2015
DOI: 10.3176/proc.2015.3.06
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Quantification of changes in the beach volume by the application of an inverse of the Bruun Rule and laser scanning technology

Abstract: We address the possibilities of combining terrestrial (TLS) and airborne laser scanning (ALS) techniques with the classical concept of equilibrium beach profile to quantify the changes in the total sand volume of slowly evolving sandy beaches. The changes in the subaerial beach are determined from a succession of ALS surveys that were reduced to the same absolute height using a TLS survey of a large horizontal surface of constant elevation. The changes in the underwater sand volume from the waterline down to t… Show more

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Cited by 11 publications
(6 citation statements)
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References 22 publications
(65 reference statements)
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“…A simple consequence of the intermittency and anisotropy of wave fields and the complicated geometry of the coast is that the evolution of Baltic Sea shores is a step-like process (Soomere and Healy, 2011): A few events cause rapid changes when strong waves arrive from specific directions during events with high water levels (Tõnisson et al, 2013b). But for most of the time changes are very slow and require high-resolution measurements such as laser scanning techniques (Eelsalu et al, 2015;Sergeev et al, 2018) to be detected. The anisotropy of the wave climate combined with the orientation of large sections of the shoreline leads to a large-scale asymmetry of the sediment flux (that is mostly counter-clockwise on the shore of the Baltic Sea proper; Soomere and Viška, 2014; Figure 3).…”
Section: )mentioning
confidence: 99%
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“…A simple consequence of the intermittency and anisotropy of wave fields and the complicated geometry of the coast is that the evolution of Baltic Sea shores is a step-like process (Soomere and Healy, 2011): A few events cause rapid changes when strong waves arrive from specific directions during events with high water levels (Tõnisson et al, 2013b). But for most of the time changes are very slow and require high-resolution measurements such as laser scanning techniques (Eelsalu et al, 2015;Sergeev et al, 2018) to be detected. The anisotropy of the wave climate combined with the orientation of large sections of the shoreline leads to a large-scale asymmetry of the sediment flux (that is mostly counter-clockwise on the shore of the Baltic Sea proper; Soomere and Viška, 2014; Figure 3).…”
Section: )mentioning
confidence: 99%
“…Although many of the cells are quite large, many are also small (Soomere et al, 2007), requiring modeling and measurements at a much finer scale than is currently available. An approach to comprehensively quantify sediment budget regions with small-scale sedimentary compartments could be to combine (airborne and terrestrial) laser scanning measurements (Eelsalu et al, 2015) and detailed bathymetric data with high-resolution, possibly phase-resolving simulations of the nearshore wave climate. Underwater sediment transport and distribution changes could be roughly estimated from approximations such as inverse Bruun's Rule (Eelsalu et al, 2015), however more sophisticated techniques should be developed that take systematically into account the alongshore transport.…”
Section: Coastline Changes and Erosionmentioning
confidence: 99%
“…The most extreme erosion events will occur when such a combination comes along with high, normally storm-surge-related, water levels (Tõnisson et al, 2013b). However, most of the time, changes are very slow and require high-resolution measurements, such as laser scanning techniques (Eelsalu et al, 2015;Sergeev et al, 2018), to be detected. The anisotropy of the wave climate combined with the orientation of large sections of the shoreline leads to a large-scale asymmetry of the sediment flux (which is mostly counterclockwise on the shore of the Baltic Sea proper; Figs.…”
Section: Variability and Change In Erosion And Sedimentationmentioning
confidence: 99%
“…The presentday water level is about 2 m below the 1731 mark (photo courtesy of Martin Ekman). (b) Stockholm annual sea level variations (black) and land rise (red) according to Ekman (2003) (redrawn from Omstedt, 2015). ment transport.…”
Section: Introductionmentioning
confidence: 99%
“…For example, such MLS can also be used for quantifying the erosion and sedimentation over long portions of sand beaches. Our previous studies (Julge et al, 2014b, Eelsalu et al, 2015 have exploited both TLS and ALS data for this purpose. However, TLS survey is very time-and labour-consuming, whereas ALS data (acquired during national mapping campaigns) are not always available nor up-to-date.…”
Section: Conclusion and Future Researchmentioning
confidence: 99%