Details
Original language | English |
---|---|
Pages (from-to) | 100-109 |
Number of pages | 10 |
Journal | Continental shelf research |
Volume | 48 |
Early online date | 3 Sept 2012 |
Publication status | Published - 1 Oct 2012 |
Abstract
Beachrocks are common coastal formations, constructed through the lithification of beach sediments by carbonate cements. The objectives of the present contribution were to (a) assess the impacts of beachrock benthic communities on nearshore wave dynamics; (b) present a numerical model, developed to simulate wave propagation over shallow nearshore waters characterized by both loose sediment beds and colonized/non-colonized beachrocks; and (c) discuss the structure and dynamics of beachrock macro-benthic communities in an E. Mediterranean micro-tidal beach (Vatera, Lesbos Island, NE Aegean Sea), as well as their interactions with the wave forcing. Field measurements of wave height and flow velocity were processed to assess shoaling wave energy dissipation due to bottom friction from the colonized beachrock outcrops. The equivalent Nikuradse hydraulic roughness of the beachrock surface, estimated through spectral wave attenuation calculations, was found to be around kN=0.13m. The corresponding wave friction factors were incorporated into a wave propagation model to obtain estimates of the wave-induced bed shear stress τw acting on the beachrock benthic communities. Information about the structure and characteristics of the latter was obtained through the collection and analysis of samples from 15 stations along a beach transect, during two months of the year (April and September) and the results showed that benthic communities at the beachrock habitat were very similar to the ones typically found at NE Mediterranean hard substrates. Wave-induced bed shear stress τw values were able to explain cross-shore variations in population density and biomass, both decreasing significantly above water depths of about h=1.8-2m. The latter values corresponded, for the studied conditions, to shear stresses of about τw=2.2Nt/m2. The present findings clearly show that nearshore wave patterns not only control to a certain extent the spatial structure of the beachrock habitats, but can be also influenced by them. Thus, hydrodynamics and beachrocks habitats constitute a complex system which remains very little understood and demands for further investigation.
Keywords
- Beachrocks, Bed shear stress, Benthic communities, Hard substrate, Mediterranean Sea, Wave friction factor
ASJC Scopus subject areas
- Earth and Planetary Sciences(all)
- Oceanography
- Agricultural and Biological Sciences(all)
- Aquatic Science
- Earth and Planetary Sciences(all)
- Geology
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In: Continental shelf research, Vol. 48, 01.10.2012, p. 100-109.
Research output: Contribution to journal › Article › Research › peer review
}
TY - JOUR
T1 - Field observations and modeling of wave attenuation over colonized beachrocks
AU - Vousdoukas, M. I.
AU - Velegrakis, A. F.
AU - Paul, M.
AU - Dimitriadis, C.
AU - Makrykosta, E.
AU - Koutsoubas, D.
N1 - Funding Information: The principal author (VMI) gratefully acknowledges the financial support by the Greek Ministry of Education through the Programme ‘Iraklitos’ . We are also thankful to Prof. Theophanis Karambas for his support in getting the numerical model running, and to Adonis Eleftheriou, Kostas Dimou, Giorgos Valais, Stergios Zarkogiannis, Raphael Meligonitis and all the other students and colleagues who contributed to the field data collection. Comments from two anonymous reviewers and the editor resulted in substantial improvements in the manuscript and are gratefully acknowledged.
PY - 2012/10/1
Y1 - 2012/10/1
N2 - Beachrocks are common coastal formations, constructed through the lithification of beach sediments by carbonate cements. The objectives of the present contribution were to (a) assess the impacts of beachrock benthic communities on nearshore wave dynamics; (b) present a numerical model, developed to simulate wave propagation over shallow nearshore waters characterized by both loose sediment beds and colonized/non-colonized beachrocks; and (c) discuss the structure and dynamics of beachrock macro-benthic communities in an E. Mediterranean micro-tidal beach (Vatera, Lesbos Island, NE Aegean Sea), as well as their interactions with the wave forcing. Field measurements of wave height and flow velocity were processed to assess shoaling wave energy dissipation due to bottom friction from the colonized beachrock outcrops. The equivalent Nikuradse hydraulic roughness of the beachrock surface, estimated through spectral wave attenuation calculations, was found to be around kN=0.13m. The corresponding wave friction factors were incorporated into a wave propagation model to obtain estimates of the wave-induced bed shear stress τw acting on the beachrock benthic communities. Information about the structure and characteristics of the latter was obtained through the collection and analysis of samples from 15 stations along a beach transect, during two months of the year (April and September) and the results showed that benthic communities at the beachrock habitat were very similar to the ones typically found at NE Mediterranean hard substrates. Wave-induced bed shear stress τw values were able to explain cross-shore variations in population density and biomass, both decreasing significantly above water depths of about h=1.8-2m. The latter values corresponded, for the studied conditions, to shear stresses of about τw=2.2Nt/m2. The present findings clearly show that nearshore wave patterns not only control to a certain extent the spatial structure of the beachrock habitats, but can be also influenced by them. Thus, hydrodynamics and beachrocks habitats constitute a complex system which remains very little understood and demands for further investigation.
AB - Beachrocks are common coastal formations, constructed through the lithification of beach sediments by carbonate cements. The objectives of the present contribution were to (a) assess the impacts of beachrock benthic communities on nearshore wave dynamics; (b) present a numerical model, developed to simulate wave propagation over shallow nearshore waters characterized by both loose sediment beds and colonized/non-colonized beachrocks; and (c) discuss the structure and dynamics of beachrock macro-benthic communities in an E. Mediterranean micro-tidal beach (Vatera, Lesbos Island, NE Aegean Sea), as well as their interactions with the wave forcing. Field measurements of wave height and flow velocity were processed to assess shoaling wave energy dissipation due to bottom friction from the colonized beachrock outcrops. The equivalent Nikuradse hydraulic roughness of the beachrock surface, estimated through spectral wave attenuation calculations, was found to be around kN=0.13m. The corresponding wave friction factors were incorporated into a wave propagation model to obtain estimates of the wave-induced bed shear stress τw acting on the beachrock benthic communities. Information about the structure and characteristics of the latter was obtained through the collection and analysis of samples from 15 stations along a beach transect, during two months of the year (April and September) and the results showed that benthic communities at the beachrock habitat were very similar to the ones typically found at NE Mediterranean hard substrates. Wave-induced bed shear stress τw values were able to explain cross-shore variations in population density and biomass, both decreasing significantly above water depths of about h=1.8-2m. The latter values corresponded, for the studied conditions, to shear stresses of about τw=2.2Nt/m2. The present findings clearly show that nearshore wave patterns not only control to a certain extent the spatial structure of the beachrock habitats, but can be also influenced by them. Thus, hydrodynamics and beachrocks habitats constitute a complex system which remains very little understood and demands for further investigation.
KW - Beachrocks
KW - Bed shear stress
KW - Benthic communities
KW - Hard substrate
KW - Mediterranean Sea
KW - Wave friction factor
UR - http://www.scopus.com/inward/record.url?scp=84867848740&partnerID=8YFLogxK
U2 - 10.1016/j.csr.2012.08.015
DO - 10.1016/j.csr.2012.08.015
M3 - Article
AN - SCOPUS:84867848740
VL - 48
SP - 100
EP - 109
JO - Continental shelf research
JF - Continental shelf research
SN - 0278-4343
ER -