Preview

Geomorfologiya i Paleogeografiya

Advanced search

Coastal dynamics in the Narva bay of the Baltic Sea: present-day state and development tendencies

https://doi.org/10.31857/S0435-42812019440-48

Abstract

Central part of Narva bay is characterized by accretive coast, which is formed due to the presence of significant volumes of sand deposits. In the paper, the current state of coastal relief was analyzed and the forecast of its evolution under the prevailing wave climate was performed. The problem of the equilibrium of the coastal morphosystem for a given sediment budget and the probable trend of relative sea level was considered. Morphodynamic forecast for the period of the next decades was justified for designing the crossing of the coastal zone by the main pipeline route. Increasing of the role of accumulation processes from the south to the north has been identified through the field survey and analysis of satellite images, and has been shown by the nature of the beach relief and the underwater coastal slope. The calculation of the longshore sediment drift revealed the existence of a convergence zone for two differently directed sediment flows. Convergence of the sediment flows leads to accumulation of sand deposits at the rate of 19.0 m3 per one running meter per year. Estimates of the sediment budget resulted in the estimation of the accumulation rate at 8 m3 per one running meter per year in the coastal zone of area of the pipeline route. Sand accumulation leads to coastal accretion at the rate of 1 m per year. The obtained results lead to the conclusion on the stability of the coast in the coming decades unless the change of the sources of sand sediments and tendencies of its transport.

About the Authors

D. V. Korzinin
Shirshov Institute of Oceanology RAS
Russian Federation

Moscow



I. O. Leont'yev
Shirshov Institute of Oceanology RAS
Russian Federation

Moscow



M. N. Shtremel'
Shirshov Institute of Oceanology RAS
Russian Federation

Moscow



References

1. Spiridonov M. A., Ryabchuk D. V., Orviku R. K., Sukhacheva L. L., Nesterova E. N., and Zhamoida V. A. Izmenenie beregovoi zony vostochnoi chasti Finskogo zaliva pod vozdeistviem prirodnykh i antropogennykh faktorov (Changes in the coastal zone of the eastern Gulf of Finland under the action of natural and anthropogenic factors). Region. Geol. Metallogen. 2010. No. 41. P. 107-118. (in Russ.)

2. Gudelis V. K. Sovremennye, posle- i pozdnelednikovye dvizheniya zemnoi kory Pribaltiki (sravnitel'nyi analiz) (The recent, post-glacial and late-glacial movements of the Earth’s crust (a comparative analysis)), in Sovremennye dvizheniya zemnoy kory (Recent movements of the Earth’s crust). Tartu: Izd-vo AN EstSSR (Publ.), 1973. No. 5. P. 291-301. (in Russ.)

3. Geologiya SSSR. Leningradskaya, Pskovskaya i Novgorodskaya oblasti. (Geology of the USSR. Leningrad, Pskov and Novgorod Regions). Vol. 1. Description of geology. Kofman V. S., Selivanova V. A. Ed. Moscow: Nedra (Publ), 1971. 504 p.

4. Rybalko A. E., Romm G. M., and Grigoryev V. V. Litologiya poverkhnostnykh osadkov i fatsial'naya zonal'nost' Narvskogo zaliva (Lithology of the surface sediments and facies zonality of the Narva Bay), in Geologiya subakval’noi chasti zony sochleneniya Baltiiskogo shchita i Russkoi plity v predelakh Finskogo zaliva. Leningrad: VSEGEI (Publ), 1989. P. 51-65. (in Russ.)

5. Logvinenko N. V., Barkov L. K., and Gontarev E. A. Issledovanie rel'efa i osadkov beregovoi zony Narvskogo zaliva Baltiiskogo morya (Studies of the relief and deposits in the coastal zone of the Baltic Sea). Litol. Paleogeogr. 1981. Iss. 3. P. 107-127. (in Russ.)

6. Pavlov A. N. Vozdeistvie volnovykh techenii na litodinamicheskuyu i inzhenerno-geologicheskuyu obstanovku dna v melkovodnykh akvatoriyakh (na primere Narvskogo zaliva) (Effect of wave currents on the lithodynamic and geotechnical conditions on the sea floor in shallow-water basins (a case of the Narva Bay). St.-Petersburg: RGGMU, 2011. 98 p.

7. Krasnov E. V. and Ryabkova O. I. Tipy beregov Baltiiskogo morya (Types of the Baltic Sea coasts), in Ekologicheskie problemy Kaliningradskoi oblasti i Baltiiskogo regiona. Kaliningrad: KGU (Publ.), 2005. P. 11-15. (in Russ.)

8. Leont’yev I. O. Morfodinamicheskie processy v beregovoi zone morya (Morphodynamic processes in the Coastal Zone of the Sea). Saarbrücken: LAP LAMBERT Academic Publishing. 2014. 251 p. (in Russ.)

9. Leont’yev I. O. O raschete vdol'beregovogo transporta nanosov (Calculation of Longshore Sediment Transport). Okeanologiya. 2014a. Vol. 54. No. 2. P. 226-232. (in Russ.)

10. Capobianco M., Larson M., Nicholls R. J., and Kraus N. C. Depth of closure: a contribution to the reconcil lation of theory, practice and evidence. Int. Conf. “Coastal Dynamics’97”. Plymouth, 1997. P. 506-515.

11. Klige R. K. Otsenka sovremennykh vertikal'nykh dvizhenii morskikh beregov po izmeneniyu urovnya okeana (Assessment of the recent vertical movements of the sea coasts based of the ocean level changes), in Beregovaya zona morya. Moscow: Nauka (Publ.), 1981. P. 11-17. (in Russ.)

12. IPCC AR4 Sea-level projections. 2012. [Electronic source]. http://www.cmar.csiro.au/sealevel/sl_proj_21st.html (date of the application 07.08.2016).


Review

For citations:


Korzinin D.V., Leont'yev I.O., Shtremel' M.N. Coastal dynamics in the Narva bay of the Baltic Sea: present-day state and development tendencies. Geomorfologiya. 2019;(4):40-48. (In Russ.) https://doi.org/10.31857/S0435-42812019440-48

Views: 985


Creative Commons License
This work is licensed under a Creative Commons Attribution 4.0 License.


ISSN 2949-1789 (Print)
ISSN 2949-1797 (Online)