In the present report stability analysis of periodic flows and whistler waves with respect to long-wavelength perturbations within the framework of dissipative electron magnetohydrodynamics is presented. Several types of flows (non-helical, isotropic helical, and anisotropic helical) and whistler waves are considered. It is shown that the destabilizing effect on the long-wavelength perturbations is due to either flow anisotropy (the negative resistivity effect) or its helicity.
IAEA 2003