Simulating decadal coastal morphodynamics
Simulating decadal coastal morphodynamics
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DOI:
10.1016/j.geomorph.2015.10.015
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发表时间:
2016-03
期刊:
影响因子:
3.9
通讯作者:
R. Nicholls;J. French;B. Maanen
中科院分区:
文献类型:
--
作者:
R. Nicholls;J. French;B. Maanen
Coastal geomorphic systems provide many services of key importance to humankind, including protection from flood and erosion hazards, diverse habitats and amenity values (Agardy et al., 2005; Jones et al., 2011). However, these systems are widely undergoing degradation that can be substantially attributed to the cumulative direct and indirect effects of human interference. Declining sediment inputs and throughputs are frequently a factor driving a shift towards progressive coastal erosion (Valiela, 2006; Nicholls et al., 2007). Such sediment starved systems have reduced resilience and are further threatened by humaninduced climate change, not only due to accelerated sea-level rise, but also through possible shifts in wave and surge climate (Wong et al., 2014).At the same time, society is starting to plan more strategically to protect and sustain growing coastal populations and economies, as well as to counter habitat decline (Nicholls et al., 2013). This inevitably leads to the challenge of predicting coastal geomorphic behaviour at what we term here the mesoscale (of the order of 10 1 to 10 2 km length scales and 10 1 to 10 2 year timescales). Geomorphic evolution at this scale involves a broad range of drivers that govern the functioning of coastal systems and determine how they will respond to external disturbances. As well as natural processes, the role of human intervention needs to be considered, including the pervasive legacy of engineering interventions over the preceding decades and even longer.