Beach Morphology and Sediment Budget Variability Based on High Quality Digital Elevation Models Derived from Field Data Sets
Mohammed Taaouati, El Mrini Abdelmounim, Driss Nachite
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DOI: 10.4236/ijg.2011.22012   PDF    HTML     5,253 Downloads   10,382 Views   Citations

Abstract

The morphological and volumetric changes of a sandy beach were investigated through a series of two- monthly filed surveys carried out aver a 2-year period from April 2005 to January 2007. This paper discuss the ability of 3-D digital elevation models (DEMs) derived from high accurate data to assess and quantify beach morphodynamics in relation with wave forcing. The methodology and data acquisition are described and consist mainly in the production of interpolated DEMs from which a variety of representations can be made, including as elevation change maps, two-dimensional cross-sections of the beach, calculation of net volume. The results of the analysis highlight seasonal changes in beach morphology due to variations in wave energy. This behavior is characterized by beach erosion and bar decay under high-energy waves and net accretion and bar formation during relatively fair weather conditions. The sand budgets adjustments show that the loss of volume in the winter months is compensated for by accumulation to the beach during summer. This trend suggests that there is a mechanism which controls the beach evolution. The correlation between beach changes and wave energy variations highlights a net relation between them. The results from this in- vestigation state the value of DEMs utilized and demonstrate the efficiency of the 3-D approach employed here to assess the erosion and accretion patterns which would not be visualized using 2-D profiles.

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M. Taaouati, E. Abdelmounim and D. Nachite, "Beach Morphology and Sediment Budget Variability Based on High Quality Digital Elevation Models Derived from Field Data Sets," International Journal of Geosciences, Vol. 2 No. 2, 2011, pp. 111-119. doi: 10.4236/ijg.2011.22012.

Conflicts of Interest

The authors declare no conflicts of interest.

References

[1] M. Ortega-Sánchez, et al., “Relation between Beachface Morphology and Wave Climate at Trafalgar Beach (Cádiz, Spain),” Geomorphology, Vol. 99, No. 1-4, 2008, pp. 171-185.
[2] B. D. Andrews, P. A. Gares and J. D. Colby, “Techniques for GIS Modeling of Coastal Dunes,” Geomorphology, Vol. 48, No. 1-3, 2002, pp. 289-308. doi:10.1016/S0169-555X(02)00186-1
[3] G. Anfuso, J. A. Martínez del Pozo, D. Nachite, J. Benavente and A. Macias, “Morphological Characteristics and Med- ium-Term Evolution of the Beaches between Ceuta and Cabo Negro (Morocco),” Environmental Geology, Vol. 52, No. 5, 2007, pp. 933-946. doi:10.1007/s00254-006-0535-3
[4] V. Chaplot, F. Darboux, H. Bourennane, S. Leguédois, N. Silvera and K. Phachomphon, “Accuracy of Interpolation Techniques for the Derivation of Digital Elevation Mo- dels in Relation to Landform Types and Data Density,” Geomorphology, Vol. 77, No. 1-2, 2006, pp. 126-141. doi:10.1016/j.geomorph.2005.12.010
[5] G. L. Heritage, D. J. Milan, A. R. G. Large and I. C. Fuller, “Influence of Survey Strategy and Interpolation Model on DEM Quality,” Geomorphology, Vol. 112, No. 3-4, 2009, pp. 334-344. doi:10.1016/j.geomorph.2009.06.024
[6] F. Duplantier and P. Lesueur, “Les Sables du Littoral Atlantique Nord-Marocain: Origines et Mode de Mise en Place [Sand on the North-Moroccan Atlantic Coast: Origins and Depositional Modes],” Bulletin de l’Institut Géologique du Bassin d’Aquitaine, Vol. 33, 1983, pp. 5-24.
[7] P. Cirac, A. D. Resseguier and O. Weber, “Situation Cou- rantologique et Hydrologique Sur le Plateau Con- tinental Atlantique Nord-Marocain: Mission Géomar II [Hy- drological structure on the North Atlantic Moroccan Shelf: Cruises Géomar II],” Bulletin de l’Institut Géologique du Bassin d’Aquitaine, Vol. 46, 1989, pp. 81-95.
[8] E. B. Jaaidi and P. Cirac, “La Couverture Sédimentaire Meuble du Plateau Continental Atlantique Marocain Entre Larache et Agadir [The soft Sedimentary Cover of the Moroccan Atlantic Continental Shelf between Larache and Agadir],” Bulletin de l’Institut Géologique du Bassin d’Aquitaine, Vol. 42, 1987, pp. 33-51.
[9] M. Taaouati, D. Nachite, J. Benavente and A. E. Mrini, “Seasonal Changes and Morphodynamic Behavior of a High-Energy Mesotidal Beach: Case Study of Charf el Akab Beach on the North Atlantic Coast of Morocco,” Environmental Earth Sciences, submitted for publication, 2011. doi: 10.1007/s12665-011-0937-8
[10] H. Günther, S. Hasselmann and P. A. E. M. Janssen, “The WAM Model Cycle 4 (Revised Version),” Technical Re- port, Deutsches Klima Rechenzentrum, Hamburg, 1992.
[11] USACE, “Coastal Hydrodynamics,” Coastal Engineering Manual, No. 1110-2-1100 (Part II), United States Army Corps of Engineers, Vicksburg, 2008, p. 608.
[12] D. C. Masson, C. Gurney and M. Kennett, “Beach Topography Mapping—A Comparison of Techniques,” Journal of Coastal Conservation, Vol. 6, No. 1, 2000, pp. 113-124.
[13] J. D. Huang, D. W. T. Jackson and J. A. G. Cooper, “Morphological Monitoring of a High Energy Beach System Using GPS and Total Station Techniques, Run- kerry, Co. Antrim, Northern Ireland,” Journal of Coastal Research, Vol. 36, No. 36, 2002, pp. 390-398.
[14] G. Masselink and B. Hegge, “Morphodynamics of Meso- and Macrotidal Beaches: Examples from Central Queens- land, Australia,” Marine Geology, Vol. 129, No. 1-2, 1995, pp. 1-23. doi:10.1016/0025-3227(95)00104-2

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