SIGNALS FROM SEVERE OCEAN STORMS IN NORTH ATLANTIC AS IT DETECTED IN KAZAKHSTAN: OBSERVATION AND MODELLING
https://doi.org/10.52676/1729-7885-2018-2-152-160
Abstract
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.
About the Authors
A. A. Smirnov
Institute of Geophysical Researches of Ministry of Energy of the Republic Kazakhstan
Kazakhstan
Kurchatov
Kazakhstan
Kurchatov
M. De Carlo
University of Western Brittany (UBO);
The Atomic Energy Commission (CEA/DAM/DIF)
France
France
Brest;
Arpajon
A. Le Pichon
The Atomic Energy Commission (CEA/DAM/DIF)
France
Arpajon
France
Arpajon
N. M. Shapiro
Institute of Physics of Globe of Paris (IPGP)
France
Paris
France
Paris
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Review
For citations:
Smirnov A.A., De Carlo M., Le Pichon A., Shapiro N.M. SIGNALS FROM SEVERE OCEAN STORMS IN NORTH ATLANTIC AS IT DETECTED IN KAZAKHSTAN: OBSERVATION AND MODELLING. NNC RK Bulletin. 2018;(2):152-160. https://doi.org/10.52676/1729-7885-2018-2-152-160
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