Simultaneous optical, CUTLASS HF radar, and FAST spacecraft observations: signatures of boundary layer processes in the cusp

被引:21
作者
Oksavik, K [1 ]
Soraas, F
Moen, J
Pfaff, R
Davies, JA
Lester, M
机构
[1] Univ Oslo, Dept Phys, Oslo, Norway
[2] Univ Bergen, Dept Phys, Bergen, Norway
[3] Univ Ctr Svalbard, Longyearbyen, Norway
[4] NASA, Goddard Space Flight Ctr, Greenbelt, MD 20771 USA
[5] Univ Leicester, Dept Phys & Astron, Leicester LE1 7RH, Leics, England
关键词
ionosphere; electric fields and currents; magnetosphere physics; magnetopause; cusp; and boundary layers; auroral phenomena;
D O I
10.5194/angeo-22-511-2004
中图分类号
P1 [天文学];
学科分类号
0704 ;
摘要
In this paper we discuss counterstreaming electrons, electric field turbulence, HF radar spectral width enhancements, and field-aligned currents in the southward IMF cusp region. Electric field and particle observations from the FAST spacecraft are compared with CUTLASS Finland spectral width enhancements and ground-based optical data from Svalbard during a meridional crossing of the cusp. The observed 630 nm rayed arc (Type-1 cusp aurora) is associated with stepped cusp ion signatures. Simultaneous counterstreaming low-energy electrons on open magnetic field lines lead us to propose that such electrons may be an important source for rayed red arcs through pitch angle scattering in collisions with the upper atmosphere. The observed particle precipitation and electric field turbulence are found to be nearly collocated with the equatorward edge of the optical cusp, in a region where CUTLASS Finland also observed enhanced spectral width. The electric field turbulence is observed to extend far poleward of the optical cusp. The broad-band electric field turbulence corresponds to spatial scale lengths down to 5 m. Therefore, we suggest that electric field irregularities are directly responsible for the formation of HF radar backscatter targets and may also explain the observed wide spectra. FAST also encountered two narrow highly structured field-aligned current pairs flowing near the edges of cusp ion steps.
引用
收藏
页码:511 / 525
页数:15
相关论文
共 106 条
[1]   Instantaneous ionospheric global conductance maps during an isolated substorm [J].
Aksnes, A ;
Stadsnes, J ;
Bjordal, J ;
Ostgaard, N ;
Vondrak, RR ;
Detrick, DL ;
Rosenberg, TJ ;
Germany, GA ;
Chenette, D .
ANNALES GEOPHYSICAE, 2002, 20 (08) :1181-1191
[2]   On the SuperDARN autocorrelation function observed in the ionospheric cusp [J].
André, R ;
Pinnock, M ;
Rodger, AS .
GEOPHYSICAL RESEARCH LETTERS, 1999, 26 (22) :3353-3356
[3]   Influence of magnetospheric processes on winter HF radar spectra characteristics [J].
André, R ;
Pinnock, M ;
Villain, JP ;
Hanuise, C .
ANNALES GEOPHYSICAE, 2002, 20 (11) :1783-1793
[4]   Identification of the low-altitude cusp by Super Dual Auroral Radar Network radars:: A physical explanation for the empirically derived signature [J].
André, R ;
Pinnock, M ;
Rodger, AS .
JOURNAL OF GEOPHYSICAL RESEARCH-SPACE PHYSICS, 2000, 105 (A12) :27081-27093
[5]  
ANDRE R, 2000, INT J GEOMAG AERONOM, V2, P77
[6]   HF RADAR SIGNATURES OF THE CUSP AND LOW-LATITUDE BOUNDARY-LAYER [J].
BAKER, KB ;
DUDENEY, JR ;
GREENWALD, RA ;
PINNOCK, M ;
NEWELL, PT ;
RODGER, AS ;
MATTIN, N ;
MENG, CI .
JOURNAL OF GEOPHYSICAL RESEARCH-SPACE PHYSICS, 1995, 100 (A5) :7671-7695
[7]   NEW MODEL FOR INTERACTION OF AURORAL ELECTRONS WITH ATMOSPHERE - SPECTRAL DEGRADATION, BACKSCATTER, OPTICAL EMISSION, AND IONIZATION [J].
BANKS, PM ;
CHAPPELL, CR ;
NAGY, AF .
JOURNAL OF GEOPHYSICAL RESEARCH, 1974, 79 (10) :1459-1470
[8]   SMALL-SCALE ELECTRODYNAMICS OF THE CUSP WITH NORTHWARD INTERPLANETARY MAGNETIC-FIELD [J].
BASINSKA, EM ;
BURKE, WJ ;
MAYNARD, NC ;
HUGHES, WJ ;
WINNINGHAM, JD ;
HANSON, WB .
JOURNAL OF GEOPHYSICAL RESEARCH-SPACE PHYSICS, 1992, 97 (A5) :6369-6379
[9]   IRREGULARITY STRUCTURES IN THE CUSP CLEFT AND POLAR-CAP REGIONS [J].
BASU, S ;
BASU, S ;
CHATURVEDI, PK ;
BRYANT, CM .
RADIO SCIENCE, 1994, 29 (01) :195-207
[10]   Investigation of the outer and inner low-latitude boundary layers [J].
Bauer, TM ;
Treumann, RA ;
Baumjohann, W .
ANNALES GEOPHYSICAE, 2001, 19 (09) :1065-1088