Bibliography
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Found 24 entries in the Bibliography.
Showing entries from 1 through 24
2022 |
Validation of in-situ ionospheric density using FORMOSAT-7/COSMIC-2 IVM and ICON IVM We investigate the validation of in-situ ion density measurements by the ion velocity meter (IVM) onboard F7/C2 and ICON, respectively, during the solar minimum condition of Choi, Jong-Min; Lin, Charles; Rajesh, PK; Park, Jaeheung; Kwak, Young-Sil; Chen, Shih-Ping; Lin, Jia-Ting; Published by: Published on: YEAR: 2022   DOI: 10.21203/rs.3.rs-1758637/v1 |
Hong, Junseok; Kil, Hyosub; Lee, Woo; Kwak, Young-Sil; Choi, Byung-Kyu; Paxton, Larry; Published by: Published on: |
2019 |
Assimilation of Multiple Data Types to a Regional Ionosphere Model With a 3D-Var Algorithm (IDA4D) For the purpose of building a regional (bound 20\textendash60\textdegreeN in latitude and 110\textendash160\textdegreeE in longitude) ionospheric nowcast model, we investigated the performance of IDA4D (Ionospheric Data Assimilation Four-Dimension) technique considering International Reference Ionosphere model as the background. The data utilized in assimilation were slant total electron content (STEC) from 27 ground GPS (Global Positioning System) receiver stations and NmF2 (ionospheric F2 peak density) from five ionosondes and COSMIC (Constellation Observing System for Meteorology, Ionosphere, and Climate) Data Analysis Archive Center. The period analyzed covered both geomagnetic quiet and disturbed days (15\textendash18 March 2015). Assimilations were run under the following data combinations (cases): (1) GPS-STEC\textquoterights only; (2) GPS-STEC\textquoterights and NmF2\textquoterights from five ionosondes; (3) only NmF2\textquoterights from five ionosondes; and (4) GPS-STEC\textquoterights and NmF2\textquoterights from both five ionosondes and COSMIC. Results showed that under case 1 the root-mean-square error (RMSE) in STEC reduced by 44\% over the background International Reference Ionosphere values and on averaged over all ionosonde stations in the analysis RMSE values of foF2 (F2 layer critical frequency) reduced by 21\%. Furthermore, foF2 RMSE values under Case 2 were 36\% smaller than those under Case 1. Under Case 4, IDA4D performance improved even further in areas not covered by GPS and ionosonde measurements. Therefore, IDA4D is a potential candidate for regional ionosphere modeling that exhibits improved performance with assimilation of different data types. Mengist, Chalachew; Ssessanga, Nicholas; Jeong, Se-Heon; Kim, Jeong-Heon; Kim, Yong; Kwak, Young-Sil; Published by: Space Weather Published on: 06/2019 YEAR: 2019   DOI: 10.1029/2019SW002159 |
2015 |
Morphology of the postsunset vortex in the equatorial ionospheric plasma drift Lee, Woo; Kil, Hyosub; Kwak, Young-Sil; Paxton, Larry; Published by: Geophysical Research Letters Published on: |
2014 |
Investigation of the Tidal Signatures in the Thermosphere Using the TIMED/GUVI Data Kil, Hyosub; Paxton, Larry; Zhang, Yongliang; Kwak, Young-Sil; Lee, Woo; Published by: Published on: |
The role of the postsunset vortex in the creation of turbulence in the bottomside F region Lee, Woo; Kil, Hyosub; Kwak, Young-Sil; Paxton, Larry; Published by: Published on: |
The zonal motion of equatorial plasma bubbles relative to the background ionosphere Kil, Hyosub; Lee, Woo; Kwak, Young-Sil; Zhang, Yongliang; Paxton, Larry; Milla, Marco; Published by: Journal of Geophysical Research: Space Physics Published on: |
The zonal motion of equatorial plasma bubbles relative to the background ionosphere Kil, Hyosub; Lee, Woo; Kwak, Young-Sil; Zhang, Yongliang; Paxton, Larry; Milla, Marco; Published by: Journal of Geophysical Research: Space Physics Published on: |
Equatorial broad plasma depletions associated with the enhanced fountain effect Lee, Woo; Kil, Hyosub; Kwak, Young-Sil; Paxton, Larry; Zhang, Yongliang; Galkin, Ivan; Batista, Inez; Published by: Journal of Geophysical Research: Space Physics Published on: |
2013 |
The Study of the origin of broad plasma depletions in the equatorial F region Oh, S; Lee, W; Kil, H; Kwak, Y; Paxton, L; Zhang, Y; Published by: Published on: |
Drivers of the hemispheric asymmetry in the low-latitude electron density distribution Kil, H; Kwak, Y; Lee, W; Paxton, L; Zhang, Y; Published by: Published on: |
Seasonal and Latitudinal Variations of the F2-Layer during Magnetic Storms Park, Yoon-Kyung; Kwak, Young-Sil; Ahn, Byung-Ho; Published by: Journal of Astronomy and Space Sciences Published on: |
2012 |
Day-to-day variability of equatorial anomaly in GPS-TEC during low solar activity period Aggarwal, Malini; Joshi, H.P.; Iyer, K.N.; Kwak, Y.-S.; Lee, J.J.; Chandra, H.; Cho, K.S.; Published by: Advances in Space Research Published on: Jan-06-2012 YEAR: 2012   DOI: 10.1016/j.asr.2012.03.005 |
Persistent longitudinal features in the low-latitude ionosphere Kil, H; Lee, WK; Kwak, Y-S; Oh, S-J; Paxton, LJ; Zhang, Y; Published by: Journal of Geophysical Research: Space Physics Published on: |
2011 |
O and N 2 disturbances in the F region during the 20 November 2003 storm seen from TIMED/GUVI Kil, H.; Kwak, Y.-S.; Paxton, L.; Meier, R.; Zhang, Y.; Published by: Journal of Geophysical Research Published on: Jan-01-2011 YEAR: 2011   DOI: 10.1029/2010JA016227 |
The source of the longitudinal asymmetry in the ionospheric tidal structure Kil, H.; Kwak, Y.-S.; Oh, S.-J.; Talaat, E.; Paxton, L.; Zhang, Y.; Published by: Journal of Geophysical Research Published on: Jan-01-2011 YEAR: 2011   DOI: 10.1029/2011JA016781 |
Longitudinal asymmetry in the crest intensity of the ionospheric tidal structure Kil, H; Paxton, LJ; Zhang, Y; Kwak, Y; Oh, S; Published by: Published on: |
O and N2 disturbances in the F region during the 20 November 2003 storm seen from TIMED/GUVI Kil, H; Kwak, Y-S; Paxton, LJ; Meier, RR; Zhang, Y; Published by: Journal of Geophysical Research: Space Physics Published on: |
2010 |
Is DE2 the source of the ionospheric wave number 3 longitudinal structure? Kil, H.; Paxton, L.; Lee, W.; Ren, Z.; Oh, S.-J.; Kwak, Y.-S.; Published by: Journal of Geophysical Research Published on: Jan-01-2010 YEAR: 2010   DOI: 10.1029/2010JA015979 |
On and N2 disturbances in the F region during the 20 November 2003 storm seen from TIMED/GUVI Kil, Hyosub; Paxton, Larry; Kwak, Young-Sil; Meier, Robert; Zhang, Yongliang; Published by: 38th COSPAR Scientific Assembly Published on: |
Kwak, Y; Kil, H; Lee, W; Cho, K; Published by: Published on: |
2009 |
The Variability of the Zonal Plasma Drift in the Equatorial F Region Kil, H; Kang, C; Oh, S; Kwak, Y; Lee, W; Paxton, LJ; Published by: Published on: |
Kwak, Y; Kil, H; Oh, S; Lee, W; Forbes, JM; Cho, K; Published by: Published on: |
Reversed ionospheric convections during the November 2004 storm: Impact on the upper atmosphere Using the Assimilative Mapping of Ionospheric Electrodynamics (AMIE) procedure, a particular period (2000–2350 UT on 9 November) in the November 2004 storm is studied. During this time interval, IMF Bz was strongly northward along with a high solar wind dynamic pressure, favorable conditions to form reversed convection in the polar region. Indeed, the AMIE outputs show strong reversed convection cells in both hemispheres for a long period (>1 h), which have rarely been observed. The impact on the thermospheric neutral wind has been investigated using the AMIE outputs as the electrodynamic inputs of the National Center for Atmospheric Research Thermosphere Ionosphere Electrodynamics General Circulation Model. After the ionospheric convection reversed, the neutral wind distribution at 400 km altitude changed correspondingly, and the difference wind patterns reversed in the polar cap region. By comparing the temporal variations of the difference ion convection and the difference neutral wind, it is found that horizontal neutral winds respond to the reversed convection with some time delay. The neutral wind response time (e-folding time) clearly has an altitudinal dependence varying from 45 min at 400 km altitude to almost 1.5 h at 200 km. The vertical component vorticity has a similar magnitude and distribution to previous studies in the northward Bz condition and changes the sign when the convection pattern is reversed. Comparison between the CHAMP observed cross-track wind and the simulated neutral wind exhibits a general agreement, and the temporal variations of CHAMP cross-track wind indicate a strong effect of the ion drag force on neutral winds. Deng, Yue; Lu, Gang; Kwak, Young-Sil; Sutton, Eric; Forbes, Jeffrey; Solomon, Stan; Published by: Journal of Geophysical Research: Space Physics Published on: YEAR: 2009   DOI: https://doi.org/10.1029/2008JA013793 |
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