• Sorted by Date • Sorted by Last Name of First Author •
Halter, Bryce F., Malaspina, David, Roddy, Patrick A., Maruyama, Naomi, and Andersson, Laila, 2026. The Role of Neutral Winds in Polar Cap Patch Instability Growth. Journal of Geophysical Research (Space Physics), 131(7):e2025JA034673, doi:10.1029/2025JA034673.
• from the NASA Astrophysics Data System • by the DOI System •
@ARTICLE{2026JGRA..13134673H,
author = {{Halter}, Bryce F. and {Malaspina}, David and {Roddy}, Patrick A. and {Maruyama}, Naomi and {Andersson}, Laila},
title = "{The Role of Neutral Winds in Polar Cap Patch Instability Growth}",
journal = {Journal of Geophysical Research (Space Physics)},
keywords = {polar cap patch, neutral wind, thermosphere, gradient drift instability, ionosphere},
year = 2026,
month = jul,
volume = {131},
number = {7},
eid = {e2025JA034673},
pages = {e2025JA034673},
abstract = "{Polar cap patches are regions of dense plasma in the polar cap that
convect from noon to midnight, moving against the neutral gas
background. The gradient drift instability (GDI) destabilizes
the edge of these patches as they convect, yet the rate of this
destabilization is not well known due to the scarcity of
coincident neutral wind and plasma measurements. Polar cap
patches detected by Swarm with conjunction measurements from
GRACE-FO are assessed for their GDI growth time with and without
the neutral wind and for high and low collisionality regimes.
This analysis shows significant differences in growth times with
and without the neutral wind, and that the low collisionality
growth times are different by a factor of 65\%. These results
demonstrate that coincident plasma and neutral wind measurements
are essential for accurately determining how the GDI, and by
extension polar cap patches, evolve.}",
doi = {10.1029/2025JA034673},
adsurl = {https://ui.adsabs.harvard.edu/abs/2026JGRA..13134673H},
adsnote = {Provided by the SAO/NASA Astrophysics Data System}
}
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