Skip to main content
Log in

Alongshore Fluxes of Sand Sediments in the Region of Propagation of Tropical Cyclones (Example of the Hicacos Peninsula, Cuba)

  • OCEANOLOGY
  • Published:
Doklady Earth Sciences Aims and scope Submit manuscript

Abstract

The results of analysis of climatic peculiarities of the alongshore fluxes of bottom sediments are presented. The object of research is the coastal zone of the Hicacos Peninsula in the northern part of Cuba. The main goal of this work is to analyze the peculiarities of alongshore transport of bottom sediments in the region of the Hicacos Peninsula in the period from 1990 to 2019. Components of surface waves are considered as a transport mechanism: pure wind waves and swell. The research method is mathematical modeling. The parameters of surface waves were estimated using the modern DHI MIKE 21 SW spectral wave model. A mathematical model, which calculates the fluxes of noncohesive material under the influence of wind waves, is used to estimate the volumes of transported bottom sediments. It was estimated that the annual mean (climatic) values of the fluxes from east to west are 45 000 m3/year, while those from west to east are about 11 000 m3/year. The contribution of individual tropical cyclones to the annual fluxes can be very significant; they are measured in tens of percent.

This is a preview of subscription content, log in via an institution to check access.

Access this article

Price excludes VAT (USA)
Tax calculation will be finalised during checkout.

Instant access to the full article PDF.

Institutional subscriptions

Fig. 1.
Fig. 2.
Fig. 3.
Fig. 4.
Fig. 5.
Fig. 6.
Fig. 7.
Fig. 8.
Fig. 9.
Fig. 10.
Fig. 11.

Similar content being viewed by others

REFERENCES

  1. N. N. Dunaev, I. O. Leont’yev, and J. L. J. Marti, Oceanology 60 (4), 542–548 (2020).

    Google Scholar 

  2. N. N. Dunaev, I. O. Leont’yev, T. Yu. Repkina, and J. F. Herrera, Uch. Zap. Ross. Gos. Gidrometeorol. Univ., No. 50, 152–169 (2018).

  3. I. Mitrani-Arenal, A. Perez-Bello, J. Cabrales-Infante, Y. Povea-Perez, M. Hernández-Gonzalez, and O. Diaz-Rodriguez, Rev. Cubana Meteorol. 25 (2), 121–138 (2019).

    Google Scholar 

  4. A. Pérez-Bello, I. Mitrani-Arenal, O. Diaz-Rodríguez, C. Wettre, and L. Hole, Rev. Cubana Meteorol. 25 (1), 109–120 (2019).

    Google Scholar 

  5. V. S. Medvedev and J. L. Juanes, Morpholithodynamical researches in the littoral zone and at shelf of Cuba northern bank, in Continental and Island Shelfs. Relief and Depositions (Nauka, Moscow, 1981), pp. 229–251 [in Russian].

    Google Scholar 

  6. N. N. Dunaev, I. O. Leont’yev, T. Y. Repkina, and J. L. J. Marti, Springer Geol. 1, 83–92 (2020). https://doi.org/10.1007/978-3-030-38177-6_10

    Google Scholar 

  7. MIKE 21, Spectral Wave Module, DHI Water & Environment, 2007.

  8. B. Divinsky and R. Kosyan, Cont. Shelf Res. 136, 1–19 (2017). https://doi.org/10.1016/j.csr.2017.01.008

    Google Scholar 

  9. B. Divinsky and R. Kosyan, Oceanologia 60, 277–287 (2018). https://doi.org/10.1016/j.oceano.2017.11.006

    Google Scholar 

  10. K. Taylor, J. Geophys. Res. 106, 7183–7192 (2001).

    Google Scholar 

  11. M. S. Longuet-Higgins, J. Geophys. Res. 75, 6788–6801 (1970).

    Google Scholar 

  12. M. Larson, L. X. Hoan, and H. Hanson, J. Waterway, Port, Coast, Ocean Eng. 136 (2), 119–122 (2009).

    Google Scholar 

  13. S. Zou, R. Dalrymple, F. Asce, and B. Rogers, in Proc. 5th Int. Symp. on Ocean Waves Measurement and Analysis Waves-2005 (Madrid, 2005), pp. 186–192.

  14. T. Walton, Coastal Engineering Manual, Part III: Coastal Sediment Processes, Engineer Manual 1110-2-1100 (U.S. Army Corps of Engineers, Washington, 2002), Chapter III-6, p. 72.

  15. R. Kos’yan, Coast. Eng. 9, 171–187 (1985).

    Google Scholar 

  16. J. G. Jonsson, On the existence of universal velocity distributions in an oscillatory, turbulent boundary layer, in Report No. 12 of Coast. Eng. Lab/Hydraul. Lab. (Tech. Univ. Denmark, 1966), pp. 2–10.

  17. A. D. Ashton and A. B. Murray, J. Geophys. Res. 111, F04011 (2006). https://doi.org/10.1029/2005JF000422

    Google Scholar 

  18. C. M. González-Ramirez and L. E. Guadalupe, Rev. Cubana Meteorol. 25 (3), 469–480 (2019).

    Google Scholar 

Download references

Funding

This problem was formulated according to a State Assignment (project no. 0149-2019-0005), and was supported by the Russian Foundation for Basic Research (project no. 18-55-34002), analysis of the experimental data was supported by the Russian Science Foundation (project no. 20-17-00060), and the mathematical modeling and computational part was performed with the support of grants from the Russian Foundation for Basic Research (project nos. 18-05-80035, 19-05-00041, and 19-45-230002). The analysis of the results was supported within the framework of program no. 0149-2019-0014 and by the Russian Foundation for Basic Research (project no. 20-05-00009).

Author information

Authors and Affiliations

Authors

Corresponding author

Correspondence to B. V. Divinsky.

Additional information

Translated by E. Morozov

Rights and permissions

Reprints and permissions

About this article

Check for updates. Verify currency and authenticity via CrossMark

Cite this article

Divinsky, B.V., Dunaev, N.N. & Kosyan, R.D. Alongshore Fluxes of Sand Sediments in the Region of Propagation of Tropical Cyclones (Example of the Hicacos Peninsula, Cuba). Dokl. Earth Sc. 497, 328–340 (2021). https://doi.org/10.1134/S1028334X2104005X

Download citation

  • Received:

  • Revised:

  • Accepted:

  • Published:

  • Issue Date:

  • DOI: https://doi.org/10.1134/S1028334X2104005X

Keywords:

Navigation