RESONANCE OF WAVES AT A TRAIN FERRY
Abstract
The authors describe the researches on resonance wave oscillations in the port of Kholmsk and negative influence of the sea elements on unloading of the trains arriving to Sakhalin from the continent port of Vanino by train ferry. The authors used autonomous and cable recorders of sea-floor hydrostatic pressure that reflected the variations of sea surface. It was proved that during tsunami the zero mode of resonance oscillations with 8 min period increased largely in the port bay. During the storms not only the zero mode but also the peer longitudinal seiche of the bay increased. This seiche has nodal line in the center and antinode in the apex of the bay.
About the Authors
G. V. Shevchenko
Institute of Sea Geology and Geophysics of Far-Eastern Branch of Russian Academy of Sciences
Russian Federation
D.Sc. (Phys-Math), chief of the laboratory of tsunami
Russian Federation
D.Sc. (Phys-Math), chief of the laboratory of tsunami
P. D. Kovalev
Institute of Sea Geology and Geophysics of Far-Eastern Branch of Russian Academy of Sciences
Russian Federation
D.Sc. (Tech), chief of the laboratory of wave dynamics and coastal flows
Russian Federation
D.Sc. (Tech), chief of the laboratory of wave dynamics and coastal flows
D. P. Kovalev
Institute of Sea Geology and Geophysics of Far-Eastern Branch of Russian Academy of Sciences
Russian Federation
Ph.D. (Phys-Math), senior researcher
Russian Federation
Ph.D. (Phys-Math), senior researcher
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Review
For citations:
Shevchenko G.V., Kovalev P.D., Kovalev D.P. RESONANCE OF WAVES AT A TRAIN FERRY. World of Transport and Transportation. 2012;(1):58-65. (In Russ.)
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