Statistical description of low-latitude plasma blobs as observed by DMSP F15 and KOMPSAT-1 |
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Authors: | J. Park K.W. Min V.P. Kim H. Kil H.J. Kim J.J. Lee E. Lee S.J. Kim D.Y. Lee M. Hairston |
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Affiliation: | 1. Institute of Space Science, National Central University, Chung-Li, Taiwan;2. Department of Physics, KAIST, Daejeon, Republic of Korea;3. IZMIRAN, Moscow Region, Russia;4. Applied Physics Laboratory, Johns Hopkins University, Laurel, MD, USA;5. Satellite Technology Research Center, KAIST, Daejeon, Republic of Korea;6. Space Science Laboratory, University of California at Berkeley, CA, USA;g Department of Astronomy and Space Science, Chungbuk National University, Cheong-ju, Republic of Korea;h William B. Hanson Center for Space Sciences, University of Texas at Dallas, TX, USA |
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Abstract: | The global distribution of low-latitude plasma blobs was investigated by in-situ plasma density measurements from the Korea Multi-Purpose Satellite-1 (KOMPSAT-1) and Defense Meteorological Satellite Program (DMSP) F15. In the observations, blobs occurred in the longitude sector where the activity of the equatorial plasma bubble (EPB) was appreciable, and additional blobs were found at the lower (KOMPSAT-1) altitude as in the EPBs. However, several notable differences exist between the distributions of EPBs and blobs. First, KOMPSAT-1 found few blobs around 0°E in March and June, as did DMSP F15 from 30°W to 120°E for every season. Second, the overall occurrences in December and March at the DMSP F15 (840 km) altitude were somewhat lower than expected from those of the EBPs. Third, at the DMSP F15 altitude, the occurrence probability of plasma blobs was less controlled by yearly variations in the solar activity. These results imply that topside ionospheric conditions as well as the existence of EPBs control further development of blobs. Additionally, it was found that the blob latitudes became higher as the yearly solar activity increased. Moreover, most of the blobs were encountered in the winter hemisphere, possibly due to the low ambient density. |
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Keywords: | Low-latitude ionosphere Topside irregularity Plasma blob Ionospheric climatology In-situ observation |
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