Description of littoral, alongshore sediment movement from empirical eigen‐function analysis
作者:
D. J. Clarke,
I. G. Eliot,
期刊:
Journal of the Geological Society of Australia
(Taylor Available online 1982)
卷期:
Volume 29,
issue 3-4
页码: 327-341
ISSN:0016-7614
年代: 1982
DOI:10.1080/00167618208729217
出版商: Taylor & Francis Group
关键词: Beach;sediment movement;swash processes;tidal and current processes;eigen‐function analysis
数据来源: Taylor
摘要:
Measurements of 18 closely spaced beach profiles spanning Warilla Beach, N.S.W., over a 5‐year period have been examined for alongshore exchanges in beachface configuration. Horizontal slices of beach corresponding with berm, upper swash, upper and lower intertidal zones were examined by empirical orthogonal function (EOF) analysis. The first four EOF's for each of the four slices contain over 90% of the total variance for each slice. In each instance the first eigen‐function mode represents the onshore‐offshore component of beach response, and accounts for 50 to 60% of the variance. Subsequent modes describe alongshore exchange of sediment associated with large, standing, cellular water circulations of the embayment. Sediment shunts along each horizontal slice are determined by identification of nodal points in the eigen‐functions. These represent pivotal points through which sediment is transferred. The patterns of exchange vary considerably from slice to slice, reflecting change in the dominant beach processes from swash processes in the top of the beach to wave, tidal and current processes on the lower beach slope. Despite their disparity, similar periodicities are determined for the sediment exchanges in each slice. The amplitude spectra of the time series associated with each eigen‐function indicate that the exchanges take place at 24, 12 and 6 monthly periods.
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