Form of presentation | Conference proceedings in international journals and collections |
Year of publication | 2018 |
Язык | английский |
|
Guryanov Vladimir Vladimirovich, author
|
Bibliographic description in the original language |
Guryanov V. Height-latitude structure of the Hayashi waves in the Northern stratosphere and lower mesosphere in winter //42th COSPAR Scientific Assembly, 14 - 22 July 2018, Pasadena, CA, USA. |
Annotation |
42th COSPAR Scientific Assembly, 14 - 22 July 2018, Pasadena, CA, USA. |
Keywords |
ERA-Interim, reanalysis, Hayashi waves |
The name of the journal |
42th COSPAR Scientific Assembly, 14 - 22 July 2018, Pasadena, CA, USA.
|
URL |
https://www.cospar-assembly.org/uploads/documents/AbstractCD_COSPAR-18.iso |
Please use this ID to quote from or refer to the card |
https://repository.kpfu.ru/eng/?p_id=183847&p_lang=2 |
Resource files | |
|
Full metadata record |
Field DC |
Value |
Language |
dc.contributor.author |
Guryanov Vladimir Vladimirovich |
ru_RU |
dc.date.accessioned |
2018-01-01T00:00:00Z |
ru_RU |
dc.date.available |
2018-01-01T00:00:00Z |
ru_RU |
dc.date.issued |
2018 |
ru_RU |
dc.identifier.citation |
Guryanov V. Height-latitude structure of the Hayashi waves in the Northern stratosphere and lower mesosphere in winter //42th COSPAR Scientific Assembly, 14 - 22 July 2018, Pasadena, CA, USA. |
ru_RU |
dc.identifier.uri |
https://repository.kpfu.ru/eng/?p_id=183847&p_lang=2 |
ru_RU |
dc.description.abstract |
42th COSPAR Scientific Assembly, 14 - 22 July 2018, Pasadena, CA, USA. |
ru_RU |
dc.description.abstract |
By using the winter (from November to March) ERA-Interim reanalysis geopotential, temperature,zonal and meridional wind data in the troposphere, stratosphere and lower mesosphere (up to the 0.1 hPa isobaric level) for 1979-2016, an analysis of the Hayashi spectra for wave disturbances with zonal wave numbers 1-10 and with periods from 2 to 156 days is performed. In this, contributions of the eastward traveling (E), westward traveling (W), propagating (P), stationary (S) and total (T) waves are estimated. The climatological spatial-temporal distributions
Hayashi waves are integrated by wave number and frequency. As a result, were received integrated height-latitude distributions of waves E, W, P, S and T. It has been established that magnitude of wave energy for geopotential, zonal and meridional wind has two peaks:
in the upper stratosphere - lower mesosphere and in the area of the tropopause. |
ru_RU |
dc.language.iso |
ru |
ru_RU |
dc.subject |
ERA-Interim |
ru_RU |
dc.subject |
reanalysis |
ru_RU |
dc.subject |
Hayashi waves |
ru_RU |
dc.title |
Height-latitude structure of the Hayashi waves in the Northern stratosphere and lower mesosphere in winter |
ru_RU |
dc.type |
Conference proceedings in international journals and collections |
ru_RU |
|