Volume 37 Issue 6
Nov.  2017
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SHANG Sheping, SHI Jiankui, YAN Jingye, YANG Guotao, YAN Chunxiao, WANG Xiao, WU Qiongzhi. Analysis of Low Latitude F Region Field-aligned Irregularity Events Observed with Hainan VHF Radar[J]. Chinese Journal of Space Science, 2017, 37(6): 702-709. doi: 10.11728/cjss2017.06.702
Citation: SHANG Sheping, SHI Jiankui, YAN Jingye, YANG Guotao, YAN Chunxiao, WANG Xiao, WU Qiongzhi. Analysis of Low Latitude F Region Field-aligned Irregularity Events Observed with Hainan VHF Radar[J]. Chinese Journal of Space Science, 2017, 37(6): 702-709. doi: 10.11728/cjss2017.06.702

Analysis of Low Latitude F Region Field-aligned Irregularity Events Observed with Hainan VHF Radar

doi: 10.11728/cjss2017.06.702
  • Received Date: 2017-01-11
  • Rev Recd Date: 2017-05-10
  • Publish Date: 2017-11-15
  • Hainan VHF radar has the rapid scan observation capability of two-dimensional imaging of ionospheric irregularities, which is essential for investigating the generation and evolution of Field-Aligned Irregularities (FAI). In this study, the ionospheric irregularities observed by Hainan VHF radar on the night of Oct. 27, 2011 have been analyzed. The main results show that the observed irregularities can be divided into three stages. In the initial formation stage, the irregularities appear very weak and develop very slowly, which mainly expand upward and last for about 14 minutes. In the expansion and enhancement stage, the irregularities rapidly expand and develop both in upward and zonal directions, which last for about 14 minutes. The intensity of irregularities early increases rapidly and later slightly decreases. The spatial scale of irregularities exceeds more than 200km. In the stage of eastward drift and leaving, the intensity of irregularities further decreases, and the expansion area reaches the maximum. It mainly shows the eastward drift and last for nearly 30 minutes. This observation firstly gives the formation and development processes of ionospheric irregularities over the Hainan region, which seems to be quite different from that of other regions.

     

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  • [1]
    KELLEY M C. The Earth's Ionosphere:Plasma Physics and Electrodynamics[M]. 2nd ed. Amsterdam:Elsevier, 2009
    [2]
    WOODMAN R F, LA HOZ C. Radar observations of F region equatorial irregularities[J]. J. Geophys. Res., 1976, 81(31):5447-5466
    [3]
    HYSELL D L, BURCHAM J D. JULIA radar studies of equ-atorial spread F[J]. J. Geophys. Res., 1998, 103(A12):29155-29167
    [4]
    HYSELL D L. An overview and synthesis of plasma irre-gularities in equatorial spread F[J]. J. Atmos. Sol.-Terr. Phys., 2000, 62(12):1037-1056
    [5]
    HYSELL D L, BURCHAM J D. Long term studies of equatorial spread F using the JULIA radar at Jicamarca[J]. J. Atmos. Sol.-Terr. Phys., 2002, 64(12/13/14):1531-1543
    [6]
    CHAPAGAIN N P, FEJER B G, CHAU J L. Climatology of postsunset equatorial spread F over Jicamarca[J]. J. Geophys. Res., 2009, 114(A7):A07307. DOI: 10.1029/2008JA013911
    [7]
    WOODMAN R F, CHAU J L, AQUINO F, et al. Low la-titude field-aligned irregularities observed in the E region with the Piura VHF radar:first results[J]. Radio Sci., 1999, 34(4):983-990
    [8]
    RAO P B, JAIN A R, KISHORE P, et al. Indian MST radar 1. System description and sample vector wind measurements in ST mode[J]. it Radio Sci., 1995, 30(4):1125-1138
    [9]
    FUKAO S, HASHIGUCHI H, YAMAMOTO M, et al. Equa-to-rial Atmosphere Radar (EAR):system description and first results[J]. Radio Sci., 2003, 38(3):1053. DOI: 10.1029/2002RS002767
    [10]
    CHAU J L, WOODMAN R F, FLORES J A. Statistical characteristics of low-latitude ionospheric field-aligned irregularities obtained with the Piura VHF radar[J]. Ann. Geophys., 2002, 20(8):1203-1212
    [11]
    PATRA A K, PHANIKUMAR D V, PANT T K. Gadanki radar observations of F region field-aligned irregula-rities during June solstice of solar minimum:First re-su-lts and preliminary analysis[J]. J. Geophys. Res., 2009, 114(A12):A12305. DOI: 10.1029/2009JA014437
    [12]
    TSUNODA R T. Time evolution and dynamics of equatorial backscatter plumes 1. Growth phase[J]. J. Geophys. Res., 1981, 86(A1):139-149
    [13]
    TSUNODA R T, WHITE B R.On the generation and growth of equatorial backscatter plumes 1. Wave structure in the bottomside F layer[J]. J. Geophys. Res., 1981, 86(A5):3610-3616
    [14]
    TSUNODA R T, LIVINGSTON R C, MCCLUREJ P, et al. Equatorial plasma bubbles:vertically elongated wedges from the bottomside F layer[J]. J. Geophys. Res., 1982, 87(A11):9171-9180
    [15]
    TSUNODA R T. On the generation and growth of equatorial backscatter plumes:2. Structuring of the west walls of upwellings[J]. J. Geophys. Res., 1983, 88(A6):4869-4874
    [16]
    FUKAO S, OZAWA Y, YOKOYAMA T, et al. First observations of the spatial structure of F region 3-m-scale field-aligned irregularities with the Equatorial Atmosphere Radar in Indonesia[J]. J. Geophys. Res., 2004, 109(A2):A02304. DOI: 10.1029/2003JA010096
    [17]
    YOKOYAMA T, FUKAO S, YAMAMOTO M. Relationship of the onset of equatorial F region irregularities with the sunset terminator observed with the Equatorial Atmosphere Radar[J]. Geophys. Res. Lett., 2004, 31(24):L24804. DOI: 10.1029/2004GL021529
    [18]
    FUKAO S, YOKOYAMA T, TAYAMA T, et al. Eastward traverse of equatorial plasma plumes observed with the Equatorial Atmosphere Radar in Indonesia[J]. Ann. Geophys., 2006, 24(5):1411-1418
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