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University of Saskatchewan

F-region Dusk Ion Temperature Spikes at the Equatorward Edge of the High Latitude Convection Region

Abstract

dc:description.abstract

By examining continuous data from the Poker Flat Incoherent Scatter Radar (PFISR) in Poker Flat, Alaska, short-lived enhancements in the F-region ion temperature, or "Tᵢ spikes", were discovered in the evening while the radar was on the equatorward edge of the high latitude convection region. These enhancements were several hundred Kelvin above the background temperature, would last less than 15 minutes and were preceded by sharp depletions in plasma density (of roughly one half). Though they were mostly detected in the summer, 25 events throughout a whole year of data were identi ed in which the spike occurred within 1.5 hours of the density drop. By examining the location of PFISR at the time of the enhancements, as well as the conditions under which these spikes occurred, it was concluded that these enhancements were the result of electric elds increasing the frictional heating between ions and neutrals. By then examining geophysical data, it was found that these events were temporal and related to changes in magnetic indices. One possible explanation for the observations is that the electric eld is at its strongest near the plasmapause during substorms. Another more likely possibility is that during substorms the region of sunward ion convection expands into a region in the evening side where the neutral gas moves in a direction opposite to the ions, thereby enhancing the frictional heating rate.

Degree

thesis:*
Name thesis:degree_name
Master of Science (M.Sc.)
Level thesis:degree_level
Masters
Discipline thesis:degree_discipline
Physics
Grantor
University of Saskatchewan
Year dc:date.issued
2013

Author and committee

dc:creator, dc:contributor.*
Author dc:creator
  • Goodwin, Lindsay
Advisor dc:contributor.advisor
  • St.-Maurice, Jean-Pierre
Committee members dc:contributor.committeemember
  • Sofko, George
  • Koustov, Sasha
  • Smolyakov, Andrei
  • Bugg, Jim

Subjects

dc:subject × 8

Rights

Language dc:language.iso
eng

Identifiers

dc:identifier.*
OAI identifier oai:identifier
oai:harvest.usask.ca:10388/ETD-2013-12-1333

Chain of custody

source
Harvested from
University of Saskatchewan
Base URL
harvest.usask.ca/server/oai/request
Last updated
2026-07-24
Source record
OAI-PMH GetRecord
citation

Goodwin, Lindsay. F-region Dusk Ion Temperature Spikes at the Equatorward Edge of the High Latitude Convection Region. Masters thesis, University of Saskatchewan, 2013. https://hdl.handle.net/10388/ETD-2013-12-1333