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As stated in the introduction, a true definition of SLR remains elusive and superficial. Rather, multiple definitions exist simply due to the lack of consensus or lack of calculation (Murdoch et al., 20141106; Gogola et al., 20161107; IAM, 20161108). It is also important to note that there is no single term or measure that can definitely be considered representative of SLR. Therefore, we have selected the term SLR for this chapter, but we should recognise that, based on indicative maps, a SLR of up to 5 feet is more or less equivalent to a rise of 4 feet. Hence, the term SLR refers to a change of between 0.08 and 0.25 metre, which represents a 10% increase in sea level. There are several metrics that can be useful to consider in the SLO modelling. One of these is as follows:
Ethnic groups have a traditional knowledge of the coastline, which they often hold as a collective inheritance. One example is the seagoing Fulani community in northern Nigeria, whose knowledge of the shoreline is transmitted from generation to generation by oral traditions and a unique system of naming the coastal features known as Ketene (Njike et al., 20145111; Diabaté et al., 20151112; Laderman et al., 20161117; Moses et al., 20161118; Van der Hammen et al., 20101113). This community has adapted their local livelihood to the changing conditions of tidal marsh ecosystems. d2c66b5586
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