![]() |
The POLAR
|
POLAR is the second mission of NASA's Global Geospace Science (GGS) initiative to study the dynamics of the magnetosphere. With 11 instruments on board, POLAR is designed to measure energy input to the Earth's polar regions. It provides global images of the aurora, as well as particle measurements of solar wind entering the magnetosphere and ionospheric plasma flowing out. Additional information about the POLAR mission and the International Solar-Terrestrial Physics Science Initiative is on-line at Goddard Space Flight Center. For current mission status, see the Mission Operations Home Page for POLAR and WIND. |
![]()
Artist's concept of the POLAR spacecraft. |
The University of Washington's research is based primarily upon data from the Ultraviolet Imager (UVI). (See below). Extensive documentation on UVI is also available at the Marshall Space Flight Center UVI home page. | ![]()
Schematic of POLAR's instrumentation. |
![]()
|
Background: The aurorae are the result of collisions between the
atmosphere and energetic particles which have their origin in the solar
wind, and which reach the atmosphere after being accelerated and
redistributed within the Earth's magnetosphere. The global-scale
phenomenon represented by the aurorae therefore contains considerable
information concerning the solar-terrestrial connection. For example,
by correctly measuring specific auroral emissions, and using
comprehensive models of the region, we can infer the total energy flux
entering the atmosphere and the average energy of the particles
causing these emissions. Furthermore, from these auroral emissions we
can model the ionospheric conductances that contribute to the closing
of magnetospheric currents through the ionosphere, and from these we
can obtain the electric potentials and convective patterns that are an
essential aspect of the interaction between the ionosphere,
thermosphere, and mesosphere. Simultaneous images of the auroral oval
and polar cap not only yield the temporal and spatial morphology from
which we can infer activity indices, they also allow the comparison of
parts of the oval with measurements made by other spacecraft of source
regions in the magnetosphere.
|
The POLAR Spacecraft Experiment / Updated 13 October 1999 / britt@geophys.washington.edu