Mahmut Onur KARSLIOĞLU Hocamızdan aldığım iletiyi sizlerle paylaşıyorum.
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Dear colleagues,
we would like to draw your attention to our session
G5.1 Monitoring and modelling of the ionosphere from space-geodetic techniques
at the European Geosciences Union (EGU) General Assembly 2013 (7-12 April 2013, Vienna, Austria) and call for contributions.
The
relation between space geodetic measurements and ionosphere models is
twofold: (1) the geodetic measurements can be evaluated to derive
parameters of physical, empirical or analytical ionosphere models and
(2)
models are used to correct the electromagnetic signals for the
ionospheric effects. The potential for ionospheric sensing from space
geodetic techniques has improved considerably over the last few years as
a result of technological advances, larger ground networks and
developments of appropriate models and algorithms. Accurate ionospheric
estimates and retrievals based on these techniques may significantly
improve our understanding on the physical and dynamic characteristics of
electron density and space weather at various scales.
We
invite contributions on physical modeling of the ionosphere. Recent
sounding results, report on achieved improvements of the accuracy and of
the spatio-temporal resolution of derived ionospheric parameters as
well as theoretical studies that assess requirements for the accuracy of
relevant parameters are also welcome.
More
information on this session as well as on details concerning abstract
submission and possibilities for financial support of young scientists
can be found on the following web site:
The abstract submission deadline is January 9, 2013!
And, of course, we would appreciate, if you could circulate this email to colleagues who might be interested.
Many thanks,
Michael Schmidt, Mahmut Onur Karslioglu, Andrzej Krankowski, Denise Dettmering
(Conveners)
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Session abstract:
The
relation between space geodetic measurements and ionosphere models is
twofold: (1) the geodetic measurements can be evaluated to derive
parameters of physical, empirical or analytical ionosphere models and
(2) models are used to correct the electromagnetic signals for the
ionospheric effects. In other words ionospheric signals such as electron
density or vertical total electron content are either the target
functions or interpreted as disturbing signals.
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