The OI‐135.6 nm Nighttime Emission in ICON‐FUV Images: A New Tool for the Observation of Classical Medium‐Scale Traveling Ionospheric Disturbances?

Abstract

The National Aeronautics and Space Administration Ionospheric Connection Explorer (ICON) mission will study the close relationship between the ionosphere, the atmospheric weather, and space weather using in situ and remote sensing instruments proving plasma density, temperature, ion drift velocity, and thermospheric wind velocity over the equatorial region. In particular, the far ultraviolet (FUV) instrument will image the terrestrial limb in two wavelength channels. During nighttime, only the channel characterizing the bright 135.6‐nm emission of atomic oxygen will be used. The purpose of this study is to simulate FUV nightglow measurements under quiet as well as disturbed ionospheric conditions. Classical medium‐scale traveling ionospheric disturbances (MSTIDs), which are understood as the ionospheric signature of atmospheric gravity waves, are one of the main sources of ionospheric variability. Here, we simulate their potential appearance in the FUV instrument data. The simulation model produces FUV images used as input to identify and characterize MSTIDs. MSTID propagation parameters can be retrieved under specific geometrical configurations between the FUV lines of sight and propagation direction of the MSTID, which differs depending on the limb or sublimb observing geometry. The largest MSTID signature is expected during equinoxes under solar maximum periods, for MSTID periods of less than 30 min. The weak brightness of the 135.6‐nm multiplet under solar minimum conditions is the main limitation to the MSTID detection on the nightside. Future MSTID detection algorithms would have to cope with very low signal‐to‐noise ratio, in particular during solstices and under solar minimum conditions.

Climatology of Equatorial Plasma Bubbles in Ionospheric Connection Explorer/Far-UltraViolet (ICON/FUV) Limb Images

“…They used 630.0 nm (i.e., red-color) limb images taken by the Imager of Sprites and Upper Atmospheric Lightnings onboard the Formosa Satellite II (Formosat-2). Using numerical simulations, Wautelet et al (2019) investigated possibility of using FUV limb images for MSTID detection. However, the method has not yet been applied to actual observations.…”

A new strategy for ionospheric remote sensing using the 130.4/135.6 nm airglow intensity ratios

“…The pervasive presence of these emissions over the entire globe makes them excellent proxies for remote sensing of the nighttime ionosphere and thermosphere (Meier, 1991;Stephan et al, 2001;DeMajistre et al, 2005;Zhang YL et al, 2006;Dymond, 2009;Zhang YL and Paxton, 2019;Kil et al, 2020;Wang YG et al, 2022). In the past two decades, space-based observations of these two resonant lines, particularly the 135.6 nm emission, have been used as a primary means for global-scale monitoring of the nighttime ionosphere at midto-low latitudes (DeMajistre et al, 2004;Kil et al, 2004;Fu LP et al, 2015;Qin JQ et al, 2015;Qin JQ et al, 2016;Eastes et al, 2017;Kamalabadi et al, 2018;Wautelet et al, 2019;Wautelet et al, 2021). In the literature, extensive works have been dedicated to the development of numerical methods for the retrieval of ionospheric parameters from the absolute intensities of these airglow emissions (Meier, 1991;Dymond et al, 1997;Qin JQ et al, 2015).…”