Mesospheric gravity waves and ionospheric plasma bubbles observed during the COPEX campaign

Abstract During the Conjugate Point Experiment (COPEX) campaign performed at Boa Vista ( 2 . 80 ∘ N ; 60 . 70 ∘ W , dip angle 21 . 7 ∘ N ) from October to December 2002, 15 medium-scale gravity waves in the OHNIR airglow images were observed. Using a Keogram image analysis, we estimate their parameters. Most of the waves propagate to Northwest, indicating that their main sources are Southeast of Boa Vista. Quasi-simultaneous plasma bubble activities in the OI 630 nm images were observed in seven cases. The distances between the bubble depletions have a linear relationship with the wavelengths of the gravity waves observed in the mesosphere, which suggests a direct contribution of the mesospheric medium-scale gravity waves in seeding the equatorial plasma bubbles.

[1]  Thomas Dautermann,et al.  Overview and summary of the Spread F Experiment (SpreadFEx) , 2009 .

[2]  J. W. Dungey,et al.  Convective diffusion in the equatorial F region , 1956 .

[3]  M. Taylor,et al.  Identification of a Thunderstorm as a Source of Short Period Gravity Waves in the Upper Atmospheric Nightglow Emissions , 1988 .

[4]  B. Reinisch,et al.  Equatorial spread F and sporadic E-layer connections during the Brazilian Conjugate Point Equatorial Experiment (COPEX) , 2008 .

[5]  J. Holton,et al.  The Role of Gravity Wave Induced Drag and Diffusion in the Momentum Budget of the Mesosphere , 1982 .

[6]  S. Vadas,et al.  Generation of large-scale gravity waves and neutral winds in the thermosphere from the dissipation of convectively generated gravity waves , 2009 .

[7]  S. Vadas,et al.  Thermospheric responses to gravity waves: Influences of increasing viscosity and thermal diffusivity , 2005 .

[8]  Ronald F. Woodman,et al.  Radar observations of F region equatorial irregularities , 1976 .

[9]  R. Tsunoda On seeding equatorial spread F: Circular gravity waves , 2010 .

[10]  I. Batista,et al.  Vertical ionization drift velocities and range type spread F in the evening equatorial ionosphere , 1983 .

[11]  David L. Hysell,et al.  Nonlinear Rayleigh-Taylor instabilities, atmospheric gravity waves and equatorial spread F , 1993 .

[12]  Suratno,et al.  Mesospheric gravity waves observed near equatorial and low–middle latitude stations: wave characteristics and reverse ray tracing results , 2006 .

[13]  S. Fukao,et al.  Possible evidence of gravity wave coupling into the mid‐latitude F region ionosphere during the SEEK Campaign , 1998 .

[14]  H. Takahashi,et al.  Atmospheric gravity wave propagation direction observed by airglow imaging in the South American sector , 2005 .

[15]  M. Kelley,et al.  Nonlinear evolution of equatorial spread F: 2. Gravity wave seeding of Rayleigh‐Taylor instability , 1996 .

[16]  M. Larsen,et al.  Gravity wave initiation of equatorial spread F: A case study , 1981 .

[17]  E. Dewan,et al.  Simultaneous Observations of Mesospheric Gravity Waves and Sprites Generated by a Midwestern Thunderstorm , 2003 .

[18]  Gary R. Swenson,et al.  High Frequency Atmospheric Gravity Wave Damping in the Mesosphere , 2003 .

[19]  D. Fritts,et al.  The impact of gravity waves rising from convection in the lower atmosphere on the generation and nonlinear evolution of equatorial bubble , 2009 .

[20]  S. Vadas,et al.  Three‐dimensional nonlinear evolution of equatorial ionospheric bubbles with gravity wave seeding and tidal wind effects , 2009 .

[21]  F. S. Johnson,et al.  Occurrence of equatorial F region irregularities: Evidence for tropospheric seeding , 1998 .

[22]  F. Kamalabadi,et al.  Gravity wave and tidal influences on equatorial spread F based on observations during the Spread F Experiment (SpreadFEx) , 2008 .

[23]  S. Vadas,et al.  Thermospheric responses to gravity waves arising from mesoscale convective complexes , 2004 .

[24]  M. Nicolls,et al.  Strong evidence for gravity wave seeding of an ionospheric plasma instability , 2005 .

[25]  C. J. Zamlutti,et al.  Association between plasma bubble irregularities and airglow disturbances over Brazilian low latitudes , 1980 .

[26]  M. Muella,et al.  Magnetic conjugate point observations of kilometer and hundred‐meter scale irregularities and zonal drifts , 2010 .

[27]  P. Stamus,et al.  Convection: the likely source of the medium-scale gravity waves observed in the OH airglow layer near Brasilia, Brazil, during the SpreadFEx campaign , 2009 .

[28]  R. Tsunoda Seeding of equatorial plasma bubbles with electric fields from an Es-layer instability , 2007 .

[29]  B. Clemesha An investigation of the irregularities in the F-region associated with equatorial type spread-F , 1964 .

[30]  C. J. Zamlutti,et al.  Ionospheric zonal velocities at conjugate points over Brazil during the COPEX campaign: Experimental observations and theoretical validations , 2009 .

[31]  S. Eckermann,et al.  A three-dimensional nonhydrostatic ray-tracing model for gravity waves : formulation and preliminary results for the middle atmosphere , 1995 .

[32]  S. W. Bowen,et al.  Gravity waves generated by a tropical cyclone during the STEP tropical field program: A case study , 1993 .

[33]  P. J. Sultan,et al.  Linear theory and modeling of the Rayleigh‐Taylor instability leading to the occurrence of equatorial spread F , 1996 .

[34]  Jia Yue,et al.  A model study of the effects of winds on concentric rings of gravity waves from a convective plume near Fort Collins on 11 May 2004 , 2009 .

[35]  G. Crowley,et al.  Periodic spacing between consecutive equatorial plasma bubbles , 2010 .

[36]  H. Takahashi,et al.  MLT gravity wave climatology in the South America equatorial region observed by airglow imager , 2007 .

[37]  Harold A. B. Gardiner,et al.  MSX satellite observations of thunderstorm‐generated gravity waves in mid‐wave infrared images of the upper stratosphere , 1998 .

[38]  Takuji Nakamura,et al.  A concentric gravity wave structure in the mesospheric airglow images , 2007 .

[39]  W. L. Jones Ray tracing for internal gravity waves , 1969 .

[40]  R. Woodman,et al.  Seeding and layering of equatorial spread F by gravity waves , 1990 .

[41]  B. Reinisch,et al.  F2 Peak parameters, drifts and spread F derived from digisonde ionograms for the COPEX campaign in Brazil , 2008 .

[42]  B. Reinisch,et al.  Conjugate Point Equatorial Experiment (COPEX) Campaign in Brazil: Electrodynamics highlights on spread F development conditions and day-to-day variability , 2009 .

[43]  M. Alexander,et al.  Gravity wave dynamics and effects in the middle atmosphere , 2003 .

[44]  Bodo W. Reinisch,et al.  Multistation digisonde observations of equatorial spread F in South America , 2004 .

[45]  I. Batista,et al.  Conjugate Sporadic-E measurements , 2009 .

[46]  S. Vadas,et al.  Reconstruction of the gravity wave field from convective plumes via ray tracing , 2009 .

[47]  R. Roble,et al.  In‐situ generated gravity waves as a possible seeding mechanism for equatorial spread‐F , 1982 .

[48]  Suratno,et al.  Reverse ray tracing of the mesospheric gravity waves observed at 23°S (Brazil) and 7°S (Indonesia) in airglow imagers , 2006 .

[49]  H. Takahashi,et al.  Simultaneous observation of ionospheric plasma bubbles and mesospheric gravity waves during the SpreadFEx Campaign , 2009 .

[50]  E. R. de Paula,et al.  Gravity wave initiation of equatorial spread F/plasma bubble irregularities based on observational data from the SpreadFEx campaign , 2009 .

[51]  S. Vadas Horizontal and vertical propagation and dissipation of gravity waves in the thermosphere from lower atmospheric and thermospheric sources , 2007 .

[52]  Michael J. Taylor,et al.  Characteristics of mesospheric gravity waves near the magnetic equator, Brazil, during the SpreadFEx campaign , 2009 .

[53]  Steven C. Reising,et al.  Concentric gravity waves in the mesosphere generated by deep convective plumes in the lower atmosphere near Fort Collins, Colorado , 2009 .