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  4. Cusp Dynamics and Polar Cap Patch Formation Associated With a Small IMF Southward Turning

Cusp Dynamics and Polar Cap Patch Formation Associated With a Small IMF Southward Turning

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JGR Space Physics - 2021 - Nishimura - Cusp Dynamics and Polar Cap Patch Formation Associated With a Small IMF Southward.pdf

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Author(s)
Nishimura, Y
•
Sadler, FB
•
Varney, RH
•
Gilles, R
•
Zhang, SR
•
Coster, AJ
•
Nishitani, N
•
Otto, A
Date Issued
May 6, 2021
Journal
Journal of Geophysical Research: Space Physics
Publisher
American Geophysical Union
Citation
Nishimura, Y., Sadler, F. B., Varney, R. H., Gilles, R., Zhang, S. R., Coster, A. J., et al. (2021). Cusp dynamics and polar cap patch formation associated with a small IMF southward turning. Journal of Geophysical Research: Space Physics, 126, e2020JA029090.
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Final published version
Abstract
We present high‐resolution Resolute Bay Incoherent Scatter Radar (RISR) measurements in the cusp region during an IMF southward turning. The simultaneous RISR‐N and RISR‐C operation provided 3‐D observations of the dayside polar region, and offered an opportunity to identify the cusp dynamics and polar cap patch formation. Associated with the IMF southward turning, the F‐region density and temperature increased in the cusp, and the increase was particularly evident in the topside ionosphere. The high‐density plasma drifted into the polar cap by an enhanced poleward convection, and became a polar cap patch. The patch plasma was initially dominated by density originating in the cusp, and then later the subauroral ionospheric plasma also contributed to the density enhancement. Weak upflows were present but their contribution within the RISR altitude range was minor. We suggest that the patch source region switches due to dynamic variations of the cusp precipitation and convection from lower latitudes. RISR also detected a flow vortex embedded in the large‐scale convection, which is likely a poleward moving auroral form (PMAF) signature. Joule heating peaked in the cusp E and lower F‐regions. The F‐region Pedersen conductivity increased more than the Hall conductivity, and the high conductivity region extended poleward associated with the patch density enhancement. A 1‐D cusp simulation reproduced the density and temperature enhancements by soft electron precipitation, indicating the importance of soft electron precipitation for the cusp dynamics and the initial part of the patch formation.
MIT Department
Haystack Observatory
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Article is made available in accordance with the publisher's policy and may be subject to US copyright law. Please refer to the publisher's site for terms of use.
Persistent DSpace Link
https://dspace.mit.edu/handle/1721.1/175918
DOI of Published Version
https://doi.org/10.1029/2020ja029090
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