КФУ. Карточка публикации. Height-latitude structure of the Hayashi waves in the Northern stratosphere and lower mesosphere in winter

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HEIGHT-LATITUDE STRUCTURE OF THE HAYASHI WAVES IN THE NORTHERN STRATOSPHERE AND LOWER MESOSPHERE IN WINTER

Форма представления

Тезисы и материалы конференций в зарубежных журналах и сборниках

Год публикации

2018

Язык

английский

Авторы, сотрудники КФУ

Гурьянов Владимир Владимирович, автор

Библиографическое описание на языке оригинала

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.

Аннотация

42th COSPAR Scientific Assembly, 14 - 22 July 2018, Pasadena, CA, USA.

Ключевые слова

ERA-Interim, reanalysis, Hayashi waves

Название журнала

42th COSPAR Scientific Assembly, 14 - 22 July 2018, Pasadena, CA, USA.

URL

https://www.cospar-assembly.org/uploads/documents/AbstractCD_COSPAR-18.iso

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https://repository.kpfu.ru/?p_id=183847

Файлы ресурса

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F_C0.2_0055_18.pdf	0,06	pdf	посмотреть / скачать

Полная запись метаданных

Поле DC	Значение	Язык
dc.contributor.author	Гурьянов Владимир Владимирович	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/?p_id=183847	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	Тезисы и материалы конференций в зарубежных журналах и сборниках	ru_RU