Abstract

AbstractWe explore the characteristics, controlling parameters, and relationships of multiscale field‐aligned currents (FACs) using a rigorous, comprehensive, and cross‐platform analysis. Our unique approach combines FAC data from the Swarm satellites and the Advanced Magnetosphere and Planetary Electrodynamics Response Experiment (AMPERE) to create a database of small‐scale (∼10–150 km, <1° latitudinal width), mesoscale (∼150–250 km, 1–2° latitudinal width), and large‐scale (>250 km) FACs. We examine these data for the repeatable behavior of FACs across scales (i.e., the characteristics), the dependence on the interplanetary magnetic field orientation, and the degree to which each scale “departs” from nominal large‐scale specification. We retrieve new information by utilizing magnetic latitude and local time dependence, correlation analyses, and quantification of the departure of smaller from larger scales. We find that (1) FACs characteristics and dependence on controlling parameters do not map between scales in a straight forward manner, (2) relationships between FAC scales exhibit local time dependence, and (3) the dayside high‐latitude region is characterized by remarkably distinct FAC behavior when analyzed at different scales, and the locations of distinction correspond to “anomalous” ionosphere‐thermosphere behavior. Comparing with nominal large‐scale FACs, we find that differences are characterized by a horseshoe shape, maximizing across dayside local times, and that difference magnitudes increase when smaller‐scale observed FACs are considered. We suggest that both new physics and increased resolution of models are required to address the multiscale complexities. We include a summary table of our findings to provide a quick reference for differences between multiscale FACs.

Highlights

  • Field-aligned currents (FACs), or the system of currents flowing along Earth’s magnetic field lines, are the dominant form of energy and momentum exchange between the magnetosphere and ionosphere and are critical to understanding the entire solar wind to magnetosphere-ionosphere-thermosphere (MIT) coupling

  • We find that the C2012 R1/R2 field-aligned currents (FACs) accurately capture the large-scale FAC observations (low median absolute deviation (MAD) are recorded at dawn and dusk for Swarm A 350 km scale and AMPERE)

  • Our results suggest that small-scale and mesoscale FACs likely play a significant role in critical geospace phenomena in these magnetic local time (MLT)

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Summary

Introduction

Field-aligned currents (FACs), or the system of currents flowing along Earth’s magnetic field lines, are the dominant form of energy and momentum exchange between the magnetosphere and ionosphere and are critical to understanding the entire solar wind to magnetosphere-ionosphere-thermosphere (MIT) coupling. The existence of such a system of currents electrodynamically linking the magnetosphere and ionosphere was hypothesized at the turn of the twentieth century (Birkeland, 1908, 1913). R1 FACs flow into the ionosphere (downward current) at dawn local times (LTs) and out (upward current) at dusk LTs, and the R2 FACs exhibit opposite polarities in each LT sector.

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