Day-to-day variability of equatorial and low latitude F-region ionosphere in the Indian zone

[1]  B. Jenkins,et al.  Southern hemisphere observations of a long‐term decrease in F region altitude and thermospheric wind providing possible evidence for global thermospheric cooling , 1998 .

[2]  K. Mahajan,et al.  Atmospheric greenhouse effect and ionospheric trends , 1998 .

[3]  Thomas Ulich,et al.  Evidence for long‐term cooling of the upper atmosphere in ionosonde data , 1997 .

[4]  B. M. Reddy,et al.  Zonal/meridional wind and disturbance dynamo electric field control of the low‐latitude ionosphere based on the SUNDIAL/ATLAS 1 Campaign , 1996 .

[5]  J. Bremer The influence of high speed plasma streams on the ionospheric plasma , 1996 .

[6]  R. Stening Modelling the low latitude F region , 1992 .

[7]  T. Kikuchi,et al.  North-south asymmetry of the equatorial ionospheric anomaly observed in East Asia during the SUNDIAL-87 campaign , 1991 .

[8]  K. Cheng,et al.  On the equatorial anomaly of the ionospheric total electron content near the northern anomaly crest region , 1989 .

[9]  C. Hanuise,et al.  On the dependence of the phase velocity of equatorial irregularities on the polarization electric field and theoretical implications , 1986 .

[10]  J. O. Adeniyi Magnetic storm effects on the morphology of the equatorial F2-layer , 1986 .

[11]  Donald T. Farley,et al.  Theory of equatorial electrojet plasma waves: new developments and current status , 1985 .

[12]  P. Bhuyan,et al.  Day-to-day changes in ionospheric electron content at low latitudes , 1984 .

[13]  G. Walker,et al.  A comparison of the ionospheric equatorial anomaly in the East Asian and the American regions at Sunspot minimum , 1981 .

[14]  T. Turunen,et al.  Examples of the influence of strong magnetic storms on the equatorial F-layer , 1980 .

[15]  H. S. Gurm,et al.  Day-to-day variability in TEC of low latitude ionosphere , 1979 .

[16]  G. Walker,et al.  The early morning development and the evening decay of electron content-latitude profiles at low latitudes and their dependence upon solar declination , 1977 .

[17]  C. S. Chan,et al.  The diurnal variation of the equatorial anomaly in the topside ionosphere at sunspot maximum. , 1976 .

[18]  R. Schunk,et al.  Effect of electric fields on the daytime high-latitude E and F regions , 1975 .

[19]  H. Chandra,et al.  Geomagnetic storm effects on ionospheric drifts and the equatorial E/sub s/ over the magnetic equator , 1974 .

[20]  J. Titheridge Continuous records of the total electron content of the ionosphere , 1966 .

[21]  T. Tyagi,et al.  Some Results of Electron Content Measurements at Delhi From Faraday Fading of S‐66 Transmissions , 1966 .

[22]  A. Depueva Quiet timeF2–layer disturbances at geomagnetic equator , 2005 .

[23]  H. Volland,et al.  Handbook of atmospheric electrodynamics , 1995 .

[24]  Michael C. Kelley,et al.  The earth's ionosphere , 1989 .

[25]  B. M. Reddy,et al.  Estimation of the hourly variability of f0F2 at a low‐latitude station , 1987 .

[26]  D. T. Farley,et al.  Theory of Spectral Asymmetries and Nonlinear Currents in the Equatorial Electrojet , 1985 .

[27]  G. Sethia,et al.  Equatorial electrojet control of the low latitude ionosphere. , 1980 .

[28]  R. Rastogi,et al.  ELECTROJET EFFECTS ON THE EQUATORIAL F REGION DURING MAGNETICALLY QUIET AND DISTURBED DAYS. , 1971 .