Longshore and Cross-Shore Morphological Variability of a Berm-Bar System under Low to Moderate Wave Energy

被引:3
|
作者
Lopez-Doriga, Uxia [1 ]
Ferreira, Oscar [1 ]
机构
[1] Univ Algarve, CIMA, Campus Gambelas, P-8005139 Faro, Portugal
关键词
Profile active zone; volumetric changes; storms; depth of closure; sediment transfer; VIDEO OBSERVATIONS; MACROTIDAL BEACH; SANDY BEACH; NEARSHORE; MORPHODYNAMICS; TRANSPORT; EXAMPLES; BEHAVIOR; CURRENTS; ISLAND;
D O I
10.2112/JCOASTRES-D-16-00050.1
中图分类号
X [环境科学、安全科学];
学科分类号
08 ; 0830 ;
摘要
The morphological variability of a berm-bar system is highly dependent on wave conditions with direct consequences for the evolution of the nearby coast; however, an understanding of this variability based on field measurements is still lacking, in particular with respect to the assessment of both longshore and cross-shore components. In this study, the berm-bar morphological changes were assessed by simultaneously measuring longshore and cross-shore variability as well as the forcing mechanisms (i.e. wave conditions). A sandy beach in southern Portugal (Tavira Barrier Island, Ria Formosa) was surveyed from the dune crest to 20-m depth along six profiles over a period of 16 months. Wave time series between surveys were analysed to obtain relationships between wave conditions, the depth of closure, and berm-bar variations. For the surveyed period, waves approached mainly from the W-SW (78% of the time) and E-SE (18%), and eight moderate storms were recorded. Results show that the active zone of the profiles descends to 6 m below mean sea level (MSL), the maximum depth of closure registered. On the basis of the pattern of vertical variability, the profiles can be divided into three cross-shore sectors: A (emerged beach and berm), B (subtidal terrace), and C (submerged longshore bar). A new index (longshore vs. cross-shore [LvC]) is proposed, relating the dominance of longshore or cross-shore processes to volumetric changes resulting from sediment transport. In the study area, cross-shore sediment transfer (LvC similar to 0) dominated when the largest and longest storms occurred and is associated with storm erosion and poststorm recovery. Longshore dominance (LvC similar to 1 and 1 for erosion and accretion, respectively) occurred during periods with smaller and shorter storms. The proposed index allows the relative roles of cross-shore vs. longshore processes in coastal areas with berm-bar interaction to be distinguished.
引用
收藏
页码:1161 / 1171
页数:11
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