FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W4366977450> ?p ?o ?g. }

• W4366977450 endingPage "102973" @default.
• W4366977450 startingPage "102973" @default.
• W4366977450 abstract "A unique dataset of 27 years of shoreline changes along the western coast of Cotentin Peninsula (Normandy, France) with a high temporal resolution (about 60 fields surveys) provides an opportunity to analyse the space and time variability of a tidal sandy wave-exposed shoreline and to identify the main drivers of this variability. Spatially, as often observed around the world, this coast shows a clear balance between erosional and accretionary sectors. Maximum shoreline retreat and mean annual erosional rates are, however, greater by a factor of two than maximum and mean accretion rates, with hotspots mainly observed in the vicinity of tidal inlets. A cluster analysis highlighted nine groups of shoreline behaviour that show important contrasts, depending on locations, between erosional and accretionary trends. Linear trends over the nearly three decades of monitoring are uncommon and reverse trends are frequent. Clear divergences in behaviour were observed over the same time periods depending on location, e.g., erosion and accretion can be contemporaneous as can accretion and stability, independently of the antecedent multi-annual trends. Ebb delta zones show heterogeneous patterns, and survey locations belonging to the same clusters appear spatially scattered. The temporal shoreline behaviour can be linked to combinations of high wave energy and high spring tides only for at best 37.5% of the survey locations, and this only over the last decade. No obvious link with mean sea-level rise and the 18.6 y lunar tidal cycle was observed. However, as in the case of wave activity, these external drivers can often be masked by local factors such as inlet dynamics or/and anthropogenic influences (essentially shoreline engineering). Further insight on sand supply and beach elevation changes is necessary to improve the understanding of the main factors driving space and time variability in shoreline mobility, and it is expected that sea-level rise in the future will be of increasing concern, with important, potentially negative, implications for shoreline mobility on the low sandy sectors of the Normandy coast." @default.
• W4366977450 created "2023-04-27" @default.
• W4366977450 creator A5045048829 @default.
• W4366977450 creator A5055203646 @default.
• W4366977450 creator A5081628745 @default.
• W4366977450 date "2023-09-01" @default.
• W4366977450 modified "2023-09-25" @default.
• W4366977450 title "Multi-decadal shoreline mobility of a managed sandy tidal coast (Normandy, France): Behavioural variability in a context of sea-level rise and increasing storm intensity" @default.
• W4366977450 cites W1487177596 @default.
• W4366977450 cites W1505974718 @default.
• W4366977450 cites W1968936568 @default.
• W4366977450 cites W1973132854 @default.
• W4366977450 cites W1975186752 @default.
• W4366977450 cites W1978030580 @default.
• W4366977450 cites W1985182130 @default.
• W4366977450 cites W1986540456 @default.
• W4366977450 cites W1990036228 @default.
• W4366977450 cites W1993195633 @default.
• W4366977450 cites W2006673484 @default.
• W4366977450 cites W2014431014 @default.
• W4366977450 cites W2015414214 @default.
• W4366977450 cites W2018322332 @default.
• W4366977450 cites W2019260987 @default.
• W4366977450 cites W2023429321 @default.
• W4366977450 cites W2027631897 @default.
• W4366977450 cites W2041744576 @default.
• W4366977450 cites W2042255117 @default.
• W4366977450 cites W2046013777 @default.
• W4366977450 cites W2056254080 @default.
• W4366977450 cites W2058747386 @default.
• W4366977450 cites W2066512275 @default.
• W4366977450 cites W2072786341 @default.
• W4366977450 cites W2073748894 @default.
• W4366977450 cites W2078860096 @default.
• W4366977450 cites W2088796769 @default.
• W4366977450 cites W2091873982 @default.
• W4366977450 cites W2092805829 @default.
• W4366977450 cites W2098775769 @default.
• W4366977450 cites W2099778733 @default.
• W4366977450 cites W2103585617 @default.
• W4366977450 cites W2105942710 @default.
• W4366977450 cites W2110621574 @default.
• W4366977450 cites W2111045719 @default.
• W4366977450 cites W2111726831 @default.
• W4366977450 cites W2121295996 @default.
• W4366977450 cites W2125901020 @default.
• W4366977450 cites W2128014304 @default.
• W4366977450 cites W2144427418 @default.
• W4366977450 cites W2146754360 @default.
• W4366977450 cites W2155161125 @default.
• W4366977450 cites W2160540655 @default.
• W4366977450 cites W2167030799 @default.
• W4366977450 cites W2266617176 @default.
• W4366977450 cites W2322930025 @default.
• W4366977450 cites W2326596904 @default.
• W4366977450 cites W2466078552 @default.
• W4366977450 cites W2497060941 @default.
• W4366977450 cites W2514117783 @default.
• W4366977450 cites W2560130412 @default.
• W4366977450 cites W2577061241 @default.
• W4366977450 cites W2577270457 @default.
• W4366977450 cites W2604594859 @default.
• W4366977450 cites W2604879303 @default.
• W4366977450 cites W2607882288 @default.
• W4366977450 cites W2735015065 @default.
• W4366977450 cites W2767074716 @default.
• W4366977450 cites W2770391880 @default.
• W4366977450 cites W2782481028 @default.
• W4366977450 cites W2796047770 @default.
• W4366977450 cites W2888493296 @default.
• W4366977450 cites W2905747096 @default.
• W4366977450 cites W2910533402 @default.
• W4366977450 cites W2938672244 @default.
• W4366977450 cites W2941409255 @default.
• W4366977450 cites W2942389611 @default.
• W4366977450 cites W2964908798 @default.
• W4366977450 cites W3004760715 @default.
• W4366977450 cites W3005493472 @default.
• W4366977450 cites W3010403880 @default.
• W4366977450 cites W3022683052 @default.
• W4366977450 cites W3032987234 @default.
• W4366977450 cites W3087193216 @default.
• W4366977450 cites W3093234102 @default.
• W4366977450 cites W4214852840 @default.
• W4366977450 cites W4226479162 @default.
• W4366977450 cites W4282946811 @default.
• W4366977450 cites W4291281891 @default.
• W4366977450 doi "https://doi.org/10.1016/j.rsma.2023.102973" @default.
• W4366977450 hasPublicationYear "2023" @default.
• W4366977450 type Work @default.
• W4366977450 citedByCount "0" @default.
• W4366977450 crossrefType "journal-article" @default.
• W4366977450 hasAuthorship W4366977450A5045048829 @default.
• W4366977450 hasAuthorship W4366977450A5055203646 @default.
• W4366977450 hasAuthorship W4366977450A5081628745 @default.
• W4366977450 hasConcept C100970517 @default.
• W4366977450 hasConcept C105306849 @default.
• W4366977450 hasConcept C111368507 @default.

• next