<div dir="ltr"><div><div><div>Dear Colleagues,<br><br></div><span><span>the IAGA meeting will be in Cape Town, South Africa from 27 August to 1
September
2017. </span></span>The IAGA abstract submission <b>deadline is on 12 March 2017.</b><br><span><span><br>We want to bring to your attention an across discipline session A39 “<b>Developing
and Using Realistic
External Source Models for imaging global
deep Earth conductivity
with Satellite and Ground-based Data”. </b>Please
consider submitting an abstract. The session description is attached below.<br><br></span></span></div><span><span>Sincerely,<br></span></span></div><span><span>The conveners </span></span><span><span style="color:black">(Gary Egbert, Astrid
Maute, Patrick Alken, Nils Olsen)<br></span></span><div><div><span><span><br>=============================================================<br></span></span><div><div><span><p style="text-align:justify;background-image:initial;background-position:initial;background-size:initial;background-repeat:initial;background-origin:initial;background-clip:initial"><span style="color:black">A39 - Developing and
Using Realistic
External Source Models for Imaging global
deep Earth conductivity
with Satellite and Ground-based Data (DIV VI
– DIV II – DIV
V)</span><br></p>
<p style="margin:0in 0in 15pt;text-align:justify;background-image:initial;background-position:initial;background-size:initial;background-repeat:initial;background-origin:initial;background-clip:initial"><span style="color:black">Recent developments in
EM induction
modeling and inversion, together with new
global geomagnetic
datasets (e.g., from the SWARM mission),
present exciting new
opportunities for imaging three-dimensional
electrical conductivity
variations in the mantle. Results from these
studies may ultimately
provide important new constraints on the
composition (e.g., water
content), physical state, and geodynamics of
the deep Earth.
Probably the greatest obstacle to success in
this endeavor is the
need to accurately characterize the
spatially complex external
source fields, which must be disentangled
from the induced internal
fields to image mantle conductivity
reliably. Observations of the
time-varying magnetic fields remain sparse,
making a direct
empirical separation very challenging. One
promising approach is to
make use of physics-based numerical models
of ionospheric and
magnetospheric current systems. These are
becoming increasingly
sophisticated, and may provide additional
constraints on source
geometries, and enable significant advances
in realistic modeling
of external sources. This symposium seeks to
bring the induction
and external source communities together, to
explore progress on
combining ground- and satellite-based
geomagnetic observations with
numerical models for improved separation,
characterization and
modeling of external source current systems
in the ionosphere and
magnetosphere.</span></p>
<p style="margin:0in 0in 15pt;text-align:justify;background-image:initial;background-position:initial;background-size:initial;background-repeat:initial;background-origin:initial;background-clip:initial;box-sizing:border-box"><span style="color:black">Contributions on
improving source models
for mantle induction studies are sought,
along with novel uses of
satellite and ground based data to validate
or improve models for
external source studies. We also welcome
contributions on other
aspects of global-scale studies of mantle
electrical conductivity,
including theoretical or methodological
developments, and results
based on analysis of data from ongoing or
past satellite magnetic
missions, as well as ground based arrays.</span></p></span></div></div></div></div></div>