HR: 1340h
AN: P43A-1024 [Abstracts]
TI: Magnetospheric Storms at Saturn and Earth
AU: * Brandt, P C
EM: pontus.brandt@jhuapl.edu
AF: The Johns Hopkins University
Applied Physics Laboratory, 11100 Johns Hopkins Rd, Laurel, MD 20723, United States
AU: Mitchell, D G
EM: don.mitchell@jhuapl.edu
AF: The Johns Hopkins University
Applied Physics Laboratory, 11100 Johns Hopkins Rd, Laurel, MD 20723, United States
AU: Carbary, J
EM: jim.carbary@jhuapl.edu
AF: The Johns Hopkins University
Applied Physics Laboratory, 11100 Johns Hopkins Rd, Laurel, MD 20723, United States
AU: Rymer, A
EM: abigail.rymer@jhuapl.edu
AF: The Johns Hopkins University
Applied Physics Laboratory, 11100 Johns Hopkins Rd, Laurel, MD 20723, United States
AU: Hill, M E
EM: matt.hill@jhuapl.edu
AF: The Johns Hopkins University
Applied Physics Laboratory, 11100 Johns Hopkins Rd, Laurel, MD 20723, United States
AU: Paranicas, C
EM: chris.paranicas@jhuapl.edu
AF: The Johns Hopkins University
Applied Physics Laboratory, 11100 Johns Hopkins Rd, Laurel, MD 20723, United States
AU: Dougherty, M K
EM: m.dougherty@imperial.ac.uk
AF: Imperial College, Blackett Laboratory, London, SW72BZ, United Kingdom
AU: Young, D T
EM: dyoung@swri.edu
AF: Southwest Research Institute, Space Sci and Eng Division
6220 Culbera Dr, San Antonio, TX 78238, United States
AB:
The terrestrial magnetospheric storms are a well-known phenomenon in which
plasma from the solar wind and the ionosphere is convected into the
inner magnetosphere ("ring current") and energized by betatron
acceleration and rapid changes in the magnetic field (substorms). Here
we compare terrestrial storm characteristics with similar, newly found
characteristics of Saturn's magnetosphere. We characterize Saturn's
magnetospheric response to solar wind variability by using remote
energetic neutral atom (ENA) measurements with simultaneous in-situ
solar wind measurements when Cassini was outside the Saturnian
magnetosphere.
The Ion and Neutral Camera on board the Cassini spacecraft have
obtained global energetic neutral atom (ENA) images of the hot plasma
of Saturn's magnetosphere since February 2004. INCA obtains ENA images in
the ~3-200 keV/nuc of protons and O+. The typical observations
show hot plasma distributed roughly between 6 to 30 RS orbiting the
planet with a period around the 10h45min rotation period depending on
energy and species. However, some observations show how ENA intensity
builds up on the nightside during intervals longer than the rotation
period which indicates a gradual source of plasma. The intervals are
often ended by a dramatic ENA intensification followed by a rotation
of the newly injected plasma around the planet. We have selected a few
of such intervals when Cassini was in the solar wind and could obtain
solar wind parameters and simulataneous ENA image sequences. We use
the Magnetic Field Experiment (MAG), the Cassini Charge Energy Mass
Spectrometer (CHEMS), and the Cassini Plasma Spectrometer Subsystem
(CAPS) to study the IMF, solar wind speed and density during these
events and find that Saturn's magnetospheric activity most likely
depends more on solar wind pressure than magnetic field orientation.
DE: 2756 Planetary magnetospheres (5443, 5737, 6033)
DE: 2784 Solar wind/magnetosphere interactions
DE: 2788 Magnetic storms and substorms (7954)
DE: 6275 Saturn
DE: 6939 Magnetospheric physics (2700)
SC: Planetary Sciences [P]
MN: 2007 Fall Meeting