Shoreline variability of an urban beach fronted by a beachrock reef from video imagery
| Autor: | Th. Hasiotis, Isavela N. Monioudi, F. Psarros, Michalis Vousdoukas, George Ghionis, O. Andreadis, Antonios Chatzipavlis, Vasilis Trygonis, Adonis F. Velegrakis, Th. V. Karambas |
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| Rok vydání: | 2016 |
| Předmět: |
Beachrock
Shore Atmospheric Science geography geography.geographical_feature_category 010504 meteorology & atmospheric sciences Elevation 010502 geochemistry & geophysics Inlet 01 natural sciences Oceanography Earth and Planetary Sciences (miscellaneous) Submarine pipeline Geomorphology Reef Geology Beach morphodynamics Rip current 0105 earth and related environmental sciences Water Science and Technology |
| Zdroj: | Natural Hazards. 83:201-222 |
| ISSN: | 1573-0840 0921-030X |
| Popis: | This contribution presents the results of a study on the shoreline variability of a natural perched urban beach (Ammoudara, N. Crete, Greece). Shoreline variability was monitored in high spatio-temporal resolution using time series of coastal video images and a novel, fully automated 2-D shoreline detection algorithm. Ten-month video monitoring showed that cross-shore shoreline change was, in some areas, up to 8 m with adjacent sections of the shoreline showing contrasting patterns of beach loss or gain. Variability increased in spring/early summer and stabilized until the end of the summer when partial beach recovery commenced. Correlation of the patterns of beach change with wave forcing (as recorded at an offshore wave buoy) is not straightforward; the only discernible association was that particularly energetic waves from the northern sector can trigger changes in the patterns of shoreline variability and that increased variability might be sustained by increases in offshore wave steepness. It was also found that the fronting beachrock reef exerts significant geological control on beach hydrodynamics. Hydrodynamic modelling and observations during an energetic event showed that the reef can filter wave energy in a highly differential manner, depending on its local architecture. In some areas, the reef allows only low-energy waves to impinge on the shoreline, whereas elsewhere penetration of higher waves is facilitated by the low elevation and limited width of the reef or by the presence of an inlet. Wave/reef interaction can also generate complex circulation patterns, including rip currents that appeared to be also constrained by the reef architecture. |
| Databáze: | OpenAIRE |
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