Statistical characteristics of field-aligned currents in Saturn's nightside magnetosphere

Details Statistical characteristics of field-aligned currents in Saturn's nightside magnetosphere Statistical characteristics of field-aligned currents in Saturn's nightside magnetosphere

Apr 2011

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2011jgra..11604213t&link_type=abstract

Journal of Geophysical Research, Volume 116, Issue A4, CiteID A04213

Physics

3

Magnetospheric Physics: Planetary Magnetospheres (5443, 5737, 6033), Magnetospheric Physics: Field-Aligned Currents And Current Systems (2409), Magnetospheric Physics: Auroral Phenomena (2407), Magnetospheric Physics: Ring Current, Magnetospheric Physics: Solar Wind/Magnetosphere Interactions

Scientific paper

During 2008, the Cassini spacecraft traversed Saturn's high-latitude field-aligned current systems on sequential north-south periapsis passes in the nightside magnetosphere. Two types of current systems have previously been identified, associated with antisymmetric azimuthal field signatures in the northern and southern hemispheres. The first exhibits exclusively “lagging” field morphology, while the second also includes an equatorward interval of “leading” field. Here we report the statistical characteristics of these currents, their strength, ionospheric location, and relationship to plasma boundaries. From high to low latitude, the first type comprises a downward current followed by an upward current, whose strengths are ˜0.5-3.5 MA per radian of azimuth. The downward current maps to ionospheric colatitudes of ˜13.5° and ˜16° in the north and south, respectively, usually centered in the outer magnetosphere, while the upward current maps to ˜16.5° and ˜19° in the north and south, located within the ring current region. The second type comprises a distributed downward current of ˜1-2 MA rad-1 flowing in the open field and outer magnetosphere regions, followed by an upward current of ˜2.5-5 MA rad-1 mapping to ˜15.5° and ˜18° in the north and south, corresponding to the outer magnetosphere and outer ring current, and a further downward current of ˜1-2.5 MA rad-1 mapping to ˜17.5° and ˜20° in the north and south, corresponding to the inner ring current.

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