Physics Dept
Seminar
April 10, Monday
Modelling to Support High
Latitude Radio Propagation Studies:
How Far Can Empirical
Methods Take Us?
Dr. David Themens
University
of Birmingham, U.K
(Terrestrial
Physics, Host: Perry)
Time: 11:45 am - 12:45 pm with 11:30 am teatime
Room: ECE 202
The plasma in the upper atmosphere, called the
ionosphere, has the unique property of being a highly refractive medium for
electromagnetic signals in the High Frequency (HF) band (3–30 MHz). This
property allows one to use the ionosphere as a reflector for signals in this
band, enabling long range (1000s of km) communications, as well as enabling
long-range remote sensing systems, like Over-the-horizon Radar (OTHR). Due to
the dependence of these systems on the ionosphere, however, they are heavily
reliant on our capacity to model the ionosphere that their signals propagate
through. At mid latitudes, climatological models, like the International
Reference Ionosphere, are generally reliable and can be used under most quiet
conditions; however, at high latitudes, where the ionosphere is heavily driven
by external forcing from the magnetosphere and solar wind above, as well as the
atmosphere below, ionospheric models have traditionally performed quite poorly
and cannot be used to support operational systems, like OTHR. To mitigate this
issue, we have developed the Empirical Canadian High Arctic Ionospheric Model
(E-CHAIM) to prescribe the climatological state of the ionosphere. To further
capture ionospheric weather, an advanced data assimilation system (A-CHAIM) was
later integrated into E-CHAIM, and semi-physical modules have been developed to
integrate additional phenomena, including auroral particle precipitation and
solar energetic proton precipitation. In this talk, we will examine the effects
of various high latitude ionospheric dynamics on HF radio propagation at high
latitudes, spanning their impact on the absorption of these signals and on
scientific and operational radar systems, such as the Super Dual Auroral Radar
Network (SuperDARN).