*************************** ** THE GEM MESSENGER ** *************************** Volume 16, Number 7 April 13, 2006 --------------------------------------------------------------------------- MI Coupling Campaign Mass Outflow Working Group GEM 2006 Summer Meeting (June 25-30, 2006) Snowmass, CO 1. Workshop on "Magnetospheric/Ionospheric Coupling: Heavy Ion Effects on Tail Dynamics and Magnetic Reconnection" 2. Workshop on "Energization of thermal O+ below 3000 km during geomagnetically quiet times" --------------------------------------------------------------------------- From: From Robert Winglee and Bill Peterson 1. Workshop on "Magnetospheric/Ionospheric Coupling: Heavy Ion Effects on Tail Dynamics and Magnetic Reconnection" During active periods the tail is known to thin substantially to scale lengths as small as a few hundred km. At the same time ionospheric outflows are known to be substantially increased, and on occasions heavy ionospheric ions can even be the dominant ion component in the tail. Because of their much larger gyro-radius, these heavy ions have the potential for substantially modifying the dynamics of these thin currents sheets and influence reconnection rates and the creation of energetic particle populations. The workshop will focus on the observations and modeling of heavy ion effects on the tail dynamics. Lynn Kistler will provide a lead off discussion on observations aspects and Michael Shay will give a lead off discussion on model aspects. The workshop solicits additional contributions addressing but not limited to: 1. How much O+ is needed to modify the tail dynamics from that of a simple H+ (Is it just a few percent or is substantial injection needed?) 2. Does the tail response dependent on newly ejected O+ or will it see immediate effects from pre-existing O+ that has convected into the tail from earlier ionospheric outflows? 3. What are (if any) the physical differences in the tail dynamics from a proton dominated tail to a heavy ion enriched tail (e.g. reconnection rate, size of reconnection region)? Joint with Global Interaction (GI) Campaign Working Group on Plasma Acceleration and Transport in the Magnetotail (PATM). Please contact Robert Winglee (winglee@ess.washington.edu) or Bill Peterson (Bill.Peterson@lasp.colorado.edu) if you want to participate in this workshop. ====================================================== 2. Workshop on "Energization of thermal O+ below 3000 km during geomagnetically quiet times" In this workshop we want to focus on the processes responsible for the energization of O+ during geomagnetically quiet intervals in the altitude region below ~ 3000 km. Heavy thermal ions such as O+ and NO+ are created in the ionosphere and are strongly gravitationally bound. It is well know that, during geomagnetically active times, O+ and NO+ with energies of up to 100's of keV are observed throughout the magnetosphere. It is also well established that, during geomagnetically quiet times, measureable fluxes of O+ are observed deep in the magnetotail with energies on the order of a few hundred eV. The observed maximum upwelling velocities of ~ 1 km/s in the top side ionosphere provide only a small fraction of the ~10 eV energy required to explain the large fluxes of O+ observed at quiet times in the magnetotail. Anecdotal evidence suggests that the extra energy required to explain the quiet time escape of O+ is added in the altitude region below the auroral acceleration cavity (~3000 km). Processes thought to be involved include wave-particle interactions, ambi-polar electric fields, and hydrodynamic expansion in response to a plasma pressure gradient along the magnetic field line. Paul Kintner will be presenting a tutorial lecture on "Magnetosphere- Ionosphere Coupling Below 1500 km: Conversion of Upwelling Ions to Escaping Ions" For this workshop, we solicit short presentations (less than 5 view graphs) ideally supplemented by a poster presentation on: - Wave-particle interactions at all local times, not just the cusp. - Hydrodynamic expansion of O+ on auroral field lines as well as within the polar cap. - Observational constraints on the velocity and density of upflowing O+ Please contact Robert Winglee (winglee@ess.washington.edu) or Bill Peterson (Bill.Peterson@lasp.colorado.edu) if you want to participate in this workshop. Instructions on how to submit posters will appear soon on the workshop web page (http://gem.rice.edu/~gem/gem2006/index.html) +-------------------------------------------------------------------------+ |To subscribe GEM Messengers, send an e-mail to | | with the following command in the body of your e-mail message: | | subscribe gem | |To remove yourself from the mailing list, the command is: | | unsubscribe gem | | | |To broadcast a message to the GEM community, please contact Peter Chi at | | | |Please use plain text as the format of your submission. | | | |URL of GEM Home Page: http://www-ssc.igpp.ucla.edu/gem/Welcome.html | |Workshop Information: http://gem.rice.edu/~gem | +-------------------------------------------------------------------------+