Форма представления | Статьи в зарубежных журналах и сборниках |
Год публикации | 2019 |
Язык | английский |
|
Валиуллин Фаргат Саляхутдинович, автор
Коротышкин Дмитрий Викторович, автор
Мерзляков Евгений Геннадьевич, автор
|
Библиографическое описание на языке оригинала |
Korotyshkin, D., Merzlyakov, E., Sherstyukov, O., Valiullin, F., Mesosphere/lower thermosphere wind regime parameters using a newly installed SKiYMET meteor radar at Kazan (56?N, 49?E)//Advances in Space Research, 2019, doi: https://doi.org/10.1016/j.asr.2018.12.032 |
Аннотация |
New meteor radar (MR) horizontal wind data obtained during 2015-2018 at Kazan (56?N, 49?E) are presented. The measurements were carried out with a state-of-the-art SKiYMET meteor radar. Monthly mean vertical profiles of zonal and meridional components of the the prevailing wind speeds, also amplitudes and phases of the components of diurnal (DT) and semidiurnal tide (SDT) winds are displayed as contour plots for a mean calendar year over the four recent years and compared with distributions of these parameters provided by the previous multiyear (1986-2002) meteor radar (MR) measurements at Kazan and by the recent HWM07 empirical model. The analysis shows that the SKiYMET zonal and meridional prevailing wind speeds are generally in good agreement, sharing the same seasonal features, with the earlier MR seasonal winds. Comparisons with the HWM07 model are not favourable: eastward solstitial cells as modelled are significantly larger, >30 m/s compared to 15-20 m/s. Also, reversal lines ar |
Ключевые слова |
meteor radar; mesosphere and lower thermosphere; wind regim |
Название журнала |
Advances in Space Research
|
URL |
https://ac.els-cdn.com/S0273117718309475/1-s2.0-S0273117718309475-main.pdf?_tid=59fc4d1b-debb-4d68-946e-d3ce8e354e72&acdnat=1547211050_a162bb4ae386274aa583181dc41612ce |
Пожалуйста, используйте этот идентификатор, чтобы цитировать или ссылаться на эту карточку |
https://repository.kpfu.ru/?p_id=193532 |
Полная запись метаданных |
Поле DC |
Значение |
Язык |
dc.contributor.author |
Валиуллин Фаргат Саляхутдинович |
ru_RU |
dc.contributor.author |
Коротышкин Дмитрий Викторович |
ru_RU |
dc.contributor.author |
Мерзляков Евгений Геннадьевич |
ru_RU |
dc.date.accessioned |
2019-01-01T00:00:00Z |
ru_RU |
dc.date.available |
2019-01-01T00:00:00Z |
ru_RU |
dc.date.issued |
2019 |
ru_RU |
dc.identifier.citation |
Korotyshkin, D., Merzlyakov, E., Sherstyukov, O., Valiullin, F., Mesosphere/lower thermosphere wind regime parameters using a newly installed SKiYMET meteor radar at Kazan (56?N, 49?E)//Advances in Space Research, 2019, doi: https://doi.org/10.1016/j.asr.2018.12.032 |
ru_RU |
dc.identifier.uri |
https://repository.kpfu.ru/?p_id=193532 |
ru_RU |
dc.description.abstract |
Advances in Space Research |
ru_RU |
dc.description.abstract |
New meteor radar (MR) horizontal wind data obtained during 2015-2018 at Kazan (56?N, 49?E) are presented. The measurements were carried out with a state-of-the-art SKiYMET meteor radar. Monthly mean vertical profiles of zonal and meridional components of the the prevailing wind speeds, also amplitudes and phases of the components of diurnal (DT) and semidiurnal tide (SDT) winds are displayed as contour plots for a mean calendar year over the four recent years and compared with distributions of these parameters provided by the previous multiyear (1986-2002) meteor radar (MR) measurements at Kazan and by the recent HWM07 empirical model. The analysis shows that the SKiYMET zonal and meridional prevailing wind speeds are generally in good agreement, sharing the same seasonal features, with the earlier MR seasonal winds. Comparisons with the HWM07 model are not favourable: eastward solstitial cells as modelled are significantly larger, >30 m/s compared to 15-20 m/s. Also, reversal lines ar |
ru_RU |
dc.language.iso |
ru |
ru_RU |
dc.subject |
|
ru_RU |
dc.title |
Mesosphere/lower thermosphere wind regime parameters using a newly installed SKiYMET meteor radar at Kazan (56?N, 49?E) |
ru_RU |
dc.type |
Статьи в зарубежных журналах и сборниках |
ru_RU |
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