Solar eclipses provide an opportunity to study ionospheric dynamics in a way unlike any other. The majority of the sun's direct energy link into Earth's atmosphere is rapidly turned off and on again, and the impact of such a modulation is profound. Anyone who has experienced an eclipse from under the track of totality in person can attest to the dramatic temperature swings that occur from the momentary absence of sunlight. From the perspective of the global atmospheric system, the effects are equally noteworthy. Not only does an eclipse directly affect the thermosphere (Li et al., 2021;McInerney et al., 2018), but the obscuration related reduction in photoioniza tion undoubtedly impacts the ionospheric composition (and therefore dynamics) as well (X. Chen et al., 2021;Dang et al., 2018). As a result of changes to the ionosphere's local total electron content (TEC), currents flowing within the ionosphere should also be modified by an eclipse. However, the exact physical description of how these currents are modified is an unsettled question, particularly in polar regions where data coverage is sparse and eclipses are relatively rare. It is therefore necessary for multi-point observations supported by modeling efforts to advance our understanding of eclipse related effects.Several studies have suggested that ionosphere-thermosphere (IT) dynamics will be altered during an eclipse. One of the main drivers of these modified dynamics (at least at mid to low latitudes) is expected to be changes in the neutral wind structure that create counteracting flows in opposition to the regular wind dynamo (Aa et al., 2020;Choudhary et al., 2011;St.-Maurice et al., 2011). Because of coupling between the ionosphere and thermosphere, the normal evolution of the ionospheric electrojets are likely to be impacted as well by deviations in neutral