SETI bioastro: FW: SwRI: Jovian magnetosphere circulation differs from Earth's

From: LARRY KLAES (ljk4_at_msn.com)
Date: Tue Oct 23 2007 - 11:08:53 PDT

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    >From: Lynn Cominsky <lynnc_at_universe.sonoma.edu>
    >To: lynnc_at_universe.sonoma.edu
    >Subject: SwRI: Jovian magnetosphere circulation differs from Earth's
    >Date: Tue, 23 Oct 2007 09:41:44 -0700
    >
    >THE FOLLOWING RELEASE WAS RECEIVED FROM THE SOUTHWEST RESEARCH INSTITUTE,
    >IN SAN ANTONIO, TEXAS, AND IS FORWARDED FOR YOUR
    >INFORMATION. (FORWARDING DOES NOT IMPLY ENDORSEMENT BY THE AMERICAN
    >ASTRONOMICAL SOCIETY.) Lynn Cominsky, American Astronomical Society
    >lynnc_at_universe.sonoma.edu 1-707-664-2655
    >
    >New theory proposes Jovian magnetosphere circulates magnetic field
    >remarkably
    >different from that of Earth
    >
    >
    >For immediate release
    >
    >PIO Contact:
    >Maria Martinez
    >maria.martinez_at_swri.org
    >(210) 522-3305
    >
    >
    >San Antonio -- Oct. 23, 2007 -- Space physicists have long assumed that the
    >magnetosphere at Jupiter circulates that planet's magnetic field in the
    >same way as Earth. At Earth, this circulation drives the aurora and the
    >magnetic storms that cause space weather. Researchers from Southwest
    >Research Institute and the University of Colorado at Boulder have developed
    >a new model that postulates the structure and magnetospheric processes at
    >Jupiter are significantly different from those at Earth.
    >
    >
    >
    >The invisible area of space around a planet controlled by its magnetic
    >field,
    >the magnetosphere, interacts with the high-speed solar wind in a complex
    >way,
    >particularly in the area where the magnetic field in the solar wind
    >interconnects with the planetary field, through a process called magnetic
    >reconnection. The Dungey cycle, developed by British scientist Jim Dungey
    >in 1961, is the scientifically accepted paradigm for explaining how
    >magnetic
    >reconnection circulates the Earth's magnetic field. During this cycle,
    >magnetic
    >field lines are brought up near the nose of the magnetosphere where they
    >interconnect, becoming "open" and coupling the energy from the motion of
    >the
    >solar wind into the magnetosphere. That interconnection allows vast energy
    >from the million mile-per-hour solar wind into the magnetosphere, which is
    >the driving force behind geomagnetic storms, or space weather, that can
    >seriously damage or destroy probes and satellites. Subsequent motion of the
    >solar wind around the Earth's magnetosphere drags the interconnected field
    >lines back over its magnetic poles where they drift down into the center of
    >the magnetotail and reconnect again, but this time with similar field lines
    >from the opposite hemisphere so that they are "closed" or connected to the
    >planet at both ends. Finally, the Dungey cycle completes as the newly
    >closed
    >field lines circulate back toward Earth, around to its dayside and back to
    >its starting position at the nose of the magnetosphere.
    >
    >"For years space physicists have considered the Dungey cycle to be the
    >dominant circulation process in magnetospheres throughout the solar system,
    >even though observations from the largest magnetosphere in the solar system
    >--
    >Jupiter's -- didn't add up," says Dr. David McComas, senior executive
    >director
    >of the Space Science and Engineering Division at Southwest Research
    >Institute.
    >
    >"There are three key ways that the magnetosphere of Jupiter differs from
    >that
    >of Earth," argues Dr. Fran Bagenal, a professor of Astrophysical and
    >Planetary
    >Sciences at CU. "It's much bigger, it spins faster and it has a powerful
    >source of material."
    >
    >The large size of the Jovian magnetosphere means that the time it takes for
    >material that reconnects in the magnetotail and moves back up to Earth is
    >only about 10 hours, less than half a day. However, the process at Jupiter
    >takes 750 to 1,000 hours.
    >
    >"Consider that a Jupiter day is only about 10 hours," says McComas. "That
    >means it would take as many as 100 Jovian days for reconnected field lines
    >to
    >move back up to Jupiter -- a staggering difference."
    >
    >Furthermore, the magnetosphere of Jupiter is coupled to the spinning
    >planet.
    >"Imagine stirring up a bowl of spaghetti," says Bagenal. "The fast, 10-hour
    >spin of the Jovian magnetic field complicates the topology of flux tubes
    >that are connected to the planet on one end while the other, open end is
    >swept
    >away by the solar wind."
    >
    >Another difference is that Jupiter has an active volcanic moon, Io, which
    >spews out roughly a ton of material, mostly sulfur and oxygen, every
    >second.
    >Half of that material is lost through a process called charge exchange, but
    >the other half moves down the Jovian magnetotail as ions dragging the
    >planetary
    >magnetic field tailward. Earth has no such counterpart to impede the
    >return
    >flow back toward the planet.
    >
    >The new theory suggests a different geometry for closing off the magnetic
    >field
    >that has become interconnected with the solar wind -- additional magnetic
    >reconnection with other solar wind field lines that produce closed
    >planetary
    >field lines by reconnecting with open lines anchored back to both magnetic
    >poles. This geometry at Jupiter allows for tailward flow everywhere in the
    >tail and doesn't require a planetward flow, as at Earth. This explains why
    >the
    >polar aurora at Jupiter doesn't look like the terrestrial aurora. It also
    >explains why observations from Ulysses showed that open flux occurs at low
    >latitudes, not at the high latitudes required at Earth. The magnetosphere
    >at
    >Jupiter drags the material further down the sides so that they occur at
    >lower
    >latitudes.
    >
    >"Our model matches up with the observations -- further evidence that the
    >magnetospheric structure and processes at Earth and Jupiter are quite
    >different," says McComas.
    >
    >McComas and Bagenal determined these processes for Jupiter, yet they could
    >aid
    >in understanding the magnetospheres of the other outer planets, as well as
    >in other astrophysical environments where magnetic fields play an important
    >role.
    >
    >The paper, "Jupiter: A Fundamentally Different Magnetospheric Interaction
    >with
    >the Solar Wind," by David J. McComas and Fran Bagenal was published in the
    >Oct. 24 issue of Geophysical Research Letters.
    >
    >
    >Editors: Images to accompany this article are available at

    >http://www.swri.org/press/2007/Jovian.htm.
    >

    >


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