Simulating cross-shore material exchange at decadal scale. Model application

被引:24
|
作者
Palalane, Jaime [1 ,2 ]
Fredriksson, Caroline [1 ]
Marinho, Barbara [3 ,4 ]
Larson, Magnus [1 ]
Hanson, Hans [1 ]
Coelho, Carlos [3 ,4 ]
机构
[1] Lund Univ, Dept Water Resources Engn, Box 118, S-22100 Lund, Sweden
[2] Eduardo Mondlane Univ, Dept Civil Engn, CP 257, Maputo, Mozambique
[3] Univ Aveiro, RISCO, P-3810193 Aveiro, Portugal
[4] Univ Aveiro, Dept Civil Engn, P-3810193 Aveiro, Portugal
关键词
Cross-shore transport; Mathematical model; Long-term profile evolution; Regional coastal evolution; Dune erosion; Overwash; Wind-blown sand; Bar volume; Angelholm; Barra; Macaneta; CLIMATE-CHANGE; AVEIRO COAST; PROFILE; EROSION;
D O I
10.1016/j.coastaleng.2016.05.007
中图分类号
TU [建筑科学];
学科分类号
0813 ;
摘要
A model developed to describe long-term cross-shore (CS) exchange of sand and resulting profile evolution at regional scale was employed to simulate the evolution at three different sites. The model consists of modules for calculating dune erosion and overwash, bar-berm material exchange, and dune build-up by wind-blown sand transport, as described in detail in a companion paper (Larson et al., 2016). Selected study sites represent coastal stretches influenced by beach nourishment (Barra in Portugal), overwash and breaching (Macaneta spit in Mozambique), and dune development (Angelholm in Sweden). The model applications showed overall good performance and the results of the simulations are promising. Due to limitations in data availability in Angelholm and Macaneta, values on calibration parameters were mainly determined based on previous studies. For Barra, where more field measurements were available, the application showed good agreement between the simulated results and observations. The CS-model proved to be a useful tool to predict long-term evolution of beach-dune systems in a time perspective from years to decades. However, additional efforts should be directed towards improving the schematized model profile so that it can better represent other beach shapes such as a sloping berm or a barrier shape. (C) 2016 Elsevier B.V. All rights reserved.
引用
收藏
页码:26 / 41
页数:16
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