Yuzhno-Sakhalinsk, Russian Federation
from 01.01.2021 until now
Nizhny Novgorod, Nizhny Novgorod, Russian Federation
Yuzhno-Sakhalinsk, Russian Federation
Yuzhno-Sahalinsk, Sakhalin Oblast, Russian Federation
VAC 1.6 Науки о Земле и окружающей среде
UDK 551.46.062.1 Результаты наблюдений за уровнем моря
UDK 551.46.062.6 Волнение и зыбь (морские волны)
UDK 55 Геология. Геологические и геофизические науки
UDK 550.34 Сейсмология
UDK 550.383 Главное магнитное поле Земли
GRNTI 37.25 Океанология
GRNTI 37.01 Общие вопросы геофизики
GRNTI 37.15 Геомагнетизм и высокие слои атмосферы
GRNTI 37.31 Физика Земли
GRNTI 38.01 Общие вопросы геологии
GRNTI 36.00 ГЕОДЕЗИЯ. КАРТОГРАФИЯ
GRNTI 37.00 ГЕОФИЗИКА
GRNTI 38.00 ГЕОЛОГИЯ
GRNTI 39.00 ГЕОГРАФИЯ
GRNTI 52.00 ГОРНОЕ ДЕЛО
OKSO 05.06.01 Науки о Земле
BBK 260 Земля в целом
BBK 26 Науки о Земле
TBK 6325 Гидрофизика. Гидрология
TBK 63 Науки о Земле. Экология
BISAC NAT038000 Natural Resources
BISAC SCI SCIENCE
The results of the study of tidal and subtidal variations in sea level in the area of the southeastern coast of the Sakhalin Island and a series of atmospheric pressure and wind speed from the open website “Weather Schedule” are presented. Using spectral analysis, astronomical tides were studied and diurnal M1, K1 and semi-diurnal M2, S2 tidal harmonics with high energy were detected. The maximum heights of tidal waves have been determined and the tidal regime in the studied water area is classified as mixed with a predominance of diurnal tides. It is shown that sea level rises due to the impact of winds on the sea surface are observed in the northerly direction of the winds, which is associated with storm surge in the coastal zone of Mordvinov Bay. The lowering of the sea level is observed with southerly winds and it is caused by the downsurge. The magnitude of the decrease in sea level for events that have a correlation between high wind speeds and the duration of influence to the winds of the western directions is maximal, and the wind speed has less influence on the magnitude of the decrease in level than its duration. Calculations of the level response to changes in atmospheric pressure using the Proudman equation and analysis of the results showed that these events can be attributed to the phenomenon of the “inverted barometer”. A comparison of theoretical profiles calculated from the time form of the Korteweg–de Vries equation with the registered profiles of sea level showed that they are well described by the profile of a solitary wave.
sea level variations, tidal waves, wave set-up, storm surge and downsurge, inverted barometer, cnoidal wave
1. Adams, J. K., and V. T. Buchwald (1969), The generation of continental shelf waves, Journal of Fluid Mechanics, 35(4), 815–826, https://doi.org/10.1017/S0022112069001455.
2. Andrade, M. M., E. E. Toldo, and J. C. R. Nunes (2018), Tidal and subtidal oscillations in a shallow water system in southern Brazil, Brazilian Journal of Oceanography, 66(3), 245–254, https://doi.org/10.1590/s1679-87592018017406603.
3. Brunner, K., D. Rivas, and K. M. M. Lwiza (2019), Application of Classical Coastal Trapped Wave Theory to High Scattering Regions, Journal of Physical Oceanography, 49(9), 2201–2216, https://doi.org/10.1175/JPO-D-18-0112.1.
4. Darelius, E., L. H. Smedsrud, S. Osterhus, A. Foldvik, and T. Gammelsrod (2009), Structure and variability of the Filchner overflow plume, Tellus A, 61(3), 446–464, https://doi.org/10.1111/j.1600-0870.2009.00391.x.
5. de Miranda, L. B., B. M. de Castro, and B. Kjerfve (2002), Princípios de Oceanografia Física de Estuários, 152 pp., EDUSP, Sao Paulo.
6. de Vries, H., M. Breton, T. de Mulder, Y. Krestenitis, et al. (1995), A comparison of 2D storm surge models applied to three shallow European seas, Environmental Software, 10(1), 23–42, https://doi.org/10.1016/0266-9838(95)00003-4.
7. Dingemans, M. W. (1997), Water Wave Propagation Over Uneven Bottoms: (In 2 Parts), 782 pp., World Scientific Publishing Company, https://doi.org/10.1142/9789812796042.
8. Gill, A. E. (1982), Atmosphere-Ocean Dynamics, 662 pp., Academic Press, London.
9. Giovanangeli, J.-P., C. Kharif, and Y. Stepanyants (2018), Soliton spectra of random water waves in shallow basins, Mathematical Modelling of Natural Phenomena, 13(4), 40, https://doi.org/10.1051/mmnp/2018018.
10. Goryachkin, Y. I., V. A. Ivanov, and Y. A. Stepanyants (1999), Oscillations of the Black Sea sea level in the north part of the coast, Physical Oceanography, 10(2), 123–130, https://doi.org/10.1007/BF02512983.
11. Hamon, B. V. (1966), Continental shelf waves and the effects of atmospheric pressure and wind stress on sea level, Journal of Geophysical Research, 71(12), 2883–2893, https://doi.org/10.1029/JZ071I012P02883.
12. Hereman, W. (2009), Shallow Water Waves and Solitary Waves, in Encyclopedia of Complexity and Systems Science, pp. 8112–8125, Springer New York, https://doi.org/10.1007/978-0-387-30440-3_480.
13. Isozaki, I. (1969), An Investigation on the Variations of Sea Level due to Meteorological Disturbances on the Coast of Japanese Islands (III): On the Variation of Daily Mean Sea Level, Journal of the Oceanographical Society of Japan, 25(2), 91–102, https://doi.org/10.5928/KAIYOU1942.25.91.
14. Jones, I. S. F., and Y. Toba (2001), Wind Stress over the Ocean, 307 pp., Cambridge University Press, Cambridge, https://doi.org/10.1017/CBO9780511552076.
15. Kato, L. N., Y. V. Lyubitsky, and G. V. Shevchenko (2003), Assessment of extreme values of sea level fluctuations on the southeastern coast of Sakhalin Island, Sea level fluctuations: collection of papers, in Sea level fluctuations, pp. 111–128, Russian State Hydrometeorological University, St. Petersburg (in Russian).
16. Koohestani, K., Y. Stepanyants, and M. N. Allahdadi (2023), Analysis of Internal Solitary Waves in the Gulf of Oman and Sources Responsible for Their Generation, Water, 15(4), 746, https://doi.org/10.3390/w15040746.
17. Korteweg, D. J., and G. de Vries (1895), Xli. on the change of form of long waves advancing in a rectangular canal, and on a new type of long stationary waves, The London, Edinburgh, and Dublin Philosophical Magazine and Journal of Science, 39(240), 422–443, https://doi.org/10.1080/14786449508620739.
18. Kovalev, D. P. (2013), Extreme Negative Surge at the South-Eastern Coast of Sakhalin Island, Fundamental and Applied Hydrophysics, 6(1), 52–56 (in Russian).
19. Kovalev, D. P. (2018), Patent of the Russian Federation, RU 2018618773, registration date: 07/19/2018, https://new.fips.ru/registers-doc-view/fips_servlet?DB=EVM&DocNumber=2018618773 (in Russian).
20. Kovalev, D. P., P. D. Kovalev, A. S. Borisov, and K. V. Kirillov (2021), Wave characteristics in the southern part of the Sea of Okhotsk - the area of water transport routes to the southern Kuril Islands, Geosystems of Transition Zones, 5(4), 328–338, https://doi.org/10.30730/gtrz.2021.5.4.328-338 (in Russian).
21. Kovalev, D. P., P. D. Kovalev, and A. S. Borisov (2022), Long-term rise and fall of level of ice-covered Okhotsk Sea near the coast of Mordvinov Bay, Journal of Oceanological Research, 50(4), 5–29, https://doi.org/10.29006/1564-2291.JOR-2022.50(4).1 (in Russian).
22. Kovalev, P. D., and D. P. Kovalev (2018), Long-wave processes in southeastern shelf Sakhalin Island, Ecological Systems and Devices, 8, 36–41, https://doi.org/10.25791/esip.08.2018.121 (in Russian).
23. Kovalev, P. D., and G. V. Shevchenko (2008), Experimental studies of long-wave processes on the Northwestern shelf of the Pacific Ocean, 213 pp., Dalnauka, Vladivostok (in Russian).
24. Kovalev, P. D., A. B. Rabinovich, and G. V. Shevchenko (1991), Investigation of long waves in the tsunami frequency band on the southwestern shelf of Kamchatka, Natural Hazards, 4(2–3), 141–159, https://doi.org/10.1007/BF00162784.
25. Kurkin, A., D. Kovalev, O. Kurkina, and P. Kovalev (2023), Features of Long Waves in the Area of Cape Svobodny (South-Eastern Part of Sakhalin Island) During the Passage of Cyclones, Russian Journal of Earth Sciences, 23(3), ES3003, https://doi.org/10.2205/2023es000852.
26. Leontiev, I. O. (1980), On the possibility of forecasting a wave set-up in a surf zone with an arbitrary bottom profile, Oceanology, 20(2), 290–299.
27. Longuet-Higgins, M. S., and R. W. Stewart (1962), Radiation stress and mass transport in gravity waves, with application to ’surf beats’, Journal of Fluid Mechanics, 13(4), 481–504, https://doi.org/10.1017/S0022112062000877.
28. Longuet-Higgins, M. S., and R. W. Stewart (1964), Radiation stresses in water waves; a physical discussion, with applications, Deep Sea Research and Oceanographic Abstracts, 11(4), 529–562, https://doi.org/10.1016/0011-7471(64)90001-4.
29. Morozov, E. G., D. I. Frey, A. A. Polukhin, V. A. Krechik, et al. (2020), Mesoscale Variability of the Ocean in the Northern Part of the Weddell Sea, Oceanology, 60(5), 573–588, https://doi.org/10.1134/S0001437020050173.
30. Osborne, A. R. (2002), Nonlinear Ocean Wave and the Inverse Scattering Transform, in Scattering, pp. 637–666, Elsevier, https://doi.org/10.1016/B978-012613760-6/50033-4.
31. Parker, B. B. (2007), Tidal analysis and prediction, NOAA, NOS Center for Operational Oceanographic Products and Services, Silver Spring (Maryland), https://doi.org/10.25607/OBP-191.
32. Plekhanov, F. A., and D. P. Kovalev (2016), The complex program of processing and analysis of time-series data of sea level on the basis of author’s algorithms, Geoinformatika, 1, 44–53 (in Russian).
33. Ponte, R. M. (2006), Low-Frequency Sea Level Variability and the Inverted Barometer Effect, Journal of Atmospheric and Oceanic Technology, 23(4), 619–629, https://doi.org/10.1175/JTECH1864.1.
34. Pérez Gómez, B., I. Vilibić, J. Šepić, I. Međugorac, et al. (2022), Coastal sea level monitoring in the Mediterranean and Black seas, Ocean Science, 18(4), 997–1053, https://doi.org/10.5194/os-18-997-2022.
35. Rabinovich, A. B. (1993), Long waves of ocean gravity: trapped, resonance and radiation, 325 pp., Hydrometeoizdat, St. Petersburg (in Russian).
36. Raj, N., Z. Gharineiat, A. A. M. Ahmed, and Y. Stepanyants (2022), Assessment and Prediction of Sea Level Trend in the South Pacific Region, Remote Sensing, 14(4), 986, https://doi.org/10.3390/rs14040986.
37. Squire, V. A., D. P. Kovalev, and P. D. Kovalev (2021a), Aspects of surface wave propagation with and without sea ice on the south-eastern shelf of Sakhalin Island, Estuarine, Coastal and Shelf Science, 251, 107,227, https://doi.org/10.1016/j.ecss.2021.107227.
38. Squire, V. A., P. D. Kovalev, D. P. Kovalev, and V. S. Zarochintsev (2021b), On the trapping of energy from storm surges on the coasts of the Sea of Okhotsk, Estuarine, Coastal and Shelf Science, 250, 107,136, https://doi.org/10.1016/j.ecss.2020.107136.
39. Sudolsky, A. S. (1991), Dynamic phenomena in reservoirs, 262 pp., Hydrometeoizdat, Leningrad (in Russian).
40. Timmerman, H. (1975), On the importance of atmospheric pressure gradients for the generation of external surges in the North Sea: With plates 5 and 6, Deutsche Hydrographische Zeitschrift, 28(2), 62–71, https://doi.org/10.1007/BF02232250.
41. Truccolo, E. C., D. Franco, and C. A. F. Schettini (2006), The low frequency sea level oscillations in the northern coast of Santa Catarina, Brazil, Journal of Coastal Research, SI 39, 547–552.
42. Valentim, S. S., M. E. C. Bernardes, M. Dottori, and M. Cortezi (2013), Low-frequency physical variations in the coastal zone of Ubatuba, northern coast of São Paulo State, Brazil, Brazilian Journal of Oceanography, 61(3), 187–193, https://doi.org/10.1590/S1679-87592013000300003.
43. Weather Schedule LLC (2023), Weather Schedule LLC, https://rp5.ru/Weather_in_Sakhalin (in Russian), (visited on 03/31/2023).
44. Williams, S. J. (2013), Sea-Level Rise Implications for Coastal Regions, Journal of Coastal Research, 63, 184–196, https://doi.org/10.2112/SI63-015.1.
45. Wunsch, C., and D. Stammer (1997), Atmospheric loading and the oceanic "inverted barometer" effect, Reviews of Geophysics, 35(1), 79–107, https://doi.org/10.1029/96RG03037.
