Multiyear changes of the Danube delta marine edge

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Abstract

With the help of field and remote (space) methods, detailed studies of long-term changes of the Danube delta coastline (DCL) were carried out. It was established that the DCL displacements (progradation or retreat) can be an effective indicator of delta formation process as a whole: the dynamics of the delta channel network and the redistribution of water flow and sediment load between the branches, the impact of external factors on the delta (river water flow and sediment load, wind and wave action, rise or drop of the sea level). To determine the causes and characteristics of the Danube DCL changes on seven genetically homogeneous areas the contribution of various factors to the balance of sand sediments forming the DCL was evaluated. Locations of the DCL progradation or retreat were determined. Comparison of the results of a study of the Danube DCL dynamics with the data on changes of morphology and regime of other large deltas may allow one to assess the causes and trends of modern processes in river deltas.

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About the authors

M. V. Mikhailova

Water Problems Institute of the Russian Academy of Sciences

Author for correspondence.
Email: mv.mikhailova@gmail.com
Russian Federation, 119333 Moscow

V. I. Kravtsova

Lomonosov Moscow State University

Email: valentinamsu@yandex.ru
Russian Federation, 119991 Moscow

V. N. Morozov

Danube Hydrometeorological Observatory

Email: morozov@dhmo.org.ua
Ukraine, 68609 Izmail

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Supplementary files

Supplementary Files
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2. Fig. 1. Map of the Danube Delta with selected sections of its marine edge (1–7).

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3. Fig. 2. Layout of profiles on the sea edge of the Kiliysky delta (a) and graphs of changes in distances from benchmarks to MKD for 1975–2016. (b)

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4. Fig. 3. Changes in the MKD of the Danube for 2002–2016 in sections 1 (a) and 2 (b): 1 - MKD advance, 2 - MKD retreat.

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5. Fig. 4. Changes in the MKD of the Danube for 2002–2016 in sections 3 (a), 4 (b) and 5 (c): 1 - MKD advance, 2 - MKD retreat.

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6. Fig. 5. Changes in the MKD of the Danube for 2002–2016 in sections 6 (a) and 7 (b): 1 - MKD advance, 2 - MKD retreat.

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7. Fig. 6. The evolution of the Sakhalin Spit at the mouth of St. George’s hands., According to [10].  

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