Development prospects of natural-territorial complex of the Dolgaya spit

Krylenko, Marina; Krylenko, Viacheslav; Volkova, T. A.

doi:10.1016/j.ocecoaman.2018.03.020

Cited by 9 publications

(2 citation statements)

References 2 publications

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“…The Azov Sea Coast has been observed for more than 60 years [2][3][4][5][6][7][8][9]. Scientific monitoring is carried out by a reference network within the Russian coasts of the Don, Kuban areas, the Crimea involving 70 major districts.…”

Section: Methodsmentioning

confidence: 99%

Hazardous Exogenous Geological Processes of Coastal Zone of Azov Sea

Ivlieva¹,

Bespalova²,

Tsygankova³

et al. 2019

Proceedings of the VIII Science and Technology Conference “Contemporary Issues of Geology, Geophysics and Geo-Ecology of the No

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Section: Methodsmentioning

confidence: 99%

Hazardous Exogenous Geological Processes of Coastal Zone of Azov Sea

Ivlieva¹,

Bespalova²,

Tsygankova³

et al. 2019

Proceedings of the VIII Science and Technology Conference “Contemporary Issues of Geology, Geophysics and Geo-Ecology of the No

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“…On 24 September 2014, a SW storm lasting more than a day, accompanied by a surge, destroyed the distal of the main part of the spit and all the islands. Since then, the Dolgaya Spit geosystem has been represented by a relatively stable near-shore part and an extremely dynamic submarine shoal, along the axis of which islands have started to form again since 2016 (Krylenko, Krylenko, 2017).…”

Section: Characteristics Of the Development Of The Accumulative Geosy...mentioning

confidence: 99%

Features of the morphology and dynamics of the shallow-island part of the Dolgaya Spit (the Sea of Azov)

Krylenko¹,

Krylenko²

2022

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The relief of large coastal accumulative bodies, including cuspate spits, is an important subject in scientific and applied research. A characteristic feature of similar accumulative bodies is a shallow underwater part. The aim of this work is to study the shallowisland part structure of the Dolgaya Spit (the Sea of Azov) and to identify the natural mechanism that determines both the variability of accumulative body over short time intervals and the high stability of the geosystem as a whole. Digital elevation models (DEM) for the studied area were built on the basis of remote sensing data (Sentinel-2). It is established that the length of the shallow-island part is about 20 km. There are shelly shoals and islands with a complex configuration and relief. Sea level, the wind-wave regimes and the sediment load are the main factors that determine the dynamic equilibrium of the shallow-island part of the Dolgaya Spit and its relief. The Dolgaya Spit has distinctive features of a free accumulative body influenced by longshore sediment flow. The configuration of its surface part is characteristic of many cuspate spits formed by two sediment streams. But the shallow-island part develops under the influence of alternating transverse movements of water masses and waves from opposite sectors. The coexistence of signs of the near-shore bar and cuspate spit provides grounds for classifying the Dolgaya Spit not as a cuspate accumulative body (in particular as Azovtype spit) but as a separate type developing under joint action of transverse and longshore sediment flows.

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Modern state and dynamics of the Sea of Azov coasts

Kosyan

Krylenko

2019

Estuarine, Coastal and Shelf Science

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Development prospects of natural-territorial complex of the Dolgaya spit

Cited by 9 publications

References 2 publications

Hazardous Exogenous Geological Processes of Coastal Zone of Azov Sea

Hazardous Exogenous Geological Processes of Coastal Zone of Azov Sea

Features of the morphology and dynamics of the shallow-island part of the Dolgaya Spit (the Sea of Azov)

Modern state and dynamics of the Sea of Azov coasts

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