Observations of structured optical emissions and particle precipitation equatorward of the traditional auroral oval

Abstract

[1] High-sensitivity all-sky images from south-central Alaska show the common occurrence of slow-moving, faint optical emissions at 557.7 and 427.8 nm well equatorward of the discrete aurora. These emissions appear over a continuum of forms ranging from homogenous longitudinal bands to bands with irregular structure on their poleward edge to widely distributed arrays of vortex-like curls and widely spaced spots on the order of 10 km in diameter. These forms appear to correspond to various stages in the temporal evolution of nearly corotating precipitation regions populated by particles injected from more distant areas of the magnetosphere and may exhibit morphological control by an instability operating on cold plasma near the plasmapause. Although these phenomena are most common in the evening hours and typically persist for hours at a time, one case demonstrates that the features can remain throughout the night on occasion. These faint optical features appear to be colocated with regions of enhanced background counts in DMSP particle measurements and to be associated with the ring current/outer radiation belt region equatorward of subauroral polarization streams (SAPS). The features can occur in conjunction with HF and MF radio frequency absorption, at levels which are often too low to show up on routine absorption instruments such as the riometer. This has practical implications on the operation and interpretation of ionospheric interaction experiments carried out in the subauroral region.

Steve: The Optical Signature of Intense Subauroral Ion Drifts

“…Pedersen et al (2007) reported feint optical structures as far as 10 • equatorward of the traditional auroral oval. Pedersen et al (2007) reported feint optical structures as far as 10 • equatorward of the traditional auroral oval.…”

Substructures with luminosity modulation and horizontal oscillation in pulsating patch: Principal component analysis application to pulsating aurora

“…[, ]. It was also reported that diffuse aurora appears with a variety of spatial scale structures ∼30 km in width [ Wallis et al , ] and ∼10 km in width [ Pedersen et al , ]. Simultaneous ground‐based optical instruments and Fast Auroral Snapshot Explorer observation demonstrated thin auroral stripes extending along the geomagnetic latitudinal directions with a width of about 5 km in dim background luminosity [ Sergienko et al , ].…”

Fine scale structures of pulsating auroras in the early recovery phase of substorm using ground‐based EMCCD camera

“…Many cases of fine‐scale structures in discrete auroras were demonstrated by both spacecraft investigations and ground‐based observations, such as Alfvenic auroras [ Semeter et al , 2008; Frey et al , 2010] and flickering auroras [ Gustavsson et al , 2008; Whiter et al , 2008, 2010; Yaegashi et al , 2011; Kataoka et al , 2011]. While diffuse auroras have been generally regarded as uniform and not discrete structures, fine scale structures were also reported [e.g., Wallis et al , 1979; Pedersen et al , 2007]. Simultaneous optical instruments on the ground and the FAST electron spectrometer found thin auroral stripes extended along the geomagnetic latitudinal directions with a width of about 5 km in dim background luminosity [ Sergienko et al , 2008].…”