Physics
Scientific paper
May 2001
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2001agusm..sm51b04m&link_type=abstract
American Geophysical Union, Spring Meeting 2001, abstract #SM51B-04
Physics
2724 Magnetopause, Cusp, And Boundary Layers, 2736 Magnetosphere/Ionosphere Interactions, 2740 Magnetospheric Configuration And Dynamics, 2784 Solar Wind/Magnetosphere Interactions
Scientific paper
The precession of Polar's apogee toward the equator provided opportunities in March and April, 2000 for the satellite to execute south-to-north skimming orbits along the dayside magnetopause. With the spacecraft in or adjacent to the magnetopause current layer for long periods at relatively low latitudes, particle and field measurements provide new perspectives concerning the temporal evolution of merging locations. This presentation focuses on data acquired during a 16 April pass. The last closed field line was tilted toward the IMF orientation as Polar entered the current sheet, similar to recent simulations [Maynard et al., 2001]. Initially BY was positive, and plasma flow along the magnetopause was toward dawn, placing the spacecraft north of the separator line. Outside the center of the magnetopause current layer the clock angle of the magnetic field measured at Polar closely tracked variations of the IMF clock angle. As BY reversed from positive to negative polarity local minima in the magnetic field and accelerated magnetosheath ions indicate that the merging site temporarily approached the spacecraft at low latitudes. Merging returned to high-latitude locations as BY again became the dominant component. We compare in situ data with predictions of MHD simulations and with dayside convection measurements by SuperDARN radars to place point measurements by Polar into large scale contexts and specify ionospheric convection responses to the time-varying inputs.
Burke William J.
Lester Mark
Maynard Nelson C.
Mozer Forrest S.
Ober Daniel M.
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