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Some progress on linking together models Nick Achilleos Lecturer, Department of Physics University College London With thanks to Patrick Guio and Dugan Witherick – PowerPoint PPT presentation

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Title: Some progress on


1
Some progress on linking together models
  • Nick Achilleos
  • Lecturer, Department of Physics
  • University College London
  • With thanks to Patrick Guio and Dugan Witherick

2
  • Report from UCL
  • We have been pursuing activities which may
    produce some useful demonstrators and
    deliverables for the JRA3 Distributed Modelling
    Laboratory.
  • Modelling auroral dynamics at Jupiter (PhD
    project by J. N. Yates)
  • Coupling UCL Jovian magnetodisc model with a
    model of plasma flow (Achilleos, Guio)
  • Other possibilities ?

3
Auroral Dynamics at Jupiter
  • Model 1
  • - The UCL global, axisymmetric model of Jupiters
    thermosphere and ionosphere (e.g. Smith and
    Aylward, Ann. Geo., 2009).
  • Solves equations of fluid flow for the neutral
    thermosphere.
  • Needs an algorithm for computing ionospheric
    current, esp. in the auroral region.
  • Uses Model 2 the theoretical profile by Grodent
    and Gerard (JGR 2001) for auroral ionosphere
    (ion density versus altitude)

4
Model Linkage
  • Architecture Auroral profile is built into a
    subroutine of UCL code

UCL model reads auroral profile as a template
for auroral ionosphere
The ion density profile is scaled at all
altitudes by the same factor, according to the
conductance properties calculated by the disc
dynamics routine - gives plasma rotation rate and
corresponding M-I currents.
5
  • For more information, see paper submitted to PSS
    by Yates, Achilleos and Guio (2010, arxiv)
  • Grodent / Gerard profile (ascii files?) may be
    added to JRA3 Catalogue
  • We need more 1D theoretical profiles of auroral
    structure so that we may use the UCL Jovian and
    Kronian models as a testbed - this should be
    emphasised as a useful goal of the DNML.
  • Note also the work of Nicholson et al (MNRAS
    2009) on precipitation at Mars, UCL are working
    on taking this further to a coupled model of
    Martian thermosphere and aurora.

6
Giant Planet Magnetospheres
  • Example 1 UCL Magnetodisc model
  • What is it ? A model which calculates
    self-consistent magnetic field structure and
    plasma distributions for a disc-like,
    axisymmetric, rotating magnetosphere. Used for
    studies of magnetospheric structure at Saturn and
    Jupiter (giant rapid rotators) e.g. Achilleos,
    Guio and Arridge (MNRAS, 2010), Achilleos et al
    (GRL, 2010)

7
  • Present disc model assumes a fixed profile of
    plasma rotation (angular velocity ?M) versus
    radial distance.
  • New configuration couples disc B-field model to
    an independent solver of plasma ?M

B Field Profile in Plasmadisc
?M Solver
UCL Magnetodisc Model
?M profile needed to update force balance,
re-compute B Field
8
  • New configuration links two independent Matlab
    codes on different nodes in a local network
    through a simple Java class using IP Sockets.
  • We could do a similar exercise for the
    magnetopause field model - at present we use
    average value from the formulae of Alexeev et al
    (Ann. Geo. 2005) (Catalogue entry ?)

B Field Profile in Plasmadisc
?M Solver
UCL Magnetodisc Model
?M profile needed to update force balance,
re-compute B Field
9
  • A reminder of what JRA3 activities may foster in
    the long term
  • My feeling is that these are beyond the scope of
    Europlanet (not enough resource) but they may
    indicate where we are headed if we follow some
    of the more simple ideas.
  • Example A A time-dependent MHD model of Jovian
    or Kronian plasmadisc to couple to the
    appropriate atmospheric GCMs, to study transient
    auroral response.
  • Example B A time- and space-dependent model of
    auroral precipitation associated with the
    Io-Jupiter current circuit, to investigate the
    nature of wind systems driven by such a localised
    source of auroral energy input.

10
  • Progress on Catalogue-Linked Web Apps
  • These are
  • The H3 cooling function calculator (code from S.
    Miller) JRA3T3
  • The VoiSe image segmentation tool (code from P.
    Guio) JRA3T4
  • Web apps migrated to new webserver (beginning
    2011) and are now live at
  • http//astroweb.projects.phys.ucl.ac.uk/europlanet
    jra3/
  • Entries for these web apps have been update on
    the JRA3 catalogue.

11
Process diagram for each web app
Process Job
User
Results/Notification by Email
Input files?
Input parameters
Job details
Results?
Queue Job
Validate Parameters
Jobs
Job details
Job details
12
  • Technologies used for Web Apps
  • Web Interface and Parameter Validation
  • Django web framework for Python
  • Job Queuing System/Broker
  • RabbitMQ Advanced Message Queuing Protocol (AMQP)
    compliant message queuing system
  • Job Processing
  • Django-Celery asynchronous task queue/job queue.
  • Database for Job Detail Storage
  • MySQL

13
  • Upcoming Web Apps
  • MarTIM
  • Mars Thermosphere and Ionosphere Model
  • 3D general circulation model of the Martian
    middle and upper atmosphere from 0.883 to
    9.910-8 Pa.
  • Developed by Will Nicholson
  • Possible coupling to TransMars
  • UCL Magnetodisc Model
  • Described earlier
  • A library of disc model outputs for community use
    to be placed in the Catalog.

14
  • Next steps?
  • Action for all JRA3 Modellers Whose work is
    relevant to what you are trying to achieve ? Are
    they in the catalog - would they be willing to
    have an entry in the catalog ?
  • The examples shown here illustrate the need in
    some areas of planetary science for progress by
    coupling models, even at a very basic level -
    e.g. GCMs as testbeds for auroral profiles
  • There may also be a possibility that we could
    provide force-balance models for theoretical
    models of exoplanet discs (e.g. work by
    Khodachenko et al)
  • Keep it simple, keep it realistic, make it a part
    of what you would naturally want to do in your
    own research programme
  • From our meetings, it is clearer that IDIS
    ideally would provide a variety of databases
    which, in principle, could be queried from a
    system like the one described herein - keep this
    in mind, and keep informed of IDIS progress.
    (Note IDIS general meeting in Rome, June 7)
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