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Beach cusps: R. T. Guza and D. L. Inman, J. Geophys. Res. 80, 2997 (1975); B. T. Werner and T. M. Fink, Science 260, 968 (1993). Sand bars: A. J. Bowen and D. L. Inman, J. Geophys. Res. 76, 8662 (1971); M. J. F. Stive, Proc. 20th Coast. Eng. Conf. (Am. Soc. Civ. Eng.), p. 1550. Patterned ground: K. J. Gleason et al., Science 232, 216 (1986); M. A. Kessler et al., Eos 78, 270 (1997).
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0344475435
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note
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The separation of time scales required for slaving can be achieved if behavior on longer temporal and larger spatial scales is generated by self-organization (2) or by competitive interactions between emergent structures, permitting only similar or disparate scales, such as leads to uniform-sized sand dunes mantled by much smaller wind ripples.
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27
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0344906944
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note
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The hierarchical methodology presented here is objective, in that the levels and connections between levels are determined by dynamics and are testable, in contrast with a subjective, constructionist hierarchical framework previously proposed (17, 18).
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29
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See, for example, A. B. Murray and C. Paola, Nature 371, 54 (1994); R. S. Anderson and K. L. Bunas, ibid. 365, 740 (1993); C. G. Chase, Geomorphology 5, 39 (1992); B. T. Werner and B. Hallet, Nature 361, 142 (1993).
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Murray, A.B.1
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See, for example, A. B. Murray and C. Paola, Nature 371, 54 (1994); R. S. Anderson and K. L. Bunas, ibid. 365, 740 (1993); C. G. Chase, Geomorphology 5, 39 (1992); B. T. Werner and B. Hallet, Nature 361, 142 (1993).
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Anderson, R.S.1
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Chase, C.G.1
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Clifzon, H.E.1
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35
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0344044198
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note
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The top three images in Fig. 3 were acquired and processed by L. Clarke. Supported by a U.S. Navy-Office of Naval Research Scholar Award (N00014-97-1-0154) and the Andrew W. Mellon Foundation.
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