Multi-instrument observations of plasma features in the Arctic ionosphere during the main phase of a geomagnetic storm in December 2006

• Published in: Journal of atmospheric and solar-terrestrial physics Vol. 105-106; pp. 358 - 366
• Main Authors: Wu, Ye-wen, Liu, Rui-yuan, Zhang, Bei-chen, Wu, Zhen-sen, Hu, Hong-qiao, Zhang, Shun-rong, Zhang, Qing-he, Liu, Jun-ming, Honary, F.
• Format: Journal Article
• Language: English
• Published: Elsevier Ltd 01.12.2013
• Subjects: Arctic ionosphere; Electron density; Magnetic storm; Sub-storm; Total electron content; Magnetic storm; Total electron content; Electron density; Sub-storm; Arctic ionosphere
• ISSN: 1364-6826; 1879-1824
• DOI: 10.1016/j.jastp.2013.07.004

Arctic ionospheric variations during the main phase of a magnetic storm on 14–15 December, 2006 were investigated to characterize the high energy particle precipitation caused effects, based on multi-instrument observations. These include electron density observations provided by the Global Positioning System (GPS) total electron content (TEC) measurements, European Incoherent Scatter (EISCAT) radar, the radio occultation (RO) from both the CHAMP satellite and the Constellation Observing System for Meteorology, Ionosphere, and Climate (COSMIC) satellite, as well as the ionospheric absorption of cosmic radio noise measured by the Imaging Riometer for Ionospheric Studies (IRIS) at Kilpisjärvi in the northern Finland (69.05°N, 20.79°E). Significant increases in the electron density for these different observations were found in the Arctic ionosphere during the main phase of the magnetic storm. These increase occurred in Scandinavian, Northwest part of Russia and Svalbard (SNRS) region, primarily at an altitude of about 110km. These results are first reported for the SNRS region, and our study contributes to a more complete description of this space weather event during 14–15 December, 2006. Our observations also provide direct evidence that the stormtime E-layer electron density enhancement (e.g., the sporadic E) can form a nearly dominant portion in the observed TEC increase. These increases were accompanied by the ionospheric absorption enhancement at the altitude of about 90km. The Y-component of magnetic field to the south of SNRS decreased, indicating strong upward field aligned electric current in the Arctic ionosphere. These features are interpreted as the effect of the high energy electron precipitation during the magnetic storm, which is caused by the sub-storm reflected on AL index and the measurements of IMAGE (International Monitor for Auroral Geomagnetic Effects) chain. The average energy of the precipitation electrons reached to about 10keV and the boundary of the high energy electron precipitation was also found to move poleward with a speed of about 800m/s. •The results are the complement of other studies for the same event.•TEC in the E-layer (∼50%) is important for the positive ionospheric storm.•This work showed the 3-D plasma features in Arctic ionosphere during magnetic storm.•The electron temperature in F-layer and absorption of cosmic noise enhanced together.•Polar boundary of the electron precipitation moved poleward with the speed of 800m/s.