Subauroral polarization streams: observations with the Hokkaido and King Salmon SuperDARN radars and modeling
Subauroral polarization streams: observations with the Hokkaido and King Salmon SuperDARN radars and modeling
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DOI:
10.5194/angeo-26-3317-2008
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发表时间:
2008-10
影响因子:
1.9
通讯作者:
A. Koustov;N. Nishitani;Y. Ebihara;T. Kikuchi;M. Hairston;D. André
中科院分区:
文献类型:
--
作者:
A. Koustov;N. Nishitani;Y. Ebihara;T. Kikuchi;M. Hairston;D. André
The newly installed SuperDARN Hokkaido HF radar monitors ionospheric plasma flow between magnetic latitudes of 45 and 65 and thus has a great potential for studies of subauroral polarization streams (SAPS) in com- bination with another SuperDARN radar located at King Salmon, Alaska as well as the DMSP satellites and ground- based instruments in the Alaskan sector of the Arctic. Pre- liminary survey shows that although SAPS are often detected with the Hokkaido radar, their velocities are rather low, to the order of 150 m/s in its most suitable central beams. In this study, observations of unusually fast Hokkaido flows of up to 800 m/s are presented. The event of 1 April 2007 is inves- tigated in detail. It is shown that high-velocity echoes appear after substorm onsets over North America with a delay of 30 min. In terms of latitude, the velocity peaks just outside the auroral oval; signatures of a detached polarization jet are occasional and not pronounced. The King Salmon radar op- erating concurrently detects SAPS signatures as well but at different times and locations. Simulation with the Compre- hensive Ring Current Model for the 1 April event reasonably identifies the period of fast flow occurrence but the velocity is underestimated. The event studied suggests that substorm- injected particle populations may intensify the pre-existing SAPS flow and lead to a mismatch of the predictions and observations.