Dune Landscape Rejuvenation by Intended Destabilization in the … · 2016. 7. 26. · 1168 Journal...

1167

Journal of Coastal Research, Vol. 22, No. 5, 2006

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1168


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1170


Figure 11 from ‘‘Dune Landscape Rejuvenation by Intended Destabilization in the Amsterdam Water Supply Dunes’’ by S.M. Arens and L.H.W.T. Geelen, pp.1094–1107. Year-to-year variation in sand burial; from top to bottom: summer 1999; winter and summer 2000; and winters 2001, 2002, and 2003.

1171


Figure 11 from ‘‘Dune Landscape Rejuvenation by Intended Destabilization in the Amsterdam Water Supply Dunes’’ by S.M. Arens and L.H.W.T. Geelen, pp.1094–1107. Continued.

1172


Figure 4 from ‘‘Use of Airborne Hyperspectral Data and Laserscan Data to Study Beach Morphodynamics along the Belgian Coast’’ by Bart Deronde, RikHouthuys, Walter Debruyn, Dirk Fransaer, Vera Van Lancker, and Jean-Pierre Henriet, pp. 1108–1117. Classification image (2000 survey) of the beachbetween Blankenberge and Zeebrugge from the Spectral Angle Mapper classifications. Eight different sand types could be distinguished (labeled 2–9 inthe legend; class 1 is water and class 10 is vegetation).

Figure 7 from ‘‘Use of Airborne Hyperspectral Data and Laserscan Data to Study Beach Morphodynamics along the Belgian Coast’’ by Bart Deronde, RikHouthuys, Walter Debruyn, Dirk Fransaer, Vera Van Lancker, and Jean-Pierre Henriet, pp. 1108–1117. Classification image (2001 survey) of the beach nearKnokke-Zoute from the Spectral Angle Mapper classifications. Eight different sand types can be distinguished (labeled 2–9 in the legend; class 1 is waterand class 10 is vegetation). The numbers ranging from 235 to 247 are beach survey sections.

1173


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Dune Landscape Rejuvenation by Intended Destabilization in the … · 2016. 7. 26. · 1168 Journal...

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