Encyclopedia of Coastal Science 2005
DOI: 10.1007/1-4020-3880-1_18
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Cited by 1 publication
(2 citation statements)
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“…In detail, according to [49,50], shoreline position records calculated for medium-(10-60 years) or long-term (>60 years) time spans, usually by means of aerial photos and satellite images, are needed to derive a reliable trend because the longer is the investigated time span the lower is the effect of seasonal variations and the influence of individual storms on shoreline evolution [51,52]. (2) Sediment Grain Size The size of gravel and boulders restricts their transport and hence a boulder or a cobble coast is much more stable than a sandy beach [53]. In this paper, assessment values regarding sediment size relevance were modified from [54].…”
Section: Determination Of the Erodibility Indexmentioning
confidence: 99%
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“…In detail, according to [49,50], shoreline position records calculated for medium-(10-60 years) or long-term (>60 years) time spans, usually by means of aerial photos and satellite images, are needed to derive a reliable trend because the longer is the investigated time span the lower is the effect of seasonal variations and the influence of individual storms on shoreline evolution [51,52]. (2) Sediment Grain Size The size of gravel and boulders restricts their transport and hence a boulder or a cobble coast is much more stable than a sandy beach [53]. In this paper, assessment values regarding sediment size relevance were modified from [54].…”
Section: Determination Of the Erodibility Indexmentioning
confidence: 99%
“…(i) Width Understanding the relationship between platform width and exposure of wave energy is complex [53]. The lack of a clear relationship reflects the strong influence that geology has in determining morphological characteristics.…”
Section: Determination Of the Erodibility Indexmentioning
confidence: 99%