Alfvénic turbulence is the turbulent interaction of fluctuations polarized primarily as Alfvén waves. In Elsässer variables , each wave population is nonlinearly distorted by the oppositely propagating population. Equal populations give a balanced cascade; unequal populations give an imbalanced cascade. The absence of one population removes the leading nonlinear interaction in ideal reduced magnetohydrodynamics.
For balanced anisotropic Alfvénic turbulence, suppose and resonant interactions preserve the parallel scale during the perpendicular cascade. Random encounter accumulation gives . Constant energy flux then gives and the displayed perpendicular turbulent energy spectrum. Unlike isotropic phenomenology, the fixed parallel scale is independent of the decreasing perpendicular scale.
In a weak Alfvénic cascade at fixed , grows as the perpendicular scale shrinks. If its outer value is at , it reaches order one at the displayed scale. Beyond it the weak-interaction ordering fails and a critical balance model may become appropriate.
The Iroshnikov-Kraichnan spectrum phenomenology assumes balanced, isotropic local Alfvénic turbulence with , decorrelated counterpropagating encounters, and . A weak wave cascade takes . Constant energy flux gives and the displayed shell-integrated turbulent energy spectrum. Isotropy is an additional assumption, not a consequence of a strong guide field.
Goldreich–Sridhar turbulence combines critical balance, balanced counterpropagating Alfvén waves, a local perpendicular cascade, and constant energy flux per unit mass . With and , one obtains . Defining the one-dimensional perpendicular turbulent energy spectrum by gives . Critical balance also gives . This scaling argument neglects scale-dependent alignment and intermittency corrections, which are additional physical effects rather than consequences of the stated assumptions.
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