Plasma Parameters in Io's Torus: Measurements from Apache Point Observatory

Jake Turner1, Carl Schmidt2, Nicholas McCord Schneider3, Michael Chaffin4, Eric McNeil5, Nancy Chanover6, Apurva Vikram Oza1, Stacey Rugenski5, Alexander E Thelen7, Robert E Johnson8, Lauren Bittle1 and Patrick King1, (1)University of Virginia Main Campus, Charlottesville, VA, United States, (2)Boston University, Astronomy; Center for Space Physics, Boston, MA, United States, (3)Univ Colorado, Boulder, United States, (4)University of Colorado Boulder, Laboratory for Atmospheric and Space Physics, Boulder, United States, (5)Univ Colorado, Boulder, CO, United States, (6)New Mexico State University/NASA Planetary Data System (PDS), Atmospheres (ATM) Node, Las Cruces, United States, (7)USRA / NASA Goddard Space Flight Center, Greenbelt, United States, (8)University of Virginia, Materials Science and Engineering, Charlottesville, United States
Abstract:
The Io plasma torus is an astrophysical nebula wrapped around Jupiter, originating from the intense volcanic activity of Jupiter's moon Io. The torus varies both spatially and temporally, driven by changes in volcanism and asymmetries in the Jovian magnetosphere. We report results from 9 nights of observation spanning November 2013 to February 2014 with the Dual Imaging Spectrograph on the ARC 3.5m telescope at Apache Point Observatory in New Mexico. Emissions in these data include the [SII] doublets at 6716/6731A and 4069/4076A, [OII] at 3726/3729A, [SIII] at 3722A and 6312A, as well as resonantly scattered neutral [NaI] at 5890/5896A. Constraints on electron density, temperature and ion mixing rations can be obtained. Observations of both ansa during a 5 hour period characterize the complete longitudinal structure. Specifically, the intensity ratio of the collisionally excited [SII] doublet at 6716/6731A is a diagnostic for local electron density sampled at ~20 minute cadence. Absolute intensity can be derived directly from the reflectance of Jupiter's disc and standard calibrations are performed on the data such as bias subtraction, wavelength calibration and recti fication. A unique background subtraction procedure is developed to disentangle scattered Jovian reflection and the torus. These observations were made in conjunction with JAXA's Hisaki mission, the HST auroral campaign and infrared monitoring of volcanism to better understand how mass and energy are transported throughout the system.