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81.
Alexander A. Soloviev A. I. Gorshkov Anatoly A. Soloviev 《Izvestiya Physics of the Solid Earth》2016,52(6):803-809
For the first time, an attempt is made to apply the data on the lithospheric magnetic anomalies of the Earth for determining the areas prone to strong earthquakes by means of the pattern recognition algorithms. The Caucasian region with the threshold magnitude of the strong earthquakes M0 = 6 is considered. It is established that the data on the lithospheric magnetic anomalies are informative from the standpoint of recognizing the strong earthquake prone areas. Application of these data is promising for solving the similar problems for different seismically active regions. 相似文献
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83.
Krasheninnikov A. V. Loktev D. N. Soloviev S. P. 《Izvestiya Atmospheric and Oceanic Physics》2020,56(8):759-772
Izvestiya, Atmospheric and Oceanic Physics - The relationship between electric field variations and microparticle concentrations in the atmospheric surface layer has been studied using the example... 相似文献
84.
Agayan S. M. Soloviev A. A. Bogoutdinov Sh. R. Nikolova Yu. I. 《Geomagnetism and Aeronomy》2019,59(3):359-367
Geomagnetism and Aeronomy - New mathematical constructions are developed for the regression smoothing of discrete time series defined on an irregular grid. The new method is used to study secular... 相似文献
85.
The lower limit on the drag coefficient under hurricane force winds is determined by the break-up of the air–sea interface
due to Kelvin–Helmholtz instability and formation of the two-phase transition layer consisting of sea spray and air bubbles.
As a consequence, a regime of marginal stability develops. In this regime, the air–sea drag coefficient is determined by the
turbulence characteristics of the two-phase transition layer. The upper limit on the drag coefficient is determined by the
Charnock-type wave resistance. Most of the observational estimates of the drag coefficient obtained in hurricane conditions
and in laboratory experiments appear to lie between the two extreme regimes: wave resistance and marginal stability. 相似文献
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S. L. Soloviev 《Natural Hazards》1990,3(2):183-202
A list of 300 tsunamis and similar phenomena known in the Mediterranean is given. Data reliability and wave intensity are estimated; mechanisms of tsunami generation are indicated and data from literature sources on the coordinates and magnitudes of tsunamigenic earthquakes are cited. Eighteen zones of excitation and manifestation of tsunamis are identified which can be integrated into four groups with respect to the recurrence period and maximum intensity of the tsunamis. The strongest tsunamis are excited in the Aegean Sea, and the Hellenic and Calabrian island arcs. The focal depth of the earthquake-generating tsunamis in the Mediterranean is, on average, less than that in the Pacific. Correspondingly, the magnitude of tsunamigenic earthquakes is lower. According to preliminary estimates, the Mediterranean tsunamis attenuate with distance more rapidly than do those in the Pacific Ocean. 相似文献
89.
Izvestiya, Physics of the Solid Earth - Abstract—There is a brief overview of technogenic sources of microparticles associated with the extraction of mineral raw materials and fuel from the... 相似文献
90.