Standing Alfvén waves in the magnetosphere are a well-known phenomenon with a long history of research in theory (e.g., Dungey, 1954) and observation (e.g., Sugiura &Wilson, 1964). The waves have been extensively studied with regard to their basic physical properties (e.g., Radoski & Carovillano, 1966), excitation mechanisms (e.g., Chen & Hasegawa, 1974), interaction with particles (e.g., , and relation to the plasma mass density (e.g., Obayashi & Jacobs, 1958). In this study, we address a relatively unexplored property of the waves: the mode structure, that is, the variation of the amplitude and phase of the electric and magnetic field perturbations along the background magnetic field. We pay special attention to the location of the nodes. We focus on toroidal standing Alfvén waves (hereinafter referred to as toroidal waves), which are the most frequently observed class of magnetospheric ultralow frequency (ULF) waves. In space, toroidal waves are recognized as narrowband oscillations in the radial component (E ν ) of the electric field (E) (e.g., Cahill et al., 1986) and the azimuthal component (B ϕ ) of the magnetic field (B) (e.g.,