

			 ***************************
			 **   THE GEM MESSENGER   **
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						     Volume 6, Number 46
						     September 27, 1996

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Report on GGCM Campaign Activities at the GEM Snowmass Workshop, June, 1996
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From wolf at alfven.rice.edu Fri Sep 27 08:31:56 1996

This Workshop marked a transition in leadership of the Geospace General
Circulation Model (GGCM) Campaign.  George Siscoe and Joel Fedder, who
conceived and founded the GGCM effort within GEM, led it through a period
when it was "Working Group 5" in the GEM structure and through its
transition to a full GEM campaign, are retiring from the official
leadership positions, although they may be expected to continue to play
active roles informally.  Dick Wolf and Michael Hesse will succeed them as
Coordinators of the GGCM Campaign.

The GGCM-centered sessions were the following:
Monday, 6/24, 10:30 am-12:00 noon.  GGCM Planning Session.
Monday, 6/24, 1:30-3:00 pm.  Space Weather Session.
Monday, 6/24, 3:30-5:00 pm.  GGCM Science Session.
Tuesday, 6/25, 8:00 am - 12:00 noon.  Joint BL/GGCM "Modeler Challenge" Session.
Tuesday, 6/25, 7:30-9:30pm.  Continuation of GGCM Planning Session.

All of these sessions are summarized below, except for the Tuesday-morning
joint session, which is covered in the summary of the Boundary-Layer
Campaign.


GGCM PLANNING SESSIONS (Dick Wolf, chair)

In the final talk of the Plenary Session Monday morning, Dick Wolf
described his perception of how the concept of the Geospace General
Circulation Model had evolved, from the original formulation of GEM to the
present.  He discussed the special features of the GGCM concept that
distinguish it from other global magnetospheric models.  One defining
characteristic of the GGCM that was established early in its history was
that it would be a modular code, with different approaches used for
different regimes of geospace.  The modular concept, however, can be
interpreted either in a strict sense -- with different codes handling
different regions and boundary-condition information passed between
them--or in the looser sense of different subroutine packages computing
different parameters in different regions.  Much of the GGCM-directed
research activity in the last few years has been in beginning to develop
and couple modules representing different regions and/or parameters.  Wolf
raised the issue of whether the research had progressed to the point where
it was time to begin actually building the GGCM code, defining and building
the individual modules as well as the logical structure that would connect
them.  In his prepared talk, he suggested that the time might not be right
for this development, but, in the heated discussion that followed, it
quickly became clear that there was strong sentiment of the GEM community
for the fastest possible development of the GGCM.  Important factors in the
perceived urgency were the advent of the National Space Weather Program and
the practical need for rapid improvement in forecasts of space weather.

Discussion of GGCM planning issues continued through the scheduled Monday
morning GGCM planning session and into an additional session Tuesday
evening.  It was clear that there is a need for a global model that can be
widely used by the GEM community to help answer the scientific questions
that face magnetospheric physics.  One central and contentious issue that
arose in the discussions was whether the GGCM should be modular in the
strict sense (as defined in the previous paragraph) or should be based on a
global MHD code, with program modules correcting or supplementing MHD for
various parameters and various regions.  Proponents of each side presented
their cases at the Tuesday night session.  However, after vigorous debate,
the majority of those assembled voted to leave the technical decision of
basic code design to the proposal-review process.

Dick Wolf agreed to assemble a committee to draft a GGCM announcement that
would reflect the majority sentiments expressed in the discussions and that
people could reference in writing GEM proposals.  That committee, which
consisted of Jim Drake, Mike Heinemann, Michael Hesse (Co-Chair), John
Lyon, Nelson Maynard, George Siscoe, and Dick Wolf (Chair), completed its
writing assignment on the required tight time schedule. At the end of July,
a draft "Plan for the Development of a Geospace General Circulation Model"
was placed on the Web for consideration by the GEM community.  A second
draft, containing revisions made in response to community comments, was
forwarded to the GEM Steering Committee in early September, and it has been
endorsed by that Committee.  The development plan recommends that the first
round of GGCM-development proposals be submitted for the October 1996
GEM solicitation; these proposals would be for short-term concept studies,
which would seek to define the computational structure of the GGCM program
as well as the institutional structure in which it would be operated and
made available to the community.  The current version of the Plan can be
accessed via the World-Wide Web through the GEM homepage or at the
following address:
http://jimme.gsfc.nasa.gov/~hesse/GGCM_plan.html


SPACE WEATHER SESSION (George Siscoe, chair)

For the last several years, the GGCM Campaign has acted as the bridge
between the GEM scientific community and the community that is concerned
with providing practical forecasts of space weather.  Although the focus of
that interaction has been in January workshops that have been held in
Boulder, this session, which was chaired by George Siscoe, was designed to
update the GEM science community at large on activity in the forecasting
community.

Kent Doggett, who is a forecaster at NOAA's Space Environment Center in
Boulder, reported on the Workshop on the Evaluation of Space Weather
Forecasts, which was held in previous week in Boulder.  This Workshop
brought together space scientists, space-weather forecasters, users of
space forecasts, and some representatives of the terrestrial-weather
forecast community to discuss techniques for systematically evaluating the
effectiveness of forecasts.

A report on Air Force space weather operations was presented Captain Dave
Hembroff, who is a shift commander at the 50th Weather Squadron at Falcon
Air Force Base outside Colorado Springs. He reported that new hardware
installation of the Magnetospheric Specification Model allows completion of
a three-hour run in a few minutes.  He summarized the existing
space-weather prediction and specification capabilities and the usefulness
for customers.  He mentioned one satellite-operations customer who was
finding that 50WS predictions of activity levels allowed him to make an
immediate judgement on whether a given anomaly was environmental in nature
-- a major advantage, because the procedure for turning the spacecraft on
again after an anomaly is much simpler if the problem is environmental.

Howard Singer, of the NOAA Space Environment Center, reported on SEC
approaches to improved space weather forcasting.  He showed encouraging
results of a new algorithm for predicting Ap 3-6 days ahead of time using
solar observations.  He discussed a proposal for establishing a rapid
prototyping center for implementing space weather models.

Phil Pratt of the TRW Systems Integration Group described a general
computing environment that TRW has developed to facilitate rapid
prototyping of models.  Transitioning space models to operations has, in
the past, sometimes proved to be expensive, time-consuming, and cumbersome.
Pratt suggests that this TRW-developed computing environment, which was
developed to be useful in a range of applications, could make it easy for a
forecast center to implement and test a space-weather model.


GGCM SCIENCE SESSION (Michael Hesse, chair)

For the last several years, the GGCM science sessions at the June GEM
Workshops have served several purposes.  They have provided a forum for the
planning of, and progress reports on, projects related to development and
coupling of computational modules designed to be part of the GGCM.  They
have also served as an annual scientific meeting for people involved in
large-scale magnetospheric theory and modeling and in the theory and
modeling of those crucial small-scale processes that affect large-scale
dynamics.  This year's science session continued in the same tradition.

Kolya Tsyganenko presented a scientific talk at the end of the Space
Weather Session due to time constraints.  He described the latest advance
in his magnetic-field-modeling effort, which rests on a large database of
spacecraft-measured magnetic fields.  His newest models have a well-defined
magnetopause and include a data-based prescription for the penetration of
the magnetosheath magnetic field through the boundary, as a function of
IMF.  The latest model is available on the World-Wide Web.

Richard Thorne summarized recent work that he has done in collaboration
with V. K. Jordanova, R. B. Horne, and Janet Kozyra, calculating ion
precipitation rates of ring-current ions by pitch-angle scattering.  They
are pursuing a very interesting approach to self-consistently representing
the effects of small-scale plasma processes in a large-scale computer model
of the ring current.  Specifically, they utilize the
Ring-Current/Atmosphere Interaction Model (RAM) to calculate the particle
distribution function for ring-current ions and use that distribution
function to calculate linear growth rates for electromagnetic ion cyclotron
waves.  Then they use the HOTRAY code to follow packets of electromagnetic
wave packets through the inner magnetosphere, and calculate the time
integral of the linear growth rate.  From that, they derive a rough
approximation to the wave amplitude and the pitch-angle scattering rate,
which is then used in the RAM code to calculate the pitch-angle
distribution.

W. B. Lyatsky presented a new theoretical interpretation of the
down-up-down average observed pattern of Birkeland currents in the midnight
sector.  He proposes that these currents result from the fact that ions
have much more difficulty than electrons in making a sharp turn in the
convection pattern - the turn that is implied by the ionospheric electric
field pattern near the Harang discontinuity.  He suggests that
plasma-sheetions and electrons tend to separate in this region, and that
the Birkeland currents are required to maintain approximate charge
neutrality.  Dr. Lyatsky presented a detailed theoretical analysis of this
process and its magnetospheric and auroral effects.

Harlan Spence reported on an effort at building comprehensive empirical
models of the ring current and inner magnetosphere particles and fields.
These models combine SCATHA, CRRES, POLAR, and other datasets.  The SCATHA
dataset is now available online.  POLAR crosses the equatorial plane near
the peak of the ring-current and provides very valuable information on
ring-current dynamics and three dimensional structure of the inner
magnetosphere.  The synthesized data sets are being sorted by location and
geomagnetic "phase" and will provide the core for future semi-empirical
models.

Frank Cheng reported on recent progress in his effort at theoretical
calculation of 3D equilibrium magnetospheric configurations, for a
magnetospheric plasma with isotropic pressure.  He has developed a 3D
quasi-static magnetospheric equilibrium code, the MAG-3D code, which makes
use of a new, accurate and efficient numerical procedure based on a flux
coordinate system.  Employing radial pressure profiles from previous
satellite measurements Cheng showed a variety of computed 3D equilibrium
configurations for the ring current and inner plasma sheet for both quiet
and disturbed times.  The Region 2 field-aligned current is shown to be
related to the azimuthal magnetic field curvature and plasma pressure
gradient.  The computed Region 2 field-aligned current is consistent with
previous satellite measurements of Iijima and Potemra.

Joachim Birn reported briefly on the status of the GEM project to couple
the Birn/Hesse tail MHD code with the Rice Convection Model (RCM), using a
frictional version of the MHD code that Frank Toffoletto has developed to
calculate magnetic equilibria in the RCM's inner-magnetospheric region. The
RCM is working effectively with the friction code, but coupling to the tail
has not been completed.  Birn also reported on some very interesting
theoretical results obtained by embedding a particle tracer inside the
tail-MHD code; fluxes calculated from Liouville's theorem seem consistent
with general observed characteristics of substorm injections at
geosynchronous orbit.

Frank Toffoletto reported on progress on a GEM project that involves a
collaboration between the Rice group and John Lyon at Dartmouth.  It
centers on embedding the Rice Convection Model inside a global MHD code.
Graduate student Michikazu Hojo has completed several RCM runs with plasma
and potential boundary conditions and the plasma initial condition taken
from a case where the Fedder-Lyon MHD code had reached an approximate
steady state.  When the RCM is run in the ideal-MHD approximation ( E + vxB
= 0), the electric field, plasma distribution, and Birkeland current
distribution all change substantially during the RCM run.  Region-2
Birkeland currents strengthen, effectively shielding the near-Earth region
from the convection electric field.

Harry Petschek presented a new physical picture of the growth phase of a
substorm. In his picture, reconnection at the dayside magnetopause causes
plasma loss and sets up a convection from the nightside to the dayside. The
plasma transport thus constitutes a plasma loss from the plasma sheet,
which can lead to thinning and subsequently substorm onset. Another way of
looking at his scenario is: Imagine that reconnection occurs at the dayside
magnetopause, so there is an electric field in the +y direction there.  If
the electric field is zero or negligible across the tail at x=x1 and along
the magnetopause on the flanks, then Faraday's law implies that Bz
decreases sunward of x1.  Petschek suggests that this mechanism drives Bz
to zero in the inner plasma sheet, triggering the onset of the expansion
phase.

The talks presented in the GGCM science session illustrate how large-scale
magnetospheric is moving into an exciting new era, characterized by new
ideas and new data.  Semi-empirical models continue to improve in
sophistication and usefulness.  Theoretical models that were developed by
different teams for different purposes are now being coupled, to allow
investigation of cause-and-effect relationships between different
magnetospheric regions and also between plasma processes with very
different scale sizes.




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