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

• Published in: Annales geophysicae (1988) Vol. 23; no. 4; pp. 1123 - 1130
• Main Authors: KISHORE, P, SUBBA REDDY, I. V, NAMBOOTHIRI, S. P, IGARASHI, K, VENKAT RATNAM, M, NARAYANA RAO, D, VIJAYA BHASKARA RAO, S
• Format: Journal Article
• Language: English
• Published: Katlenburg-Lindau European Geophysical Society 01.01.2005; Copernicus Publications
• Subjects: Earth, ocean, space; Exact sciences and technology; External geophysics; Freshwater; Marine; Physics of the high neutral atmosphere; Physics of the ionosphere; Physics of the magnetosphere; India, Andhra Pradesh, Gadanki; Tropical meteorology; Waves and tides; Zonal wind; troposphere; Meteorology and atmospheric dynamics (Middle atmosphere dynamics; Coherent radar; Kelvin wave; Atmospheric dynamics; Meteorological station; Radar observation; Tropopause; periodicity; Wind wave; stratosphere; Simultaneous observation
• ISSN: 0992-7689; 1432-0576; 1432-0576
• DOI: 10.5194/angeo-23-1123-2005

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.