An investigation of the formation patterns of the ionospheric F3 layer in low and equatorial latitudes
暂无分享,去创建一个
Biqiang Zhao | W. Wan | Jie Zhu | B. Ning | B. Zhao
[1] V. Klimenko,et al. Statistical study of the F3 layer characteristics retrieved from Intercosmos-19 satellite data , 2013 .
[2] V. Klimenko,et al. Formation mechanism of additional layers above regular F2 layer in the near-equatorial ionosphere during quiet period , 2012 .
[3] V. Klimenko,et al. Disturbance dynamo, prompt penetration electric field and overshielding in the Earth’s ionosphere during geomagnetic storm , 2012 .
[4] Biqiang Zhao,et al. Stratification of the Low-Latitude and Near-Equatorial F2 Layer, Topside Ionization Ledge, and F3 Layer: What We Know about This? A Review , 2012 .
[5] S. Rao,et al. Contrasting features of the F 3 layer during high and low solar activity conditions observed from Indian low latitude , 2012 .
[6] V. Klimenko,et al. Latitudinal structure of the equatorial F3 layer based on Intercosmos-19 topside sounding data , 2012 .
[7] P. Fagundes,et al. Seasonal and solar cycle dependence of F3-layer near the southern crest of the equatorial ionospheric anomaly , 2011 .
[8] P. Fagundes,et al. Numerical modeling of ionospheric effects in the middle‐ and low‐latitude F region during geomagnetic storm sequence of 9–14 September 2005 , 2011 .
[9] T. Maruyama,et al. Observations and model calculations of the F3 layer in the Southeast Asian equatorial ionosphere , 2011 .
[10] M. Yamamoto,et al. A statistical study of the response of the dayside equatorial F2 layer to the main phase of intense geomagnetic storms as an indicator of penetration electric field , 2011 .
[11] Biqiang Zhao,et al. Global characteristics of occurrence of an additional layer in the ionosphere observed by COSMIC/FORMOSAT‐3 , 2011 .
[12] H. Le,et al. Features of the F3 layer in the low‐latitude ionosphere at sunset , 2011 .
[13] T. Pant,et al. Features of the F3 layer occurrence over the equatorial location of Trivandrum , 2010 .
[14] Biqiang Zhao,et al. Characteristics of the ionospheric total electron content of the equatorial ionization anomaly in the Asian-Australian region during 1996-2004 , 2009 .
[15] Jann‐Yenq Liu,et al. Neutral wind effect in producing a storm time ionospheric additional layer in the equatorial ionization anomaly region , 2009 .
[16] B. Reinisch,et al. Theoretical study of new plasma structures in the low‐latitude ionosphere during a major magnetic storm , 2009 .
[17] F. C. Seman,et al. Observations of the F3-layer at equatorial region during 2005 , 2008 .
[18] Y. Otsuka,et al. F3 layer during penetration electric field , 2008 .
[19] Xueqin Huang,et al. Formation of an F3 layer in the equatorial ionosphere: A result from strong IMF changes , 2007 .
[20] S. Thampi,et al. An additional layer in the low‐latitude ionosphere in Indian longitudes: Total electron content observations and modeling , 2007 .
[21] P. Fagundes,et al. Observations of daytime F2‐layer stratification under the southern crest of the equatorial ionization anomaly region , 2007 .
[22] T. Maruyama,et al. Magnetic conjugate observation of the F3 layer using the SEALION ionosonde network , 2007 .
[23] A. Kumamoto,et al. Statistical analysis of the ionization ledge in the equatorial ionosphere observed from topside sounder satellites , 2006 .
[24] P. S. Brahmanandam,et al. Features of additional stratification in ionospheric F2 layer observed for half a solar cycle over Indian low latitudes , 2005 .
[25] Libo Liu,et al. Responses of equatorial anomaly to the October-November 2003 superstorms , 2005 .
[26] I. Batista,et al. Long term trends in the frequency of occurrence of the F3 layer over Fortaleza, Brazil , 2002 .
[27] F. T. Berkey,et al. Evidence for the geographic control of additional layer formation in the low-latitude ionosphere , 2001 .
[28] S. Pulinets,et al. INTERCOSMOS-19 OBSERVATIONS OF AN ADDITIONAL TOPSIDE IONIZATION LAYER: THE F3 LAYER , 2001 .
[29] T. Harris,et al. Stratification of the F 2 layer observed in Southeast Asia , 2000 .
[30] S. Watanabe,et al. Variability of an additional layer in the equatorial ionosphere over Fortaleza , 2000 .
[31] I. Batista,et al. Physical mechanism and statistics of occurrence of an additional layer in the equatorial ionosphere , 1998 .
[32] I. Batista,et al. Observations and model calculations of an additional layer in the topside ionosphere above Fortaleza, Brazil , 1997 .
[33] P. Richards,et al. Equatorial plasma fountain and its effects over three locations: Evidence for an additional layer, the F 3 layer , 1997 .
[34] G. J. Bailey,et al. Equatorial plasma fountain and its effects-possibility of an additional layer , 1995 .
[35] R. Raghavarao,et al. Simultaneous occurrence of ionization ledge and counterelectrojet in the equatorial ionosphere: observational evidence and its implications , 1989 .
[36] Chun-Ming Huang. The travelling bifurcation of the equatorial F2 layer , 1975 .
[37] M. Sivaraman,et al. Ionisation ledges in the equatorial ionosphere , 1974, Nature.
[38] Chun-Ming Huang. A certain behavior of the ionospheric F2 region at low latitudes , 1974 .
[39] G. L. Nelms,et al. Topside sounder observations of the equatorial anomaly in the 75° W longitude zone , 1964 .
[40] J. Wager,et al. Field Aligned Strata in the Ionization above the Ionospheric F2 Layer , 1963, Nature.
[41] L. Heisler. The anomalous ionospheric stratification F1·5 , 1962 .
[42] R. Brown,et al. Multiple stratification of the F-layer at Ibadan , 1954 .
[43] J. Ratcliffe. Some regularities in the F2 region of the ionosphere , 1951 .
[44] Hon Yung Sen. Stratification of the F2‐layer of the ionosphere over Singapore , 1949 .