Motivated by low-altitude cusp observations of small-scale (similar to 1 km) field-aligned currents (SSFACs) interpreted as ionospheric Alfven resonator modes, we have investigated the effects of Alfven wave energy deposition on thermospheric upwelling and the formation of air density enhancement... Show moreMotivated by low-altitude cusp observations of small-scale (similar to 1 km) field-aligned currents (SSFACs) interpreted as ionospheric Alfven resonator modes, we have investigated the effects of Alfven wave energy deposition on thermospheric upwelling and the formation of air density enhancements in and near the cusp. Such density enhancements were commonly observed near 400 km altitude by the CHAMP satellite. They are not predicted by empirical thermosphere models, and they are well correlated with the observed SSFACs. A parameterized model for the altitude dependence of the Alfven wave electric field, constrained by CHAMP data, has been developed and embedded in the Joule heating module of the National Center for Atmospheric Research (NCAR) Coupled Magnetosphere-Ionosphere-Thermosphere (CMIT) model. The CMIT model was then used to simulate the geospace response to an interplanetary stream interaction region (SIR) that swept past Earth on 26-27 March 2003. CMIT diagnostics for the thermospheric mass density at 400 km altitude show (1) CMIT without Alfvenic Joule heating usually underestimates CHAMP's orbit-average density; inclusion of Alfvenic heating modestly improves CMIT's orbit-average prediction of the density (by a few %), especially during the more active periods of the SIR event. (2) The improvement in CMIT's instantaneous density prediction with Alfvenic heating included is more significant (up to 15%) in the vicinity of the cusp heating region, a feature that the MSIS empirical thermosphere model misses for this event. Thermospheric density changes of 20-30% caused by the cusp-region Alfvenic heating sporadically populate the polar region through the action of corotation and neutral winds. Show less
