Temporal/spatial structure of magnetic merging at the magnetopause
inferred from 557.7-nm all-sky images
HR: 09:45h
AN: SM51A-08 [PDF]
TI: Temporal/spatial structure of magnetic merging at the magnetopause
inferred from 557.7-nm all-sky images
AU: * Maynard, N C
EM: nmaynard@mrcnh.com
AF: Mission Research Corporation, 589 West Hollis Street; Suite 201, Nashua, NH 03062 United States
AU: Moen, J
AF: University of Oslo, Deparment of Physics, Oslo, N-0316
Norway
AU: Burke, W J
AF: Air Force Research Laboratory, 29 Randolph Road, Hanscom AFB, MA 01731 United States
AU: Lester, M
AF: University of Leicester, Deparment of Physics, Leicester, LE1 7RH
United Kingdom
AU: Ober, D M
AF: Mission Research Corporation, 589 West Hollis Street; Suite 201, Nashua, NH 03062 United States
AU: Scudder, J D
AF: University of Iowa, Department of Physics and Astronomy, Iowa City, IA 52242 United States
AU: Siebert, K D
AF: Mission Research Corporation, 589 West Hollis Street; Suite 201, Nashua, NH 03062 United States
AU: Weimer, D R
AF: Mission Research Corporation, 589 West Hollis Street; Suite 201, Nashua, NH 03062 United States
AU: Russell, C T
AF: University of California at Los Angeles, IGPP, Los Angeles, CA 90015 United States
AU: Balogh, A
AF: Imperial College, Exhibition Road, London, SW7 2BW
United Kingdom
AB:
We demonstrate that high-resolution 557.7 nm all-sky images are useful tools for investigating the spatial and temporal
evolution of merging on the dayside magnetopause. Analysis of ground and satellite measurements leads us to conclude that
high-latitude merging events can occur at multiple sites simultaneously and vary asynchronously on time scales of 30 s to 3
min. Variations of 557.7 nm emissions were observed at a 10 s cadence at Ny-{\AA}lesund on December 19, 2001 while
significant changes in the IMF clock angle were reaching the magnetopause. The optical patterns are consistent with a
scenario in which merging occurs around the rim of the high-latitude cusp at positions dictated by the IMF clock angle.
Electrons energized at merging sites represent plausible sources for 557.7nm emissions in the cusp. Polar observations at the
magnetopause have directly linked enhanced fluxes of ${\ge}$0.5 keV electrons with merging. Spectra of electrons
responsible for some of the emissions, measured during a DMSP F15 overflight, exhibit ``inverted-V'' features indicating
further acceleration above the ionosphere. SuperDARN spectral width boundaries, characteristic of open-closed field line
transitions, are located at the equatorward edge of the 557.7-nm emissions. Optical data suggest that with IMF $B_Y > 0$,
the Northern Hemisphere cusp divides into three source regions. When the IMF clock angle was $\sim$150$^{\circ}$ structured
557.7 nm emissions came from east of the 1300 MLT meridian. At larger clock angles the emissions appeared between 1200 and
1300 MLT. No significant 557.7 nm emissions were detected in the prenoon MLT sector. MHD simulations corroborate our
scenario, showing that with the observed large dipole-tilt and IMF clock angles, merging sites develop near the front and
eastern portions of the high-altitude cusp rim in the Northern Hemisphere and near the western part of the cusp rim in the
Southern Hemisphere.
DE: 2407 Auroral ionosphere (2704)
DE: 2431 Ionosphere/magnetosphere interactions (2736)
DE: 2736 Magnetosphere/ionosphere interactions
DE: 2760 Plasma convection
DE: 2784 Solar wind/magnetosphere interactions
SC: SPA - Magnetospheric Physics [SM]
MN: 2003 Fall Meeting