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 |
|