12 May 2009,
The member list was updated
10 October 2008,
Special Session of the 124th SGEPSS General Assembly(Finished)
A new phase of the upper atmospheric science based on the Antarctic Syowa MST/IS radar
21 May 2008,
Special Session of the 2008 MSJ Spring Meeting(Finished)
Possibility of the polar atmospheric research based on the Antarctic Syowa MST/IS radar
PANSY
PANSY
is a new plan to introduce the first
MST (Mesosphere-Stratosphere-Troposphere) /IS (Incoherent Scatter) radar, which is a VHF monostatic pulse Doppler radar, in the Antarctic to Syowa Station as an important station observing the earth's environment with the aim to catch the climate change signals that the Antarctic atmosphere shows. We call this radar the PANSY radar. The interaction of the neutral atmosphere with the ionosphere and magnetosphere as well as the global-scale atmospheric circulation including the low and middle latitude regions are also targets of PANSY.
Specifications of the PANSY Radar
| Radar System |
Monostatic pulse Doppler radar |
| Location |
Syowa Station in the Antarctic (69°00' 22''S, 39°35' 24''E) |
| Center Frequency |
47.0 MHz |
| Antenna |
A quasi-circular array consisting of 1045 crossed Yagi antennas with 3 elements |
| Aperture |
about 18000m2 |
| Beam directions |
arbitrary zenith angles less than 30 degrees |
| Transmitter |
1045 solid-state TR modules |
| Peak power |
> 500kW |
| Average power |
> 25kW |
| Polarization |
Circular polarization |
| Receiver |
55 systems of synchronous quadratic detection |
 |
The beam direction of the PANSY radar is easily controlled by changing the phase of radio waves emitted from each antenna element. The three dimensional structure of atmospheric phenomena can be examined.
|
Atmospheric Observation at Syowa Station
A strong advantage of Syowa Station is the possibility to use a variety of preinstalled observational tools measuring various aspects of the atmosphere. Vertical profiles of winds and temperature in the mesosphere and lower thermosphere are measured by an MF radar and a sodium lidar, respectively. Air glow measurements are made by an all sky imager and a Fabry-Perot interferometer. A micro-pulse lidar is used to detect clouds in the troposphere and lower stratosphere. Simultaneous observation by the PANSY radar as well as these instruments will promise significant progress of polar middle atmosphere science.
Observations in the Arctic Region
Each atmospheric layer is being observed by various radars in the Arctic. Comparative study of the Arctic and Antarctic atmosphere will be made possible by constructing the PANSY radar at Syowa Station.
Meridional Chain of MST/IS Radars