A study of polar cap Pc1-2: source locations and wave propagation

The occurrence of Pcl-2 ULF waves in Scott Base and Casey Antarctic magnetometer data has been examined with the objective of determining whether the source region for these waves is located in the Earth's cusp/boundary layer region or the magnetosheath. In particular we explore the hypothesis...

Full description

Bibliographic Details
Main Authors: Ables, Sean, Sciffer, Murray, Fraser, Brian, Morley, Steven
Other Authors: The University of Newcastle. Faculty of Science & Information Technology, School of Mathematical and Physical Sciences
Format: Conference Object
Language:English
Published: National Space Society of Australia 2010
Subjects:
Online Access:http://hdl.handle.net/1959.13/935310
id ftunivnewcastnsw:uon:12033
record_format openpolar
spelling ftunivnewcastnsw:uon:12033 2023-05-15T13:54:38+02:00 A study of polar cap Pc1-2: source locations and wave propagation Ables, Sean Sciffer, Murray Fraser, Brian Morley, Steven The University of Newcastle. Faculty of Science & Information Technology, School of Mathematical and Physical Sciences 2010 http://hdl.handle.net/1959.13/935310 eng eng National Space Society of Australia 9th Australian Space Science Conference (ASSC 2010). Proceedings of the 9th Australian Space Science Conference (Sydney 28-30 Spetember, 2010) p. 105-114 http://www.nssa.com.au/ocs/index.php?cf=11 magnetosphere ULF waves geomagnetic mapping Antarctica conference paper 2010 ftunivnewcastnsw 2018-07-27T00:44:08Z The occurrence of Pcl-2 ULF waves in Scott Base and Casey Antarctic magnetometer data has been examined with the objective of determining whether the source region for these waves is located in the Earth's cusp/boundary layer region or the magnetosheath. In particular we explore the hypothesis that some Pcl-2 events are propagated along open field lines which convect over the southern polar cap. For a selected event the location of Scott Base with respect to the open/closed field line boundary was independently determined using DMSP spacecraft particle data and well established particle energy and flux criteria. This event provides evidence that Pcl-2 waves can be seen on the ground well inside the polar cap. The possibility of propagation in the ionospheric waveguide, away from the footpoint of the source, is investigated using numerical modelling and realistic ionospheric parameters. Under the modelled conditions we find a modification of wave ellipticity which excludes this explanation for the polar cap Pcl-2 seen in the event study. Conference Object Antarc* Antarctic Antarctica NOVA: The University of Newcastle Research Online (Australia) Antarctic Scott Base ENVELOPE(166.766,166.766,-77.849,-77.849)
institution Open Polar
collection NOVA: The University of Newcastle Research Online (Australia)
op_collection_id ftunivnewcastnsw
language English
topic magnetosphere
ULF waves
geomagnetic mapping
Antarctica
spellingShingle magnetosphere
ULF waves
geomagnetic mapping
Antarctica
Ables, Sean
Sciffer, Murray
Fraser, Brian
Morley, Steven
A study of polar cap Pc1-2: source locations and wave propagation
topic_facet magnetosphere
ULF waves
geomagnetic mapping
Antarctica
description The occurrence of Pcl-2 ULF waves in Scott Base and Casey Antarctic magnetometer data has been examined with the objective of determining whether the source region for these waves is located in the Earth's cusp/boundary layer region or the magnetosheath. In particular we explore the hypothesis that some Pcl-2 events are propagated along open field lines which convect over the southern polar cap. For a selected event the location of Scott Base with respect to the open/closed field line boundary was independently determined using DMSP spacecraft particle data and well established particle energy and flux criteria. This event provides evidence that Pcl-2 waves can be seen on the ground well inside the polar cap. The possibility of propagation in the ionospheric waveguide, away from the footpoint of the source, is investigated using numerical modelling and realistic ionospheric parameters. Under the modelled conditions we find a modification of wave ellipticity which excludes this explanation for the polar cap Pcl-2 seen in the event study.
author2 The University of Newcastle. Faculty of Science & Information Technology, School of Mathematical and Physical Sciences
format Conference Object
author Ables, Sean
Sciffer, Murray
Fraser, Brian
Morley, Steven
author_facet Ables, Sean
Sciffer, Murray
Fraser, Brian
Morley, Steven
author_sort Ables, Sean
title A study of polar cap Pc1-2: source locations and wave propagation
title_short A study of polar cap Pc1-2: source locations and wave propagation
title_full A study of polar cap Pc1-2: source locations and wave propagation
title_fullStr A study of polar cap Pc1-2: source locations and wave propagation
title_full_unstemmed A study of polar cap Pc1-2: source locations and wave propagation
title_sort study of polar cap pc1-2: source locations and wave propagation
publisher National Space Society of Australia
publishDate 2010
url http://hdl.handle.net/1959.13/935310
long_lat ENVELOPE(166.766,166.766,-77.849,-77.849)
geographic Antarctic
Scott Base
geographic_facet Antarctic
Scott Base
genre Antarc*
Antarctic
Antarctica
genre_facet Antarc*
Antarctic
Antarctica
op_relation 9th Australian Space Science Conference (ASSC 2010). Proceedings of the 9th Australian Space Science Conference (Sydney 28-30 Spetember, 2010) p. 105-114
http://www.nssa.com.au/ocs/index.php?cf=11
_version_ 1766260702122606592