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1.
I. I. Didenkulova N. Zahibo A. A. Kurkin E. N. Pelinovsky 《Izvestiya Atmospheric and Oceanic Physics》2006,42(6):773-776
The process of nonlinear deformation of a surface wave on shallow waters is investigated. The main attention is given to the relationship between the wave Fourier spectrum and the steepness of wave front slope. It is shown that an unambiguous relationship couples these quantities in the case of an initially sinusoidal wave, which allows estimation of the spectral composition of the wave field from the observed wave steepness. 相似文献
2.
A. I. Zaytsev E. N. Pelinovsky A. A. Kurkin I. S. Kostenko A. Yalciner 《Izvestiya Atmospheric and Oceanic Physics》2016,52(2):217-224
The earthquake that occurred on May 24, 2013, in the basin of the Sea of Okhotsk with a magnitude of 8.3 was the strongest in this region. We have modeled a possible tsunami caused by such an earthquake. The simulations confirm that the wave heights were sufficiently small because the earthquake epicenter depth was 640 km. We analyze the oscillations of the DART buoys in the vicinity of the earthquake source and show that they were not associated with the tsunami waves. Analysis of the available pressure gauge records at different points of the Sea of Okhotsk show that only in one case (Iturup Island) can the observed oscillations of the sea level with a height of approximately 4 cm be classified as tsunami waves. 相似文献
3.
K. I. Kuznetsov A. A. Kurkin E. N. Pelinovsky P. D. Kovalev 《Izvestiya Atmospheric and Oceanic Physics》2014,50(2):213-220
The results of wind-wave measurements with bottom-pressure sensors are discussed. These measurements were performed at the southeastern coast of the Island of Sakhalin in 2006–2009. The problems of converting data obtained with these sensors into water-level displacent in the context of the linear theory are noted. Twenty records with a duration of 2 weeks to 3 months were obtained. These records contain from 150000 to 1200000 waves for three different observation points located at the southeastern coast of Sakhalin in the regions of the village of Vzmor’ye, Lake Izmenchivoye, and the Cape of Ostryi. The estimates obtained for wave-height distributions were approximated by the Weibull distribution. They were compared to the theoretical Rayleigh, Forristall, Weibull, and Glukhovskii distributions. As one would expect, in the region of small wave heights, all distributions prove to be close to one another, and, for large wave heights, the Weibull distribution is preferred. 相似文献
4.
Zaytsev A. I. Babeyko A. Yu. Kurkin A. A. Yalciner A. C. Pelinovsky E. N. 《Izvestiya Atmospheric and Oceanic Physics》2019,55(5):462-469
Izvestiya, Atmospheric and Oceanic Physics - Tsunami forecast possibilities for areas with a small base of historical tsunamis have been discussed using the Probabilistic Tsunami Hazard Assessment... 相似文献
5.
V. A. Ivanova V. I. Kurkin N. M. Polekh L. V. Chistyakova I. G. Brynko V. V. Chuyev Z. F. Dumbrava I. N. Poddelskii 《Geomagnetism and Aeronomy》2011,51(8):1101-1104
The morphological features of wave-like ionospheric disturbances with periods of 1–2 h and the spatial extent exceeding 1000
km are studied. Oblique-incidence sounding data of the ionosphere, obtained in eastern Siberia during several continuous monthly
experiments on three radio paths from 2006 to 2010, have been used. Large-scale traveling ionospheric disturbances generated
during magnetic storms and large-scale wave-like ionospheric disturbances registered during geomagnetically quiet periods
are considered. Small-scale ionospheric structures were also observed against a background of large-scale traveling iono-spheric
disturbances considered in this study. 相似文献
6.
V. I. Kurkin N. M. Polekh O. M. Pirog V. A. Moshkova I. N. Poddel’sky 《Geomagnetism and Aeronomy》2009,49(8):1249-1253
The oblique sounding data at the Magadan-Irkutsk and Norilsk-Irkutsk paths together with the vertical sounding at stations located in northeastern Russia were used to analyze ionospheric disturbances in September 2005 and during geophysically active period in December 2006. It is found that during the main phase of magnetic storms, wave disturbances with a period of 2–4 h are registered. These disturbances cause variations in the layer maximum height up to 40–100 km and in the critical frequency up to 1.5–2 MHz. Those variations change substantially values of the maximum observed frequencies (MOF) of the ionospheric radio channel at the paths considered. Such wave disturbances can be caused by generation of AGWs in the auroral zone and their propagation to equatorial latitudes. 相似文献
7.
A. A. Kurkin E. N. Pelinovsky O. E. Poloukhina 《Izvestiya Atmospheric and Oceanic Physics》2006,42(3):353-361
Within the framework of the linear shallow-water theory, the dynamics of edge waves over a shelf characterized by a cylindrical bottom relief is investigated under the assumption that shelf parameters vary slowly in the alongshore direction. An asymptotic theory and an energy approach are used to calculate the amplitude of the edge wave. In the analytic form, the results are obtained for shelves of three different profiles with parameters varying along the shore: an infinite linear profile, a concave exponential profile, and a stepwise profile. 相似文献
8.
I. I. Didenkulova A. A. Kurkin E. N. Pelinovsky 《Izvestiya Atmospheric and Oceanic Physics》2007,43(3):384-390
The problem of sea-wave run-up on a beach is discussed within the framework of exact solutions of a nonlinear theory of shallow water. Previously, the run-up of solitary waves with different forms (Gaussian and Lorentzian pulses, a soliton, special-form pulses) has already been considered in the literature within the framework of the same theory. Depending on the form of the incident wave, different formulas were obtained for the height of wave run-up on a beach. A new point of this study is the proof of the universality of the formula for the maximum height of run-up of a solitary wave on a beach for the corresponding physical choice of the determining parameters of the incident wave, so that the effect of difference in form is eliminated. As a result, an analytical formula suitable for applications, in particular, in problems related to tsunamis, has been proposed for the height of run-up of a solitary wave on a beach. 相似文献
9.
I. S. Kostenko A. I. Zaytsev D. D. Minaev A. A. Kurkin E. N. Pelinovsky O. E. Oshmarina 《Izvestiya Atmospheric and Oceanic Physics》2018,54(1):1-9
Observation data on the September 5, 1971, earthquake that occurred near the Moneron Island (Sakhalin) have been analyzed and a numerical simulation of the tsunami induced by this earthquake is conducted. The tsunami source identified in this study indicates that the observational data are in good agreement with the results of calculations performed on the basis of shallow-water equations. 相似文献
10.