An incoherent scatter radar study of the midnight temperature maximum that occurred at Arecibo during a sudden stratospheric warming event in January 2010

[1]  R. Harper Nighttime meridional neutral winds near 350 km at low to mid-latitudes , 1973 .

[2]  R. Behnke,et al.  Vector measurements of F region ion transport at Arecibo , 1973 .

[3]  M. Faivre,et al.  New results on equatorial thermospheric winds and the midnight temperature maximum , 2008 .

[4]  Michael P. Sulzer,et al.  A radar technique for high range resolution incoherent scatter autocorrelation function measurements utilizing the full average power of klystron radars , 1986 .

[5]  X. Dou,et al.  Enhancements of nighttime neutral and ion temperatures in the F region over Millstone Hill , 2013 .

[6]  T. Fuller‐Rowell,et al.  Midnight temperature maximum (MTM) in Whole Atmosphere Model (WAM) simulations , 2009 .

[7]  J. L. Scali,et al.  Coordinated measurements of F region dynamics related to the thermospheric midnight temperature maximum , 1996 .

[8]  S. González,et al.  Midnight ionosphere collapse at Arecibo and its relationship to the neutral wind, electric field, and ambipolar diffusion , 2012 .

[9]  J. Meriwether,et al.  Comparative investigations of equatorial electrodynamics and low-to-mid latitude coupling of the thermosphere-ionosphere system , 2006 .

[10]  C. Martinis,et al.  The midnight temperature maximum from Arecibo incoherent scatter radar ion temperature measurements , 2013 .

[11]  M. Conde,et al.  Thermospheric temperatures above Poker Flat, Alaska, during the stratospheric warming event of January and February 2009 , 2010 .

[12]  Xueqin Huang,et al.  Midlatitude ionospheric responses to the 2013 SSW under high solar activity , 2016 .

[13]  N. Spencer,et al.  The midnight temperature maximum in the Earth's equatorial thermosphere , 1979 .

[14]  Shunrong Zhang,et al.  Ionospheric signatures of sudden stratospheric warming: Ion temperature at middle latitude , 2008 .

[15]  J. Meriwether,et al.  New radar observations of temporal and spatial dynamics of the midnight temperature maximum at low latitude and midlatitude , 2014 .

[16]  H. Takahashi,et al.  Climatology of the nighttime equatorial thermospheric winds and temperatures over Brazil near solar minimum , 2011 .

[17]  Jonathan T. Fentzke,et al.  Wave signatures in the midlatitude ionosphere during a sudden stratospheric warming of January 2010 , 2013 .

[18]  Qihou Zhou,et al.  Atmospheric tides in the low‐latitude E and F regions and their responses to a sudden stratospheric warming event in January 2010 , 2013 .

[19]  N. Spencer,et al.  On the horizontal distribution of the equatorial thermospheric midnight temperature maximum and its seasonal variation , 1982 .

[20]  J. Meriwether,et al.  Optical interferometric measurements of nighttime equatorial thermospheric winds at Arequipa, Peru , 1986 .

[21]  T. Matsuno,et al.  A Dynamical Model of the Stratospheric Sudden Warming , 1971 .

[22]  J. P. McClure,et al.  Seasonal variation in the occurrence time of the equatorial midnight temperature bulge , 1982 .

[23]  J. Meriwether,et al.  Climatology of the midnight temperature maximum phenomenon at Arequipa, Peru , 2006 .

[24]  C. Martinis,et al.  A nighttime temperature maximum in the thermosphere above Saint Santin in winter , 2012 .

[25]  Yun Gong,et al.  Incoherent scatter radar study of the terdiurnal tide in the E‐ and F‐region heights at Arecibo , 2011 .

[26]  M. Iredell,et al.  Midnight density and temperature maxima, and thermospheric dynamics in Whole Atmosphere Model simulations , 2010 .