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Vertical structure and characteristics of 23–60 day (zonal) oscillations over the tropical latitudes during the winter months of 1986 — Results of equatorial wave campaign—II

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Abstract

The equatorial wave campaign-II which formed a part of the Indian Middle Atmosphere Programme (IMAP), was conducted from SHAR (13.7°N, 80.2°E) from 15 January to 28 February 1986. Winds were measured from ground to 60 km by means of high altitude balloon and a meteorological rocket (RH-200), once everyday, for 45 days. The frequencies of the oscillations in the deviations of the east-west component of the winds from its mean at each height with one kilometer interval were obtained by the maximum entropy (ME) method and phases/amplitudes of these frequencies were determined by the least squares technique on the wind variation time series. The ME method has the inherent advantage of providing periodicities up to 1.5 times the data length.

The height structure of the long period waves of > 23 day periodicities that have larger amplitudes nearly by a factor of 2 as compared to the medium (9 to 22 day) or shorter period (4 to 8 day) ones, reveal two height regions of enhanced amplitudes, one in the troposphere and another in the upper stratosphere/lower mesosphere, that too, mostly in the regions of positive (westerly increasing or easterly decreasing with height) wind shears. The waves are seen to be inhibited in the negative wind shear regions. From the abrupt changes in the altitude variation of phase, the possible source region has been identified. The vertical wavelengths have been estimated to be 34 km and 19 km in the troposphere and lower stratosphere respectively and 8 km in the upper stratosphere and lower mesosphere. Around 56 km the wave amplitude is reduced to 1/4 of its value below, while the vertical shear strength in the mean wind doubled up. The tropospheric waves are suggested to be Rossby waves of extratropical origin penetrating to tropical latitudes. The stratospheric/mesospheric waves however appear to emanate from a source around the stratopause.

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References

  • Blackman R B and Tukey J W 1958Measurement of power spectra from the point of view of communications engineering (New York: Dover)

    Google Scholar 

  • Burg J P 1967 Maximum entropy spectral analysis;Paper presented in the 37th meeting Soc. Explor. Geophys., New Orleans

  • Burg J P 1970 New concepts in power spectra estimation;Paper presented in 40th meeting Soc. Explor. Geophys., New Orleans

  • Chen T C 1987 30-50 Day Oscillation of 200-mb Temperature and 850-mb height during the 1979 Northern Summer;Mon. Weather Rev. 115 1569–1605

    Google Scholar 

  • Fougere P S 1977 A solution to the problem of spontaneous line splitting in maximum entropy power spectrum analysis;J. Geophys. Res. 82 1051–1054

    Article  Google Scholar 

  • Gao X H and Stanford J L 1987 Low frequency oscillations of the large-scale stratospheric temperature field;J. Atmos. Sci. 44 1991–2000

    Article  Google Scholar 

  • Hirota I 1979 Kelvin waves in the equatorial middle atmosphere observed by the Nimbus 5 SCR;J. Atmos. Sci. 36 217–222

    Article  Google Scholar 

  • Holton J R 1975 The Dynamic Meteorology of the Stratosphere and Mesosphere;Meteor. Monogr. 37 (Amer. Meteor. Soc.)

  • Jones R H 1965 A reappraisal of the periodogram in spectral analysis;Technometrics 7 531–542

    Article  Google Scholar 

  • Krishnamurthy B V, Indukumar S, Raghava Reddi C, Raghavarao R and Rama G V 1986 Results of equatorial wave campaign of IMAP in May–June 1984;Indian Radio Space Phys. 15 125–138

    Google Scholar 

  • Lacoss R T 1971 Data adaptive spectral analysis methods;Geophysics 36 661–675

    Article  Google Scholar 

  • Madden R A and Julian P R 1971 Detection of a 40–50 day oscillation in the zonal wind in the tropical Pacific;J. Atmos. Sci. 28 702–708

    Article  Google Scholar 

  • Madden R A and Julian P R 1972 Description of global-scale circulation cells in the tropics with a 40–50 day period;J. Atmos. Sci. 29 1109–1123

    Article  Google Scholar 

  • Radoski H R, Fougere P S and Zawalick E J 1975 A comparison of power spectral estimate and application of the maximum entropy method;J. Geophys. Res. 80 619–625

    Article  Google Scholar 

  • Radoski H R, Zawalick E J and Fougere P S 1976 The superiority of maximum entropy power spectrum techniques applied to geomagnetic micro pulsations;Phys. Earth Planet. Int. 12 208

    Article  Google Scholar 

  • Sikka D R and Gadgil S 1980 On the maximum cloud zone and the ITCZ over Indian longitudes during South west monsoon;Mon. Weather Rev. 108 1840–1853

    Article  Google Scholar 

  • Smylie D E, Clarke G K S, Ulrych T J 1973 Analysis of irregularities in the earth’s rotation;Meth. Comput. Phys. 13 391–430

    Google Scholar 

  • Ulrych T J 1972 Maximum entropy power spectrum of truncated sinusoids;J. Geophys. Res. 77 1396–1400

    Article  Google Scholar 

  • Ulrych T J and Bishop 1975 Maximum entropy spectral analysis and auto regressive decomposition;Rev. Geophys. Space. Phys. 13 183–200

    Article  Google Scholar 

  • Wallace J M 1971 Spectral studies of tropospheric wave disturbances in the tropical western Pacific;Rev. Geophys. Space. Phys. 9 557–612

    Article  Google Scholar 

  • Webester P J 1983 Large-scale structure of the tropical atmospheres;Large scale dynamical process in the atmospheres (ed) B J Hoskins and R P Pearce (London: Academic Press) pp. 235–275

    Google Scholar 

  • Webester P J and Chang H R 1988 Equatorial energy accumulation and emanation regions: Impacts of a zonally varying basic state;J. Atmos. Sci. 45 803–829

    Article  Google Scholar 

  • Webester P J and Holton J R 1982 Cross equatorial response to mid latitude forcing in a zonally varying basic state;J. Atmos. Sci. 39 722–733

    Article  Google Scholar 

  • Yasunari T 1981 Structure of an Indian summer monsoon system with around 40 day period;J. Meteor. Soc. Jpn. 59 336–354

    Google Scholar 

  • Zhang C and Webester P J 1989 Effects of zonal flows on equatorially trapped waves;J. Atmos. Sci. 46 3632–3652

    Article  Google Scholar 

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Raghavarao, R., Suhasini, R., Sridharan, R. et al. Vertical structure and characteristics of 23–60 day (zonal) oscillations over the tropical latitudes during the winter months of 1986 — Results of equatorial wave campaign—II. Proc. Indian Acad. Sci. (Earth Planet Sci.) 99, 413–423 (1990). https://doi.org/10.1007/BF02841869

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  • DOI: https://doi.org/10.1007/BF02841869

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