Observations of tides and planetary waves in the atmosphere-ionosphere system

[1]  J. Laštovička,et al.  Solar cycle effect on oscillations in the period range of 2-20 days in the F region of the ionosphere , 1996 .

[2]  J. Laštovička,et al.  Quasi-five- and ten-day oscillations in f0F2 and their possible connection with oscillations at lower ionospheric heights , 1996 .

[3]  K. Hocke.  Tidal variations in the high-latitude E- and F-region observed by EISCAT , 1996 .

[4]  J. Titheridge.  Winds in the ionosphere - a review. , 1995 .

[5]  J. Laštovička,et al.  Trends in planetary wave activity inferred from Hungarian radio wave absorption measurements , 1995 .

[6]  D. Altadill,et al.  Characteristics of quasi‐2‐day oscillations in the ƒ oF2 at northern middle latitudes , 1995 .

[7]  J. Forbes,et al.  Quasi 16‐day oscillation in the mesosphere and lower thermosphere , 1995 .

[8]  K. Glassmeier,et al.  Periods of planetary waves in geomagnetic variations , 1995 .

[9]  W. Skinner,et al.  Observations of the 5-day wave in the mesosphere and lower thermosphere , 1994 .

[10]  Yi-Bo Luo,et al.  Evidence for the coincident long period oscillations in the Equatorial Ionization Anomaly with the zonal neutral wind in the mesosphere , 1994 .

[11]  H. G. Muller,et al.  Geomagnetic influences upon tides—winds from MLT radars , 1994 .

[12]  A. Manson,et al.  Variations of mean winds and solar tides in the mesosphere and lower thermosphere over time scales ranging from 6 months to 11 yr: Saskatoon, 52°N, 107°W , 1994 .

[13]  Roberta M. Johnson,et al.  Semidiurnal tide in the 80–150 km region: an assimilative data analysis , 1994 .

[14]  J. Laštovička,et al.  Long-term trends in planetary wave activity (2–15 days) at 80–100 km inferred from radio wave absorption , 1994 .

[15]  P. Canziani.  On tidal variability and the existence of planetary wave-like oscillations in the upper thermosphere—I. Observations of tidal variability , 1994 .

[16]  Yi-Bo Luo,et al.  Long period oscillations in the equatorial ionization anomaly correlated with the neutral wind in the mesosphere , 1993 .

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

[18]  B. Morena,et al.  Quasi-periodic fluctuations in ionospheric absorption in relation to planetary activity in the stratosphere , 1991 .

[19]  H. Teitelbaum,et al.  On tidal variability induced by nonlinear interaction with planetary waves , 1991 .

[20]  N. W. Spencer,et al.  Revised global model of thermosphere winds using satellite and ground‐based observations , 1991 .

[21]  C. E. Meek,et al.  Climatologies of semi-diurnal and diurnal tides in the middle atmosphere (70–110 km) at middle latitudes (40–55°) , 1989 .

[22]  T. Tsuda,et al.  Asymmetries in mesospheric tidal structure , 1989 .

[23]  J. Laštovička,et al.  Long-period fluctuations of meteorological origin observed in the lower ionosphere , 1989 .

[24]  A. Manson,et al.  Winds and waves in the middle atmosphere at Saskatoon (52°N, 107°W), Collm (52°N, 15°E) and Badary (52°N, 105°E) , 1988 .

[25]  J. Forbes,et al.  Atmospheric tides below 80 km , 1985 .

[26]  R. Vincent.  Planetary and gravity waves in the mesosphere and lower thermosphere , 1985 .

[27]  K. Kawahira.  Global structures of stationary planetary waves in the middle atmosphere , 1983 .

[28]  Jeffrey M. Forbes,et al.  Atmospheric tides: 1. Model description and results for the solar diurnal component , 1982 .

[29]  A. Prata,et al.  Evidence for a traveling two‐day wave in the middle atmosphere , 1981 .

[30]  W. Elford,et al.  Observations of the quasi 2-day wave near 90 km altitude at Adelaide /35 S/ , 1981 .

[31]  R. Bernard.  Variability of die semi-diurnal tide in the upper mesosphere , 1981 .

[32]  A. Manson,et al.  Atmospheric waves (≈ 10 min–30 days) in the mesosphere and thermosphere at saskatoon (52°N, 107°W), October 1978–September 1979 , 1981 .

[33]  R. A. Madden,et al.  Observations of large‐scale traveling Rossby waves , 1979 .

[34]  D. Cavalieri.  Traveling planetary-scale waves in the E-region , 1976 .

[35]  H. Schwentek.  Wave-like structures in the variation of ionospheric absorption , 1974 .

[36]  H. G. Muller,et al.  Non-linear planetary/tidal wave interactions in the lower thermosphere observed by meteor radar , 1996 .

[37]  A. Ebel,et al.  On the transformation of planetary waves of tropospheric origin into waves in radio wave absorption in the lower ionosphere , 1994 .

[38]  D. Pancheva,et al.  Simultaneous observation of the quasi-two-day variations in the lower and upper ionosphere over Europe , 1994 .

[39]  J. Laštovička.  Planetary wave activity in the upper middle atmosphere inferred from radio wave absorption and the quasi-biennial oscillation , 1993 .

[40]  D. Pancheva,et al.  Quasi-two-day variations observed in the lower and upper ionosphere over Europe , 1991 .

[41]  J. Laštovička,et al.  Changes in characteristics of planetary waves at 80–100 km over Central and Southern Europe since 1980 , 1991 .

[42]  R. Schminder,et al.  Variability of tides in winter especially during STRATWARM , 1990 .

[43]  J. Forbes.  Atmospheric Tides Between 80 Km and 120 Km , 1990 .