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Determination of sediment budget and assessment of areas at risk from coastal hazards on the shore of northern France using airborne LiDAR.

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Abstract

Despite strong urbanization and development of major harbors during the 20th century, the coast of northern France still largely consists of coastal dunes of variable width associated with 500 to 800 m wide, gently sloping, macrotidal sand beaches characterized by series of shore-parallel intertidal bars. These coastal accumulation landforms, which often represent the only barrier protecting low elevation backshore areas from marine flooding, are particularly vulnerable to coastal hazards that may increase during the next decades due to sea level rise associated with climate change. Climate change may have dramatic impacts along the low unconsolidated coastlines of northern France, especially where sediment supply is limited, which may result in negative sediment budget and recurring coastal erosion. Although several studies have shown that the stability of the shoreline strongly depends on the local sediment budget, no studies have been conducted so far to evaluate the changes in the coastal sediment stock at the scale of the northern France region during recent years. The main objectives of this study are to determine shoreline changes and variations in sediment budget at the regional scale, to assess the role of changes in sediment volume on the stability of the shoreline, and to indentify the areas that are the most vulnerable to coastal hazards in the near future. This work is largely based on the acquisition and analysis of high-resolution topographic data of the entire littoral zone of northern France using a LiDAR (Light Detection and Ranging) airborne laser system for high precision (vertical error margin <± 15 cm), which gives a fine rendition of the topography over large areas. LiDAR complete coverage of the coastal fringe of the northern France was conducted in 2008-2009 and another full LiDAR survey of the coastal zone was completed in March 2011. Additional LiDAR data have also been obtained in September 2011 at two specific sites (East Dunkirk and Wissant Bay) where detailed in situ topographic measurements are regularly carried out. These spatially dense elevation data sets were used for determining topographic variations between 2008 and 2011 and for carrying out high-resolution 3D mapping of the coastal zone. The analysis of these evolutions allowed us to quantify sediment volume changes in coastal dunes and intertidal areas, including estuaries that represent major sediment sinks in the coastal zone of the region. This work was complemented by an analysis of storm surge frequency based on theoretical tidal elevations and tide gauge data recorded at the harbors of Dunkirk, Calais and Boulogne-sur-Mer during the last decades. Analysis of these time series of water levels enabled to estimate the return periods of high water levels. The combination of digital elevation data with these water level statistics allowed us to determine potentially sensitive areas that may be exposed to marine flooding, but also to other natural hazards such as coastal erosion.
Determination of sediment budget and assessment of areas at risk from coastal hazards
on the shore of northern France using airborne LiDAR
A.Crapoulet1, A.Héquette1 and A. Gardel1
1Laboratoire d’Océanologie et de Géosciences, UMR CNRS 8187 LOG, Université du
Littoral Côte d’Opale
Station Marine – 28, avenue Foch, BP 80 – 62930 Wimereux France
Adrien.Crapoulet@univ-littoral.fr, Arnaud.Hequette@univ-littoral.fr,
Antoine.Gardel@univ-littoral.fr
Despite strong urbanization and development of major harbors during the 20th century, the
coast of northern France still largely consists of coastal dunes of variable width associated
with 500 to 800 m wide, gently sloping, macrotidal sand beaches characterized by series of
shore-parallel intertidal bars. These coastal accumulation landforms, which often represent the
only barrier protecting low elevation backshore areas from marine flooding, are particularly
vulnerable to coastal hazards that may increase during the next decades due to sea level rise
associated with climate change. Climate change may have dramatic impacts along the low
unconsolidated coastlines of northern France, especially where sediment supply is limited,
which may result in negative sediment budget and recurring coastal erosion. Although several
studies have shown that the stability of the shoreline strongly depends on the local sediment
budget, no studies have been conducted so far to evaluate the changes in the coastal sediment
stock at the scale of the northern France region during recent years. The main objectives of
this study are to determine shoreline changes and variations in sediment budget at the regional
scale, to assess the role of changes in sediment volume on the stability of the shoreline, and to
indentify the areas that are the most vulnerable to coastal hazards in the near future.
This work is largely based on the acquisition and analysis of high-resolution topographic data
of the entire littoral zone of northern France using a LiDAR (Light Detection and Ranging)
airborne laser system for high precision (vertical error margin <± 15 cm), which gives a fine
rendition of the topography over large areas. LiDAR complete coverage of the coastal fringe
of the northern France was conducted in 2008-2009 and another full LiDAR survey of the
coastal zone was completed in March 2011. Additional LiDAR data have also been obtained
in September 2011 at two specific sites (East Dunkirk and Wissant Bay) where detailed in situ
topographic measurements are regularly carried out. These spatially dense elevation data sets
were used for determining topographic variations between 2008 and 2011 and for carrying out
high-resolution 3D mapping of the coastal zone. The analysis of these evolutions allowed us
to quantify sediment volume changes in coastal dunes and intertidal areas, including estuaries
that represent major sediment sinks in the coastal zone of the region. This work was
complemented by an analysis of storm surge frequency based on theoretical tidal elevations
and tide gauge data recorded at the harbors of Dunkirk, Calais and Boulogne-sur-Mer during
the last decades. Analysis of these time series of water levels enabled to estimate the return
periods of high water levels. The combination of digital elevation data with these water level
statistics allowed us to determine potentially sensitive areas that may be exposed to marine
flooding, but also to other natural hazards such as coastal erosion.
... Brock and Purkis 2009;Young and Ashford 2006;Kaczmarek 2015). Importantly, this method can be applied to the investigation of the shoreline recession of the soft-sediment as well as the rocky coast environments (Crapoulet et al. 2012;Earlie et al. 2015;Obu et al. 2016). ...
Article
Full-text available
The climate changes in recent years in the southern Baltic have been resulting in an increased frequency of natural extreme phenomena (i.e. storms, floods) and intensification of abrasion processes, which leads to introduction of large amounts of sedimentary deposits into the marine environment. The aim of this study was to determine the mercury load introduced to the Baltic Sea with deposits crumbling off the cliffs — parts of the coast that are the most exposed to abrasion. The studies were carried out close to five cliffs located on the Polish coast in the years 2011 – 2014. The results show that coastal erosion could be an important Hg source into the marine environment. This process is the third most important route, after riverine and precipitation input, by which Hg may enter the Gulf of Gdańsk. In the Hg budget in the gulf, the load caused by erosion (14.3 kg a−1) accounted for 80% of the wet deposition and was 50 % higher than the amount of mercury introduced with dry deposition. Although the Hg concentration in the cliff deposits was similar to the natural background, due to their large mass, this problem could be significant. In addition, the preliminary studies on the impact of coastal erosion on the Hg level in the marine ecosystem have shown that this process may be one of the Hg sources into the trophic chain.
... Dans une étude de l'évolution du trait de côte de la baie de Wissant de 1949de à 2000de , Aernouts et Héquette (2006 ont montré que l'érosion du littoral s'est presque entièrement généralisée à l'ensemble de la baie de- puis le milieu des années 1970, la seule exception étant le secteur de la Dune d'Amont, à l'est du village de Wissant, où le rivage a au contraire progressé vers le large pendant cette période en raison du développement de la dune. Des travaux plus récents ont toutefois montré que même le sec- teur de la Dune d'Amont a commencé à s'éroder entraînant un recul du trait de côte depuis le début des années 2000 (Crapoulet et al., 2012). Plusieurs hypothèses ont été évo- quées pour expliquer l'important recul du trait de côte que connait la baie de Wissant depuis plusieurs décennies, in- cluant une importante érosion des fonds à l'avant-côte (Aer- nouts et Héquette, 2006), mais également des variations morphologiques du Banc à la Ligne ( Chamley et al., 1987 ;Aernouts et Héquette, 2006) qui auraient eu des répercus- sions sur la propagation de la houle et la répartition de leur énergie le long du rivage (Héquette et al., 2013). ...
Article
Airborne topographic LiDAR surveys carried out between 2008 and 2014 over the coastal zone of the Bay of Wissant (northern France) were used for analyzing shoreline evolution and variations in sediment volumes in coastal dunes and across the beach. Successive storm events occurred at the end of 2013 and beginning of 2014 during which high water levels with return periods in excess of 10 years were responsible for significant coastal dune erosion. Although the shoreline retreat locally exceeded 20 m between 2008 and 2014, some areas were characterized by shoreline stability or even experienced a slight progradation due to the seaward progression of coastal dunes over the study period. The comparison of shoreline change with the initial sand volume on the upper beach in 2008 showed that the more significant retreat essentially took place where there was no upper beach at high tide. Our results also suggest that when a minimum sediment volume of 12 m3 m-1 is observed on the upper beach (i.e., above the mean high tide level), the shoreline is either stable or may prograde seaward, even when storms inducing high water levels with return periods > 10 years strike the coast. The identification of such a threshold in terms of sediment volume on the upper beach may represent a valuable contribution for improving the management of shoreline evolution in providing an estimate of minimum volumes of sand necessary to ensure shoreline stability.
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