Труды сотрудников ИВМ СО РАН

/ K. V. Simonov [et al.] // E3S Web of Conferences : EDP Sciences, 2019. - Vol. 75: 2018 Regional Problems of Earth Remote Sensing, RPERS 2018 (11 September 2018 through 14 September 2018, ) Conference code: 145707, DOI 10.1051/e3sconf/20197502007 . -
Аннотация: The study is devoted to the analysis of the features of the change in the parameter EWH (Equivalent Water Height) over the geoid from the satellite measurements of the GRACE space system in seismically active areas of the strongest underwater earthquakes. The GRACE satellite data archive was created. An interpretation of the disturbed state of the geomedium using digital maps of the spatial distribution of the parameter EWH is performed. © The Authors, published by EDP Sciences, 2018.

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Держатели документа:
Institute of Computational Modeling SB RAS, Krasnoyarsk, Akademgorodok, 660036, Russian Federation
Institute of Engineering Physics and Radioelectronics of Siberian Federal University, Akademika Kirenskogo Str. 28/12B, Krasnoyarsk, 660074, Russian Federation

Доп.точки доступа:
Simonov, K. V.; Kashkin, V. B.; Rubleva, T. V.; Krasnoshekov, K. V.

/ A. Zotin [et al.] // Procedia Computer Science : Elsevier B.V., 2019. - Vol. 159: 23rd International Conference on Knowledge-Based and Intelligent Information & Engineering Systems, KES 2019 (4 September 2019 through 6 September 2019, ) Conference code: 141548. - P1642-1651, DOI 10.1016/j.procs.2019.09.334 . -
Аннотация: The paper is devoted to the analysis of the features of the EWH parameter change over the geoid using satellite measurements of the GRACE space system. These local gravitational anomalies are studied depending on the geometrical characteristics of the focal zones of the strongest underwater earthquakes in the period 2003-2016. The statistical processing of satellite observations data using the histogram and maximum entropy methods was performed. Completed interpretation and obtained estimates showing differences and similarities in observational data, due to the peculiarities of the structure of the studied geomedia and the corresponding focal areas. The final result is a statistical description of the space of anomalies of the gravitational field of the Earth as a whole and features of local gravitational anomalies over the focal zones of underwater strong earthquakes in the period from 2003 to 2016. © 2019 The Author(s). Published by Elsevier B.V.

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Держатели документа:
Reshetnev Siberian State University of Science and Technology, 31 Krasnoyarsky rabochy av., Krasnoyarsk, 660037, Russian Federation
Institute of Computational Modeling SB RAS, 50/44 Akademgorodok, Krasnoyarsk, 660036, Russian Federation
Institute of Chemistry and Chemical Technology SB RAS, 50/24 Akademgorodok, Krasnoyarsk, 660036, Russian Federation
Siberian Federal University, 79 Svobodny st., Krasnoyarsk, 660041, Russian Federation

Доп.точки доступа:
Zotin, A.; Simonov, K.; Matsulev, A.; Kurako, M.

/ V. B. Kashkin, K. V. Simonov, T. V. Rubleva, A. N. Matsulev // Proceedings of SPIE - The International Society for Optical Engineering : SPIE, 2019. - Vol. 11208: 25th International Symposium on Atmospheric and Ocean Optics: Atmospheric Physics 2019 (30 June 2019 through 5 July 2019, ) Conference code: 156374. - Ст. 112087Q, DOI 10.1117/12.2540762 . -
Аннотация: The study is devoted to the analysis of the features of the EWH (Equivalent Water Height) parameter over the geoid using satellite measurements of the GRACE space system in seismically active areas of the strongest underwater earthquakes. Created archive of satellite data GRACE. Interpretation of the disturbed state of the geomedia using digital maps of the spatial distribution of the parameter EWH is performed. © 2019 SPIE.

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Держатели документа:
Siberian Federal University, Svobodny str. 79660041, Russian Federation
Institute of Computational Modeling of the Siberian Branch of the Russian Academy of Sciences, Akademgorodok 50/44, Krasnoyarsk, 660036, Russian Federation

Доп.точки доступа:
Kashkin, V. B.; Simonov, K. V.; Rubleva, T. V.; Matsulev, A. N.