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			 **   THE GEM MESSENGER   **
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						     Volume 11, Number 28
						     August 20, 2001

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Reports of 2001 GEM Snowmass Workshops:
Inner Magnetosphere/Storms Campaign WG2: Radiation Belts 
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From: Geoff Reeves <reeves at lanl.gov>

Report on the IM/S WG2 (Radiation Belts) sessions at the 2001 GEM 
workshop by working group chairs Richard Thorne and Geoff Reeves.

Five 2-hr sessions on the radiation belts were held at the 2001 GEM 
meeting. They were:
``New Insights from the GEM storms''
``Observations of Stormtime Radiation Belt Variability''
``Observations of ULF and VLF Waves during Storms''
``Theoretical Studies of Radiation Belt Particle Acceleration and Loss''
``The Role of Substorms in Relativistic Electron Acceleration''

Our WG2 sessions were very stimulating, attracting more than 50 
participants including a large number of students and younger 
scientists.  The major emphasis was devoted at understanding the 
acceleration and loss of relativistic electrons during storms. 
Rather than itemize the separate contributions we will simply 
summarize the major advances made over the last year and outline our 
plans for further study in the coming year.

Observational Advances
* The different response to storms has been characterized as a 
  function of energy and L.
* Data have been analyzed to yield the particle phase space density 
  as a function of L for constant first and second adiabatic invariant.
* Evolution of the electron spectral properties has been measured 
  during acceleration events.
* Variation of the peak flux location seems to be controlled by the 
  storm strength.
* The solar wind parameters have a major controlling influence on 
  subsequent relativistic electron enhancements.
* The relativistic electron pitch-angle distributions have been 
  measured during acceleration events.

Precipitation Loss
* Microbursts of precipitating relativistic electrons have been seen 
  in associated with VLF chorus emissions.
* Balloon X-ray observation, have been linked to relativistic electron 
  scattering by EMIC waves.
* There is evidence for strong relativistic electron loss during the 
  main phase of a storm.
* Losses during the recovery phase appear to be much weaker, as 
  indicated by the pitch-angle distributions.

Acceleration Processes
* Radial inward diffusion.  There is convincing statistical evidence 
  that electron enhancements at geosynchronous orbit are associated 
  with sustain levels of enhanced ULF waves.
* Local stochastic acceleration.  Electron enhancements during the 
  recovery phase of storms are also associated with enhanced levels of 
  VLF whistler-mode chorus emissions.  This supports theoretical 
  studies on the viability of local stochastic energy diffusion by such 
  waves but further work is needed to quantify this process.
* Substorm dipolarization.  MeV electrons can be directly injected 
  into the outer radiation zone during dipolarization events.  Whether 
  this contributes to stormtime enhancement remains to be determined.

Maturing Models
* Empirical models have been developed to predict the behavior of 
  relativistic electrons at geosynchronous orbit, based only on solar 
  wind input parameters.
* A three-dimensional diffusion model (Salammbo) has been developed to 
  study radiation belt particle dynamics during conditions when the 
  adiabatic invariants are violated.

Future Plans
* There is a general realization that all three adiabatic invariants 
  can be violated during storm conditions.  Future work should 
  concentrate on a quantification of the competing acceleration and 
  loss process.
* ULF driven radial diffusion seems to be an important process at 
  geosynchronous orbit but further work is needed to assess whether it 
  is rapid enough to account for electron flux enhancements near L=4.
* The role of VLF waves in causing precipitation loss and energy 
  diffusion needs to be quantified.
* We need to study the loss process of electrons during the storm main phase.
* There is a need for better observational information from 
  multi-point satellite observations.

Status of Campaign Storm Studies
The focus on four storms for analysis in campaign mode has proven to 
be very helpful for this campaign and those analyses have become 
fairly mature. These storms are being studied jointly by working 
groups 1 and 2 and address the needs of both ring 
current/plasmasphere and radiation belt groups. There was consensus 
to extend this effort by
1) Using the May 1997 storm as a focus for combining models into a 
   more complete and comprehensive picture of the storm-time response. 
   May 1997 was a relatively "simple" storm and is well-suited to 
   combining, for example, ring current models and radiation belt models 
   to determine the magnitude and asymmetries of the "Dst effect" on 
   relativistic electrons.
2) October 2000 was added to the campaign studies. This is an 
   exceptionally good storm for comparing various measures of the ring 
   current through modeling, satellite observations, ENA observations, 
   and ground perturbation maps.
3) March-April 2001 was added to better understand the effects of 
  "superstorms" and extreme events.

All interested parties are encouraged to participate in these studies.

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