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dc.contributor.author | Pancheva D. | |
dc.contributor.author | Merzlyakov E. | |
dc.contributor.author | Mitchell N. | |
dc.contributor.author | Portnyagin Y. | |
dc.contributor.author | Manson A. | |
dc.contributor.author | Jacobi C. | |
dc.contributor.author | Meek C. | |
dc.contributor.author | Luo Y. | |
dc.contributor.author | Clark R. | |
dc.contributor.author | Hocking W. | |
dc.contributor.author | MacDougall J. | |
dc.contributor.author | Muller H. | |
dc.contributor.author | Kürschner D. | |
dc.contributor.author | Jones G. | |
dc.contributor.author | Vincent R. | |
dc.contributor.author | Reid I. | |
dc.contributor.author | Singer W. | |
dc.contributor.author | Igarashi K. | |
dc.contributor.author | Fraser G. | |
dc.contributor.author | Fahrutdinova A. | |
dc.contributor.author | Stepanov A. | |
dc.contributor.author | Poole L. | |
dc.contributor.author | Malinga S. | |
dc.contributor.author | Kashcheyev B. | |
dc.contributor.author | Oleynikov A. | |
dc.date.accessioned | 2018-09-17T21:31:43Z | |
dc.date.available | 2018-09-17T21:31:43Z | |
dc.date.issued | 2002 | |
dc.identifier.issn | 1364-6826 | |
dc.identifier.uri | https://dspace.kpfu.ru/xmlui/handle/net/135108 | |
dc.description.abstract | During the PSMOS Global-scale tidal variability experiment campaign of June 1-August 31, 1999, a network of radars made measurements of winds, waves and tides in the mesosphere/lower-thermosphere region over a wide range of latitudes. Clear evidence was found that fluctuations in tidal amplitudes occur on a global scale in both hemispheres, and that at least some of these fluctuations are periodic in nature. Modulation of the amplitude of the 12 h tide was particularly evident at periods of 10 and 16 days, suggesting a non-linear interaction with planetary waves of those periods to be responsible. In selected cases, the secondary waves predicted from non-linear theory could be identified and their zonal wave numbers determined. In some, but not all, cases the longitudinal structure of the secondary waves supports the theory of planetary-wave/tidal interaction being responsible for the observed tidal modulation. It was noted also that beating between a 12.4-lunar and the solar tide could produce a near 16-day modulation of the 12 h tide amplitude that is frequently observed in late summer. © 2002 Elsevier Science Ltd. All rights reserved. | |
dc.relation.ispartofseries | Journal of Atmospheric and Solar-Terrestrial Physics | |
dc.subject | Lunar tide | |
dc.subject | MLT region dynamics | |
dc.subject | Non-linear interactions | |
dc.subject | Tidal variability | |
dc.title | Global-scale tidal variability during the PSMOS campaign of June-August 1999: Interaction with planetary waves | |
dc.type | Article | |
dc.relation.ispartofseries-issue | 17 | |
dc.relation.ispartofseries-volume | 64 | |
dc.collection | Публикации сотрудников КФУ | |
dc.relation.startpage | 1865 | |
dc.source.id | SCOPUS13646826-2002-64-17-SID0036836904 |