Research output: Chapter in Book/Report/Conference proceeding › Conference contribution › Research › peer-review
Experience in Determining S-Wave Velocities Beneath the Caucasus from Surface Wave Dispersion Curves Using High-Performance Computing. / Koroleva, T.; Zarochentsev, A.
Problems of Geocosmos—2024 (ICS 2024). Springer Nature, 2026. p. 165-177 (Springer Proceedings in Earth and Environmental Sciences; Vol. Part F1503).Research output: Chapter in Book/Report/Conference proceeding › Conference contribution › Research › peer-review
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TY - GEN
T1 - Experience in Determining S-Wave Velocities Beneath the Caucasus from Surface Wave Dispersion Curves Using High-Performance Computing
AU - Koroleva, T.
AU - Zarochentsev, A.
N1 - Conference code: 15
PY - 2026
Y1 - 2026
N2 - The article describes the experience of setting and solving the inverse problem of determining the velocity of shear waves under the Caucasus from surface wave dispersion curves using a high-performance distributed grid cluster. It is about options for adapting programs written for personal computers for modern high-performance clusters. Various models for assessing the velocity structure of the Caucasus and their suitability for the programs used are considered. It is concluded that the three-layer model of the crust does not fit the data well enough, which requires changes to the source program code. Also shows the fundamental possibility of using distributed computing systems such as GRID to solve inverse problems of Earth Physics. © The Author(s), under exclusive license to Springer Nature Switzerland AG 2026.
AB - The article describes the experience of setting and solving the inverse problem of determining the velocity of shear waves under the Caucasus from surface wave dispersion curves using a high-performance distributed grid cluster. It is about options for adapting programs written for personal computers for modern high-performance clusters. Various models for assessing the velocity structure of the Caucasus and their suitability for the programs used are considered. It is concluded that the three-layer model of the crust does not fit the data well enough, which requires changes to the source program code. Also shows the fundamental possibility of using distributed computing systems such as GRID to solve inverse problems of Earth Physics. © The Author(s), under exclusive license to Springer Nature Switzerland AG 2026.
KW - Ambient noise tomography
KW - GRID
KW - HPC
KW - Inverse problem
KW - S-wave velocities
KW - Surface wave tomography
UR - https://www.mendeley.com/catalogue/0f174232-3c5d-3536-9d63-1af0163bc477/
U2 - 10.1007/978-3-031-92928-1_11
DO - 10.1007/978-3-031-92928-1_11
M3 - статья в сборнике материалов конференции
T3 - Springer Proceedings in Earth and Environmental Sciences
SP - 165
EP - 177
BT - Problems of Geocosmos—2024 (ICS 2024)
PB - Springer Nature
Y2 - 22 April 2024 through 26 April 2024
ER -
ID: 150628273