DOI: 10.18174/532101
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Biogeomorphic feedback drives dune development along nourished coastlines

Abstract: Ch. 1 Introduction Ch. 2 Accommodation space indicates dune development potential along an urbanized and frequently nourished coastline Ch. 3 Synchronous long-term measurements to characterize aeolian transport dynamics on a mega-scale beach nourishment Ch. 4 Measuring and modeling the effect of surface moisture on the spectral reflectance of coastal beach sand Ch. 5 UAV-imaging to model growth response of marram grass to sand burial: Implications for coastal dune development Ch. 6

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“…Marram grass can grow along with depositions of up to 1 m/y due to its layered root system and is thus an effective bio-builder. A burial rate of 30 cm per season provides the ideal circumstances for marram grass to grow, with a maximum of 80-100 cm per year (Nolet, 2021). Marram grass is vulnerable to saltwater intrusion and therefore occurs mostly at the upper beach and foredune zone (Van Dieren, 1934;Klijn, 1981), where new seedlings cluster around the deposition tails of grown, half-buried versions (Figure 3.45).…”
Section: Tocmentioning
confidence: 99%
“…Marram grass can grow along with depositions of up to 1 m/y due to its layered root system and is thus an effective bio-builder. A burial rate of 30 cm per season provides the ideal circumstances for marram grass to grow, with a maximum of 80-100 cm per year (Nolet, 2021). Marram grass is vulnerable to saltwater intrusion and therefore occurs mostly at the upper beach and foredune zone (Van Dieren, 1934;Klijn, 1981), where new seedlings cluster around the deposition tails of grown, half-buried versions (Figure 3.45).…”
Section: Tocmentioning
confidence: 99%