The Dual Auroral Radar Network (DARN) is a global-scale network of I-I
F and VHF radars capable of sensing backscatter from ionospheric irreg
ularities in the E and F-regions of the high-latitude ionosphere. Curr
ently, the network consists of the STARE VHF radar system in northern
Scandinavia, a northern-hemisphere, longitudinal chain of HF radars th
at is funded to extend from Saskatoon, Canada to central Finland, and
a southern-hemisphere chain that is funded to include Halley Station,
SANAE and Syowa Station in Antarctica. When all of the HF radars have
been completed they will operate in pairs with common viewing areas so
that the Doppler information contained in the backscattered signals m
ay be combined to yield maps of high-latitude plasma convection and th
e convection electric field. In this paper, the evolution of DARN and
particularly the development of its SuperDARN HF radar element is disc
ussed. The DARN/SuperDARN network is particularly suited to studies of
large-scale dynamical processes in the magnetosphere-ionosphere syste
m, such as the evolution of the global configuration of the convection
electric field under changing IMF conditions and the development and
global extent of large-scale Mi-ID waves in the magnetosphere-ionosphe
re cavity. A description of the HF radars within SuperDARN is given al
ong with an overview of their existing and intended locations, intende
d start of operations, Principal Investigators, and sponsoring agencie
s. Finally, the operation of the DARN experiment within ISTP/GGS, the
availability of data, and the form and availability of the Key Paramet
er files is discussed.