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Annales Geophysicae An interactive open-access journal of the European Geosciences Union
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Volume 23, issue 4
Ann. Geophys., 23, 1123–1130, 2005
https://doi.org/10.5194/angeo-23-1123-2005
© Author(s) 2005. This work is distributed under
the Creative Commons Attribution 3.0 License.
Ann. Geophys., 23, 1123–1130, 2005
https://doi.org/10.5194/angeo-23-1123-2005
© Author(s) 2005. This work is distributed under
the Creative Commons Attribution 3.0 License.

  03 Jun 2005

03 Jun 2005

Study of equatorial Kelvin waves using the MST radar and radiosonde observations

P. Kishore1, I. V. Subba Reddy2, S. P. Namboothiri1, K. Igarashi1, M. Venkat Ratnam3, D. Narayana Rao4, and S. Vijaya Bhaskara Rao2 P. Kishore et al.
  • 1National Institute of Information and Communications Technology, Tokyo, Japan
  • 2Department of Physics, Sri Venkateswara University, Tirupati 517 502, India
  • 3Research Institute for Sustainable Humanosphere, Kyoto University, Uji, Kyoto 611-0011, Japan
  • 4National MST Radar Facility, Department of Space, Gadanki 517 112, Tirupati, India

Abstract. In this paper an attempt has been made to study equatorial Kelvin waves using a high power coherent VHF radar located at Gadanki (13.5° N, 79.2° E), a tropical station in the Indian sub-continent. Simultaneous radiosonde observations taken from a nearby meteorological station located in Chennai (13.04° N, 80.17° E) were also used to see the coherence in the observed structures. These data sets were analyzed to study the mean winds and equatorial waves in the troposphere and lower stratosphere. Equatorial waves with different periodicities were identified. In the present study, particular attention has been given to the fast Kelvin wave (6.5-day) and slow Kelvin wave (16-day). Mean zonal wind structures were similar at both locations. The fast Kelvin wave amplitudes were somewhat similar in both observations and the maximum amplitude is about 8m/s. The phase profiles indicated a slow downward progression. The slow Kelvin wave (16-day) amplitudes shown by the radiosonde measurements are a little larger than the radar derived amplitudes. The phase profiles showed downward phase progression and it translates into a vertical wavelength of ~10-12km. The radar and radiosonde derived amplitudes of fast and slow Kelvin waves are larger at altitudes near the tropopause (15-17km), where the mean wind attains westward maximum.

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