Sporadic E morphology from GPS‐CHAMP radio occultation

[1] The scintillations of phase and amplitude in terms of signal-to-noise ratio (SNR) of the GPS radio occultation signal are caused by thin ionization layers. These thin irregular electron density layers in the E region ionosphere are often called sporadic E (Es). For a monthly retrieval of Es morphology we use the variances of the phase and SNR fluctuations of worldwide ∼6000 GPS/CHAMP occultations in the E region. The Es climatology is studied globally with the SNR and phase variances in terms of monthly zonal means, seasonal maps, and diurnal and long-term variations. The zonal mean variances reveal strong, extended Es activities at summertime midlatitudes but weak, confined activities in wintertime high latitudes, peaking at ∼105 km. Global maps at 105-km altitude show clear dependence of Es activities on the geomagnetic dip angle, where the summertime midlatitude Es occurs mostly at dip angles of 30°–60° and the wintertime high-latitude enhancement occurs mostly at dip angles >80°. The midlatitude Es variances exhibit a strong semidiurnal variation with peak hours near 0800–1000 and 2000 local solar time, respectively. The peak hours are delayed slightly with decreasing height, suggesting influences from the semidiurnal tide. To provide more insights on the observed SNR and phase variances, we model radio wave propagation for the CHAMP observing geometry under several perturbed cases in the E region ionosphere. The model simulations indicate that the SNR variance has the maximum response to Es perturbations at vertical wavelengths of ∼1.2 km, whereas the phase response maximizes at ∼2 km (for the 1-s variance analysis). The characteristic scale depends little on the truncation time used in the SNR variance analysis, but it increases with the truncation time for the phase variances. Initial studies show that reasonable global Es morphology can be produced on a monthly and seasonal basis with the CHAMP one-antenna occultations. Better results from other existing and upcoming GPS occultation missions are anticipated in future studies, and they will significantly improve our understanding of this important phenomenon.

[1]  T. Gaussiran,et al.  Passive detection of sporadic E using GPS phase measurements , 1995 .

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

[3]  K. Hockea,et al.  Global sounding of sporadic E layers by the GPS = MET radio occultation experiment , 2001 .

[4]  K. Hocke,et al.  Irregularities of the topside ionosphere observed by GPS/MET radio occultation , 2002 .

[5]  James J. Spilker,et al.  GPS Signal Structure and Performance Characteristics , 1978 .

[6]  Anthony J. Mannucci,et al.  Lower troposphere refractivity bias in GPS occultation retrievals , 2003 .

[7]  T. Tsuda,et al.  Gravity waves and ionospheric irregularities over tropical convection zones observed by GPS/MET Radio Occultation , 2001 .

[8]  Anthony J. Mannucci,et al.  CHAMP and SAC-C atmospheric occultation results and intercomparisons , 2004 .

[9]  J. Schofield,et al.  Observing Earth's atmosphere with radio occultation measurements using the Global Positioning System , 1997 .

[10]  H. Hayakawa,et al.  The SEEK (Sporadic‐E Experiment over Kyushu) Campaign , 1998 .

[11]  R. Crane,et al.  Ionospheric scintillation , 1977, Proceedings of the IEEE.

[12]  Sergey Sokolovskiy,et al.  Modeling and inverting radio occultation signals in the moist troposphere , 2001 .

[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. Whitehead Recent work on mid-latitude and equatorial sporadic-E , 1989 .

[15]  E. Karayel,et al.  Sub‐Fresnel‐scale vertical resolution in atmospheric profiles from radio occultation , 1997 .

[16]  Eh. S. Kazimirovskij,et al.  The earth's ionosphere. , 1981 .

[17]  J. M. Forbes,et al.  Global transport and localized layering of metallic ions in the upper atmosphere , 1999 .

[18]  W. Bertiger,et al.  A technical description of atmospheric sounding by GPS occultation , 2002 .

[19]  Shengpan P. Zhang,et al.  Climatology of Neutral Winds in the Lower Thermosphere Over Millstone Hill , 2001 .

[20]  Rolf König,et al.  Atmosphere sounding by GPS radio occultation: First results from CHAMP , 2001 .

[21]  Larry J. Romans,et al.  Ionospheric electron density profiles obtained with the Global Positioning System: Results from the GPS/MET experiment , 1998 .

[22]  M. Levy Parabolic Equation Methods for Electromagnetic Wave Propagation , 2000 .

[23]  Jens Wickert,et al.  Application of radio holographic method for observation of altitude variations of the electron density in the mesosphere/lower thermosphere using GPS/MET radio occultation data , 2002 .

[24]  J. D. WHITEHEAD,et al.  Formation of the Sporadic E Layer in the Temperate Zones , 1960, Nature.

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

[26]  K. L. Shrrstha Sporadic-E and atmospheric pressure waves , 1971 .

[27]  R. Bishop,et al.  A comparative study of in-situ and remote intermediate layer measurements against wind model predictions of vertical ion drift , 1998 .

[28]  Mamoru Yamamoto,et al.  On the origin of quasi‐periodic radar backscatter from midlatitude sporadic E , 1994 .

[29]  O. Sherstyukov,et al.  Dependence of sporadic-E layer and lower thermosphere dynamics on solar activity , 2001 .

[30]  W. Baggaley Ionospheric Sporadic-E Parameters: Long-Term Trends , 1984, Science.

[31]  M. E. Gorbunov,et al.  Canonical transform method for processing radio occultation data in the lower troposphere , 2002 .

[32]  Dong L. Wu,et al.  Satellite observations of atmospheric variances: A possible indication of gravity waves , 1996 .

[33]  S. Flatté,et al.  Intensity images and statistics from numerical simulation of wave propagation in 3-D random media. , 1988, Applied optics.

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

[35]  Y. Morton,et al.  Observations of ion layer motions during the AIDA campaign , 1993 .

[36]  P. R. Straus,et al.  GPS occultation sensor observations of ionospheric scintillation , 2003 .

[37]  R. Tsunoda,et al.  Coupled electrodynamics in the nighttime midlatitude ionosphere , 2001 .

[38]  Steven Businger,et al.  GPS Sounding of the Atmosphere from Low Earth Orbit: Preliminary Results , 1996 .