Relationships between coastal processes and properties of the nearshore sea bed dynamic layer:

The paper discusses the notion of a layer of sandy sediments overlying a substratum of cohesive deposits in the coastal zone. This layer of sand is generally more mobile and is therefore conventionally referred to as the dynamic layer. Its parameters are important to coastal lithodynamic and morphod...

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Main Authors: Rafał Ostrowski, Zbigniew Pruszak
Format: Article
Language:English
Published: Elsevier 2011-09-01
Series:Oceanologia
Subjects:
Online Access:http://www.iopan.gda.pl/oceanologia/53_3.html#A11
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author Rafał Ostrowski
Zbigniew Pruszak
author_facet Rafał Ostrowski
Zbigniew Pruszak
author_sort Rafał Ostrowski
collection DOAJ
description The paper discusses the notion of a layer of sandy sediments overlying a substratum of cohesive deposits in the coastal zone. This layer of sand is generally more mobile and is therefore conventionally referred to as the dynamic layer. Its parameters are important to coastal lithodynamic and morphodynamic processes caused by waves and currents. On the other hand, the dynamic layer is formed by nearshore hydrodynamic impact. The variability of the features of the dynamic layer on the southern Baltic dune and cliff shores in Poland is analysed on the basis of selected geological data supported by local seismo-acoustic field investigations. It appears that the conventional notion of the dynamic layer makes sense only in specific geomorphologic conditions. In such cases, mostly related to cliff shores, theoretical modelling of sediment transport should take the properties of the dynamic layer into account.
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spelling doaj.art-e643a4c622044f5da28097efcf7b72ee2022-12-21T23:27:13ZengElsevierOceanologia0078-32342011-09-01533861880Relationships between coastal processes and properties of the nearshore sea bed dynamic layer:Rafał OstrowskiZbigniew PruszakThe paper discusses the notion of a layer of sandy sediments overlying a substratum of cohesive deposits in the coastal zone. This layer of sand is generally more mobile and is therefore conventionally referred to as the dynamic layer. Its parameters are important to coastal lithodynamic and morphodynamic processes caused by waves and currents. On the other hand, the dynamic layer is formed by nearshore hydrodynamic impact. The variability of the features of the dynamic layer on the southern Baltic dune and cliff shores in Poland is analysed on the basis of selected geological data supported by local seismo-acoustic field investigations. It appears that the conventional notion of the dynamic layer makes sense only in specific geomorphologic conditions. In such cases, mostly related to cliff shores, theoretical modelling of sediment transport should take the properties of the dynamic layer into account.http://www.iopan.gda.pl/oceanologia/53_3.html#A11Dynamic layerSandy sedimentsMulti-bar shoreSouthern Baltic coast
spellingShingle Rafał Ostrowski
Zbigniew Pruszak
Relationships between coastal processes and properties of the nearshore sea bed dynamic layer:
Oceanologia
Dynamic layer
Sandy sediments
Multi-bar shore
Southern Baltic coast
title Relationships between coastal processes and properties of the nearshore sea bed dynamic layer:
title_full Relationships between coastal processes and properties of the nearshore sea bed dynamic layer:
title_fullStr Relationships between coastal processes and properties of the nearshore sea bed dynamic layer:
title_full_unstemmed Relationships between coastal processes and properties of the nearshore sea bed dynamic layer:
title_short Relationships between coastal processes and properties of the nearshore sea bed dynamic layer:
title_sort relationships between coastal processes and properties of the nearshore sea bed dynamic layer
topic Dynamic layer
Sandy sediments
Multi-bar shore
Southern Baltic coast
url http://www.iopan.gda.pl/oceanologia/53_3.html#A11
work_keys_str_mv AT rafałostrowski relationshipsbetweencoastalprocessesandpropertiesofthenearshoreseabeddynamiclayer
AT zbigniewpruszak relationshipsbetweencoastalprocessesandpropertiesofthenearshoreseabeddynamiclayer