Localized ion outflow in response to a solar wind pressure pulse

[1] Neutrals created by charge-exchange of low-energy (∼10–100 eV) ion outflow from the ionosphere are imaged by the Low Energy Neutral Atom (LENA) imager on the IMAGE spacecraft. Comparing the neutral flux with changes in the solar wind during an ion outflow event on 24 June 2000 indicates that changes in solar wind density (and therefore dynamic pressure) are associated with episodic bursts of ion outflow. LENA images show that these bursts are confined to the duskside. Simultaneous images of the aurora from the IMAGE FUV Wideband Imaging Camera indicate that these episodic bursts on the duskside are associated with increased duskside auroral emissions. The pitch angle and charge exchange altitude for the ion outflow distributions are estimated by applying field line tracing in a model magnetic field and assuming that the outflow occurs in the auroral zone. The pitch angle information places constraints on the neutral atom images, indicating that the ion outflow observed on the duskside probably consists of high pitch angle conics and that field-aligned ion outflow from other parts of the oval cannot be observed from the IMAGE spacecraft location.

[1]  C. M. Bjorklund,et al.  O+ and He+ restricted and extended (BI‐modal) ion conic distributions , 1992 .

[2]  E. Shelley Circulation of energetic ions of terrestrial origin in the magnetosphere , 1985 .

[3]  W.K. (Bill) Peterson,et al.  Long-term (solar cycle) and seasonal variations of upflowing ionospheric ion events at DE 1 altitudes , 1985 .

[4]  W. R. Paterson,et al.  The Comprehensive Plasma Instrumentation(CPI) for the GEOTAIL Spacecraft. , 1994 .

[5]  John W. Keller,et al.  Low energy neutral atoms in the magnetosphere , 2001 .

[6]  L. Blomberg,et al.  Ion cyclotron heating in the dayside magnetosphere , 1996 .

[7]  D. Klumpar,et al.  Direct evidence for two-stage (bimodal) acceleration of ionospheric ions , 1984 .

[8]  J. Quinn,et al.  The low-energy neutral atom imager for IMAGE , 2000 .

[9]  E. Shelley,et al.  SATELLITE OBSERVATIONS OF ENERGETIC HEAVY IONS DURING A GEOMAGNETIC STORM. , 1972 .

[10]  M. Yamauchi,et al.  Energetic ion outflow from the dayside ionosphere: Categorization, classification, and statistical study , 1999 .

[11]  B. A. Whalen,et al.  Distribution of upflowing ionospheric ions in the high‐altitude polar cap and auroral ionosphere , 1984 .

[12]  R. G. Johnson,et al.  Some mass dependent features of energetic ion conics over the auroral regions , 1985 .

[13]  J. Gérard,et al.  Proton aurora in the cusp , 2002 .

[14]  W. Miyake,et al.  On the origins of the upward shift of elevated (bimodal) ion conics in velocity space , 1996 .

[15]  O. W. Lennartsson,et al.  The seasonal variation of auroral ion beams , 1998 .

[16]  E. Shelley,et al.  Observation of an ionospheric acceleration mechanism producing energetic (keV) ions primarily normal to the geomagnetic field direction , 1977 .

[17]  Peter Wurz,et al.  Mass spectrograph for imaging low-energy neutral atoms , 1993, Optics & Photonics.

[18]  Stephen B. Mende,et al.  Ion outflow observed by IMAGE: Implications for source regions and heating mechanisms , 2001 .

[19]  A. G. McNamara,et al.  Particle and wave observations of low‐altitude ionospheric ion acceleration events , 1983 .

[20]  W. Lennartsson A scenario for solar wind penetration of earth's magnetic tail based on ion composition data from the ISEE 1 spacecraft , 1992 .

[21]  Hideaki Kawano,et al.  The GEOTAIL Magnetic Field Experiment. , 1994 .

[22]  M. Lockwood,et al.  Superthermal ion signatures of auroral acceleration processes , 1985 .

[23]  Mats André,et al.  Sources of Ion Outflow in the High Latitude Ionosphere , 1997 .