Equatorial electrodynamics and neutral background in the Asian sector during the 2009 stratospheric sudden warming

Using ground observations of total electron content (TEC) and equatorial electrojet (EEJ) in the Asian sector, along with plasma and neutral densities obtained from the CHAMP satellite, we investigate the ionospheric electrodynamics and neutral background in this longitude sector during the major stratospheric sudden warming (SSW) in January 2009. Our analysis reveals the following prominent features. First, the TEC response in tropical regions is strongly latitude dependent, with monotonic depletion at the dip equator but a semidiurnal perturbation at low latitudes. Second, the TEC semidiurnal perturbation possesses a significant hemispheric asymmetry in terms of onset date and magnitude. It starts on the same day as the SSW peak in the Northern Hemisphere but 2 days later in the Southern Hemisphere. Its magnitude is twice as strong in the north than in the south. Third, strong counter electrojet occurs in the afternoon, following the strengthening of the eastward EEJ in the morning. Fourth, semidiurnal perturbation in both TEC and EEJ possesses a phase shift, at a rate of about 0.7 h/day. Comparisons with results reported in the Peruvian sector reveal clear longitude dependence in the amplitude and hemispheric asymmetry of the semidiurnal perturbation. Finally, thermospheric density undergoes ?25% decrease at low latitudes in the afternoon local time sector during the SSW, indicating significant cooling effects in the tropical upper thermosphere.

[1]  M. Yamamoto,et al.  Strong thermospheric cooling during the 2009 major stratosphere warming , 2011 .

[2]  Anthea J. Coster,et al.  Impact of sudden stratospheric warmings on equatorial ionization anomaly , 2010 .

[3]  J. Chau,et al.  Quiet time ionospheric variability over Arecibo during sudden stratospheric warming events , 2010 .

[4]  Tsutomu Nagatsuma,et al.  Lunar‐dependent equatorial ionospheric electrodynamic effects during sudden stratospheric warmings , 2010 .

[5]  Junichi Kurihara,et al.  Links between a stratospheric sudden warming and thermal structures and dynamics in the high‐latitude mesosphere, lower thermosphere, and ionosphere , 2010 .

[6]  B. Funke,et al.  Evidence for dynamical coupling from the lower atmosphere to the thermosphere during a major stratospheric warming , 2010 .

[7]  Wenbin Wang,et al.  Ionospheric variability due to planetary waves and tides for solar minimum conditions , 2010 .

[8]  A. Coster,et al.  Unexpected connections between the stratosphere and ionosphere , 2010 .

[9]  J. Forbes,et al.  Global structure of the lunar tide in ionospheric total electron content , 2010 .

[10]  S. Sridharan,et al.  Variabilities of mesospheric tides and equatorial electrojet strength during major stratospheric warming events , 2009 .

[11]  M. Yamamoto,et al.  Wave‐4 pattern of the equatorial mass density anomaly: A thermospheric signature of tropical deep convection , 2009 .

[12]  T. Pant,et al.  Equatorial counter electrojets and polar stratospheric sudden warmings - a classical example of high latitude-low latitude coupling? , 2009 .

[13]  S.-Y. Su,et al.  FORMOSAT-3/COSMIC observations of seasonal and longitudinal variations of equatorial ionization anomaly and its interhemispheric asymmetry during the solar minimum period , 2009 .

[14]  Jorge L. Chau,et al.  Quiet variability of equatorial E × B drifts during a sudden stratospheric warming event , 2009 .

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

[16]  P. Alken,et al.  Estimating the daytime Equatorial Ionization Anomaly strength from electric field proxies , 2008 .

[17]  Lintao Liu,et al.  Wavenumber‐4 patterns of the total electron content over the low latitude ionosphere , 2008 .

[18]  S. Watanabe,et al.  Solar activity dependence of the electron density in the equatorial anomaly regions observed by CHAMP , 2007 .

[19]  T. Maruyama,et al.  Low latitude ionosphere-thermosphere dynamics studies with inosonde chain in Southeast Asia , 2007 .

[20]  Hermann Lühr,et al.  Contrasting behavior of the thermosphere and ionosphere in response to the 28 October 2003 solar flare , 2007 .

[21]  B. Reinisch,et al.  Comparison of CHAMP and Digisonde plasma frequencies at Jicamarca, Peru , 2007 .

[22]  Larry J. Paxton,et al.  Control of equatorial ionospheric morphology by atmospheric tides , 2006 .

[23]  S. Franke,et al.  Two‐day wave coupling of the low‐latitude atmosphere‐ionosphere system , 2006 .

[24]  Hermann Lühr,et al.  Zonal winds in the equatorial upper thermosphere: Decomposing the solar flux, geomagnetic activity, and seasonal dependencies , 2006 .

[25]  H. Takahashi,et al.  Planetary wave signatures in the equatorial atmosphere ionosphere system, and mesosphere- E- and F-region coupling , 2006 .

[26]  Jan Laštovička,et al.  Forcing of the ionosphere by waves from below , 2006 .

[27]  Harald U. Frey,et al.  Longitudinal structure of the equatorial anomaly in the nighttime ionosphere observed by IMAGE/FUV , 2005 .

[28]  Hermann Lühr,et al.  Global distribution of the thermospheric total mass density derived from CHAMP , 2004 .

[29]  Raymond G. Roble,et al.  A study of a self-generated stratospheric sudden warming and its mesospheric-lower thermospheric impacts using the coupled TIME-GCM/CCM3 , 2002 .

[30]  Takuya Tsugawa,et al.  A new technique for mapping of total electron content using GPS network in Japan , 2002 .

[31]  G. W. Prölss Common origin of positive ionospheric storms at middle latitudes and the geomagnetic activity effect at low latitudes , 1993 .

[32]  J. Forbes,et al.  Quasi 16-day oscillation in the ionosphere , 1992 .

[33]  G. W. Prölss Magnetic storm associated perturbations of the upper atmosphere: Recent results obtained by satellite‐borne gas analyzers , 1980 .

[34]  A. Richmond,et al.  The relationship between the structure of the equatorial anomaly and the strength of the equatorial electrojet , 1973 .

[35]  S. Fritz,et al.  Planetary Variations of Stratospheric Temperatures , 1972 .

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

[37]  S. Fritz,et al.  Large-Scale Temperature Changes in the Stratosphere Observed from Nimbus III , 1970 .

[38]  P. R. Julian,et al.  A Study of Atmospheric Energetics During the January–February 1963 Stratospheric Warming , 1965 .

[39]  S. Planetary Variations of Stratospheric Temperatures , 2022 .