TY - JOUR
T1 - Polar cap ionosphere and thermosphere during the solar minimum period
T2 - EISCAT Svalbard radar observations and GCM simulations
AU - Fujiwara, Hitoshi
AU - Nozawa, Satonori
AU - Maeda, Sawako
AU - Ogawa, Yasunobu
AU - Miyoshi, Yasunobu
AU - Jin, Hidekatsu
AU - Shinagawa, Hiroyuki
AU - Terada, Kaori
N1 - Funding Information:
Acknowledgments. We thank the staff of EISCAT for operating the facilities. EISCAT is an international association supported by research organizations in China, Finland, Germany, Japan, Norway, Sweden, and the United Kingdom. This work was supported in part by Grant-in-Aid for Scientific Research C and B (20540435, 23340144, 23340149) and Scientific Research on Innovative Areas (20200047), and the Global COE program “Global Education and Research Center for Earth and Planetary Dynamics” at Tohoku University by the Ministry of Education, Science, Sports and Culture, Japan. A part of this work was also supported by the joint research programs of the Solar-Terrestrial Environment Laboratory, Nagoya University and the National Institute of Polar Research, Japan. The empirical models of NRLMSISE-00, IRI 2007, and the solar indices, are provided from NASA/NSSDC, web of NASA/GSFC, and NOAA/NGDC, respectively.
PY - 2012
Y1 - 2012
N2 - The IPY long-run data were obtained from the European Incoherent Scatter Svalbard radar (ESR) observations during March 2007 and February 2008. Since the solar and geomagnetic activities were quite low during the period, this data set is extremely helpful for describing the basic states (ground states) of the thermosphere and ionosphere in the polar cap region. The monthly-averaged ion temperatures for 12 months show similar local time (or UT) variations to each other. The ion temperatures also show significant seasonal variations. The amplitudes of the local time and seasonal variations observed are much larger than the ones predicted by the IRI-2007 model. In addition, we performed numerical simulations with a general circulation model (GCM), which covers all the atmospheric regions, to investigate variations of the neutrals in the polar thermosphere. The GCM simulations show significant variations of the neutral temperature in the polar region in comparison with the NRLMSISE-00 empirical model. These results indicate that both the ions and neutrals would show larger variations than those described by the empirical models, suggesting significant heat sources in the polar cap region even under solar minimum and geomagnetically quiet conditions.
AB - The IPY long-run data were obtained from the European Incoherent Scatter Svalbard radar (ESR) observations during March 2007 and February 2008. Since the solar and geomagnetic activities were quite low during the period, this data set is extremely helpful for describing the basic states (ground states) of the thermosphere and ionosphere in the polar cap region. The monthly-averaged ion temperatures for 12 months show similar local time (or UT) variations to each other. The ion temperatures also show significant seasonal variations. The amplitudes of the local time and seasonal variations observed are much larger than the ones predicted by the IRI-2007 model. In addition, we performed numerical simulations with a general circulation model (GCM), which covers all the atmospheric regions, to investigate variations of the neutrals in the polar thermosphere. The GCM simulations show significant variations of the neutral temperature in the polar region in comparison with the NRLMSISE-00 empirical model. These results indicate that both the ions and neutrals would show larger variations than those described by the empirical models, suggesting significant heat sources in the polar cap region even under solar minimum and geomagnetically quiet conditions.
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U2 - 10.5047/eps.2011.05.023
DO - 10.5047/eps.2011.05.023
M3 - Article
AN - SCOPUS:84876387118
SN - 1343-8832
VL - 64
SP - 459
EP - 465
JO - Earth, Planets and Space
JF - Earth, Planets and Space
IS - 6
ER -