On the role of tidal winds in the descending of the high type of sporadic layer (Es)

[1]  M. Muella,et al.  Occurrence and Modeling Examination of Sporadic‐E Layers in the Region of the South America (Atlantic) Magnetic Anomaly , 2019, Journal of Geophysical Research: Space Physics.

[2]  I. Batista,et al.  The influence of tidal winds in the formation of blanketing sporadic e-layer over equatorial Brazilian region , 2017 .

[3]  I. Batista,et al.  Simulations of blanketing sporadic E-layer over the Brazilian sector driven by tidal winds , 2017 .

[4]  M. Pezzopane,et al.  Sporadic E layer at mid-latitudes: average properties and influence of atmospheric tides , 2014 .

[5]  H. Haralambous,et al.  Sporadic E tidal variabilities and characteristics observed with the Cyprus Digisonde , 2014 .

[6]  E. Talaat,et al.  Nonmigrating diurnal tides observed in global thermospheric winds , 2013 .

[7]  José Demisio Simões da Silva,et al.  A computational tool for ionosonde CADI's ionogram analysis , 2013, Comput. Geosci..

[8]  Jens Wickert,et al.  Semidiurnal tidal signature in sporadic E occurrence rates derived from GPS radio occultation measurements at higher midlatitudes , 2009 .

[9]  I. Batista,et al.  Simulation of the sporadic E layer response to prereversal associated evening vertical electric field enhancement near dip equator , 2007 .

[10]  P. Fagundes,et al.  Observations of daytime F2‐layer stratification under the southern crest of the equatorial ionization anomaly region , 2007 .

[11]  D. Pancheva,et al.  Terdiurnal tidelike variability in sporadic E layers , 2006 .

[12]  Dora Pancheva,et al.  Ionogram height–time–intensity observations of descending sporadic E layers at mid-latitude , 2006 .

[13]  N. Mitchell,et al.  Evidence of a role for modulated atmospheric tides in the dependence of sporadic E layers on planetary waves , 2003 .

[14]  J. Liu,et al.  The intermediate layers and associated tidal motions observed by a digisonde in the equatorial anomaly region , 2003 .

[15]  John W. MacDougall,et al.  Global-scale tidal variability during the PSMOS campaign of June–August 1999: interaction with planetary waves , 2002 .

[16]  P. Jayachandran,et al.  Sequential sporadic-E layers at low latitudes in the Indian sector , 1999 .

[17]  J. Mathews.  Sporadic E: current views and recent progress , 1998 .

[18]  Thayananthan Thayaparan,et al.  Simultaneous and colocated observation of winds and tides by MF and meteor radars over London, Canada (43°N, 81°W), during 1994–1996 , 1997 .

[19]  M. Kelley,et al.  Numerical simulations of gravity wave modulation of midlatitude sporadic E layers , 1996 .

[20]  J. Mathews,et al.  Upper atmosphere tides and the vertical motion of ionospheric sporadic layers at Arecibo , 1979 .

[21]  J. MacDougall.  Seasonal variation of semidiurnal winds in the dynamo region , 1978 .

[22]  N. P. Shrestha.  Some features of h-type Es at Uppsala , 1978 .

[23]  R. Harper.  Tidal winds in the 100‐ to 200‐km region at Arecibo , 1977 .

[24]  K. Fujitaka,et al.  A tidal theory of the ionospheric intermediate layer , 1973 .

[25]  R. Lindzen,et al.  Atmospheric Tides: Thermal and Gravitational , 1969 .

[26]  W. Axford.  The formation and vertical movement of dense ionized layers in the ionosphere due to neutral wind shears , 1963 .

[27]  J. Whitehead.  The formation of the sporadic-E layer in the temperate zones , 1961 .

[28]  R. Bishop,et al.  Metallic ion transport associated with midlatitude intermediate layer development , 2003 .

[29]  Wayne K. Hocking,et al.  Real-time determination of meteor-related parameters utilizing modern digital technology , 2001 .