PULSATING CUSP AURORA FOR NORTHWARD INTERPLANETARY MAGNETIC-FIELD

Citation
Pe. Sandholt et al., PULSATING CUSP AURORA FOR NORTHWARD INTERPLANETARY MAGNETIC-FIELD, J GEO R-S P, 103(A11), 1998, pp. 26507-26520
Citations number
27
Categorie Soggetti
Geosciences, Interdisciplinary","Astronomy & Astrophysics","Metereology & Atmospheric Sciences",Oceanografhy,"Geochemitry & Geophysics
Journal title
JOURNAL OF GEOPHYSICAL RESEARCH-SPACE PHYSICS
ISSN journal
21699380 → ACNP
Volume
103
Issue
A11
Year of publication
1998
Pages
26507 - 26520
Database
ISI
SICI code
2169-9380(1998)103:A11<26507:PCAFNI>2.0.ZU;2-N
Abstract
We report a characteristic bifurcation of the cusp aurora in associati on with northward transitions of the interplanetary magnetic field (IM F), leading to the coexistence of latitudinally separated forms, calle d types I and 2. In the northernmost form (type 2), which is located a t similar to 77 - 79 degrees MLAT, there appears a sequence of auroral brightenings at the poleward boundary of the preexisting luminosity. Each brightening is followed by equatorward motion and fading of the i ndividual forms. Furthermore, coherent intensity variations of the two latitudinally separated forms are often observed. This is documented by three case examples. The most active phase of the type 2 aurora is observed during intervals of 15 - 20 min duration following northward turnings of the IMF and with nonzero IMF B-y component, corresponding to the transition state before a new equilibrium state of solar wind-m agnetosphere coupling is established. The auroral observations are dis cussed in relation to theoretical models of ionospheric convection, fi eld-aligned currents and solar wind-magnetosphere coupling in the pola r cusp region. The type 2 auroral activity in the north is interpreted as an ionospheric signature which is directly related to reconnection between the IMF and the terrestrial lobe field at the high-latitude m agnetopause, whereas the type 1 aurora is coupled to the low latitude magnetopause. The coherent activations of the two auroral forms indica te that the corresponding current systems are strongly coupled at the ionospheric level.