nucВестник НЯЦ РКNNC RK Bulletin1729-75161729-7885Национальный ядерный центр Республики Казахстан10.52676/1729-7885-2018-2-152-160nuc-45Research ArticleСтатьиСИГНАЛЫ ОТ СИЛЬНЫХ ШТОРМОВ В СЕВЕРНОЙ АТЛАНТИКЕ ПО ДАННЫМ КАЗАХСТАНСКОЙ СЕТИ: РЕЗУЛЬТАТЫ НАБЛЮДЕНИЯ И МОДЕЛИРОВАНИЕSIGNALS FROM SEVERE OCEAN STORMS IN NORTH ATLANTIC AS IT DETECTED IN KAZAKHSTAN: OBSERVATION AND MODELLINGСмирновА. А.SmirnovA. A.

Курчатов

Kurchatov

Де КарлоМ.De CarloM.

Брест;

Арпажон

Brest;

Arpajon

Ле ПишонА.Le PichonA.

Арпажон

Arpajon

ШапироН. М.ShapiroN. M.

Париж

Paris

Институт геофизических исследований Министерства энергетики Республики КазахстанКазахстанInstitute of Geophysical Researches of Ministry of Energy of the Republic KazakhstanKazakhstanУниверситет Западной Бретани (UBO); Комиссариат по атомной энергии (CEA/DAM/DIF)ФранцияUniversity of Western Brittany (UBO); The Atomic Energy Commission (CEA/DAM/DIF)FranceКомиссариат по атомной энергии (CEA/DAM/DIF)ФранцияThe Atomic Energy Commission (CEA/DAM/DIF)FranceПарижский институт физики Земли (IPGP)ФранцияInstitute of Physics of Globe of Paris (IPGP)France20183006201802152160Copyright © Смирнов А.А., Де Карло М., Ле Пишон А., Шапиро Н.М., 20182018Смирнов А.А., Де Карло М., Ле Пишон А., Шапиро Н.М.Smirnov A.A., De Carlo M., Le Pichon A., Shapiro N.M.Данная работа распространяется под лицензией Creative Commons Attribution 4.0.This work is licensed under a Creative Commons Attribution 4.0 License.https://journals.nnc.kz/jour/article/view/45

Казахстанская сеть мониторинга состоит из четырёх сейсмических и трёх инфразвуковых групп. В записях групп найдено множество сигналов, пришедших с северо-востока. Преобладающим источником микробаром и микросейсм для территории Казахстана является Северная Атлантика [1]. Моделирование изменений положения мест генерации микросейсм и микробаром было произведено на основе данных об энергии и направлении движения морских волн. Произведено сравнение результатов моделирования и наблюдения казахской мониторинговой сети.

The Kazakh monitoring network consists of four seismic and three infrasound arrays. All the arrays record low frequency signals mostly from North-West. A dominating source region of microbarom/microseism signals is located in North Atlantic [1]. Time dependent simulations of the microbarom/microseism source regions are made using a hydrodynamic model of ocean wave interactions developed by IFREMER. Comparisons between observations at the Kazakh monitoring network and modelling results are carried out.

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The authors declare that there are no conflicts of interest present.