Journal
JOURNAL OF GEOPHYSICAL RESEARCH-SPACE PHYSICS
Volume 111, Issue A10, Pages -Publisher
AMER GEOPHYSICAL UNION
DOI: 10.1029/2006JA011676
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- Science and Technology Facilities Council [PP/D000912/1] Funding Source: researchfish
- STFC [PP/D000912/1] Funding Source: UKRI
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[ 1] The first close Titan encounters TA, TB, and T3 of the Cassini mission at almost the same Saturnian local time similar to 1030 and in the same spatial region downstream of Titan have enabled us to study the formation of the tail of its induced magnetosphere. The study is based on magnetic field and electron plasma observations as well as three-dimensional modeling. Our most important findings are the following: ( 1) No crossings of a bow shock of Titan were observed, and all encounters occurred at high plasma beta > 1 for transsonic and trans-Alfvenic Mach numbers. ( 2) The magnetic draping signature of the induced magnetosphere often shows a sharp outer boundary called the draping boundary (DB) in the near-tail region. ( 3) The DB is often occurring as a discontinuity in magnetic field spatial derivatives, and therefore the DB is a discontinuity in the spatial distribution of plasma currents. ( 4) Perpendicular to the incident flow direction the DB shows an approximately elliptic cross section elongated along the incident magnetic field direction and a displacement toward the Sun. ( 5) We argue that the DB in the magnetic tail region corresponds to the boundary of a structure which is analogous to an Alfven wing at very small beta and in our case of larger beta contains Alfvenic and slow mode features. It forms a tail like a delta wing in aerodynamics. ( 6) For the two less disturbed flybys, TA and T3, a polarity reversal layer has been observed with thicknesses of similar to 320 km and similar to 230 km, respectively.
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