Edge of polar cap patches [PDF]
AbstractOn the night of 4 December 2013, a sequence of polar cap patches was captured by an all‐sky airglow imager (ASI) in Longyearbyen, Norway (78.1°N, 15.5°E). The 630.0 nm airglow images from the ASI of 4 second exposure time, oversampled the emission of natural lifetime (with quenching) of at least ∼30 sec, introduce no observational blurring ...
K. Hosokawa, S. Taguchi, Y. Ogawa
openaire +3 more sources
The term of “polar cap hot patch” is a newly identified high‐density plasma irregularity at high latitudes, which is associated with high electron temperature and particle precipitation, while a classical polar cap patch has lower electron temperature ...
Yu‐Zhang Ma +5 more
doaj +2 more sources
The interconnection between cross‒polar cap convection and the luminosity of polar cap patches [PDF]
The transport of patches of ionization across the polar cap is carried by the convection electric field, which imposes an E×B drift to the plasma. This drift has an upward component when the plasma is convected toward the north magnetic pole and a downward component as it moves away from the pole.
G. W. Perry +2 more
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Global imaging of polar cap patches with dual airglow imagers [PDF]
During a 2 h interval from 2240 to 2440 UT on 12 November 2012, regions of increased 630.0 nm airglow emissions were simultaneously detected by dual all‐sky imagers in the polar cap, one at Longyearbyen, Norway (78.1°N, 15.5°E) and the other at Resolute Bay, Canada (74.7°N, 265.1°E). The Resolute Bay incoherent scatter radar observed clear enhancements
K. Hosokawa +5 more
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Earth's ion upflow associated with polar cap patches: global and in-situ observations [PDF]
We report simultaneous global monitoring of a patch of ionization and in situ observation of ion upflow at the center of the polar cap region during a geomagnetic storm.
Dunlop, Malcolm W. +17 more
core +3 more sources
Tracking of polar cap ionospheric patches using data assimilation [PDF]
Ionospheric F‐region patches are 2–10 larger than background electron densities in the polar ionosphere. The EISCAT Svalbard incoherent radar (ESR) observed a sequence of patches between 2000–2200 UT on 12 December 2001. In this paper the source of these structures is investigated using several other data sets, together with a convection‐driven ...
G. S. Bust, G. Crowley
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Determining decay rates of polar cap plasma using bservations of polar cap patches [PDF]
Polar cap patches are large scale structures occurring in the high-latitude ionosphere. They are regions of enhanced plasma density of at least twice the background density, and they are often observed in the polar cap region. The primary decay mechanism
Hardwick, L, Wood, A
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GPS phase scintillation at high latitudes during geomagnetic storms of 7–17 March 2012 – Part 2: Interhemispheric comparison [PDF]
During the ascending phase of solar cycle 24, a series of interplanetary coronal mass ejections (ICMEs) in the period 7–17 March 2012 caused geomagnetic storms that strongly affected high-latitude ionosphere in the Northern and Southern Hemisphere ...
P. Prikryl +20 more
doaj +6 more sources
On the possible role of cusp/cleft precipitation in the formation of polar-cap patches [PDF]
The work describes experimental observations of enhancements in the electron density of the ionospheric F-region created by cusp/cleft particle precipitation at the dayside entry to the polar-cap convection flow.
I. K. Walker +5 more
doaj +3 more sources
GPS phase scintillation and proxy index at high latitudes during a moderate geomagnetic storm [PDF]
The amplitude and phase scintillation indices are customarily obtained by specialised GPS Ionospheric Scintillation and TEC Monitors (GISTMs) from L1 signal recorded at the rate of 50 Hz.
P. Prikryl +7 more
doaj +5 more sources

