Shoreline and beach volume change between 1967 and 2007 at Raine Island, Great Barrier Reef, Australia
Dawson, John L., and Smithers, Scott G. (2010) Shoreline and beach volume change between 1967 and 2007 at Raine Island, Great Barrier Reef, Australia. Global and Planetary Change, 72 (3). pp. 141-154.
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Raine Island is a vegetated coral cay located on the far northern outer Great Barrier Reef (GBR), recognised as a globally significant turtle rookery. Cay geomorphology, specifically the morphology of the beach and swale, dictate the availability of nesting sites and influence nesting success. Understanding short and long-term shoreline change is critical for managers charged with protecting the nesting habitat, particularly as climate change progresses. Historical topographic surveys, a simple numerical model and geographic information system (GIS) techniques were used to reconstruct a 40-year (1967–2007) shoreline history of Raine Island. Results show that significant shoreline change has occurred on 78% of the island's shoreline between 1967 and 2007; 34% experienced net retreat and 44% net progradation during the study interval. Shoreline retreat is mainly concentrated on the east–southeast section of the shoreline (average annual rate of−0.3±0.3 m/yr), while the shore on the western side of the island prograded at a similar rate (0.4±0.2 m/yr). A seasonal signal was detected relating to oscillations in wind direction and intensity, with the southeast and west–southwest shorelines migrating an average of ∼17 m from season to season. The volume of sediment deposited on Raine Island between 1967 and 2007 increased by ∼68,000 m3 net, but accretion rates varied significantly seasonally and from year to year. The largest volumetric changes have typically occurred over the last 23 years (1984–2007). Despite the recent concern that Raine Island is rapidly eroding, our data demonstrate net island growth (6% area, 4% volume) between 1967 and 2007. Perceptions of erosion probably reflect large morphological changes arising from seasonal, inter-annual and inter-decadal patterns of sediment redistribution rather than net loss from the island's sediment budget.
|Item Type:||Article (Refereed Research - C1)|
|Keywords:||sand cay; erosion; sediment transport; GIS; Great Barrier Reef; Raine Island; geomorphology; climate change|
|FoR Codes:||04 EARTH SCIENCES > 0406 Physical Geography and Environmental Geoscience > 040699 Physical Geography and Environmental Geoscience not elsewhere classified @ 30%|
04 EARTH SCIENCES > 0403 Geology > 040310 Sedimentology @ 30%
04 EARTH SCIENCES > 0403 Geology > 040305 Marine Geoscience @ 40%
|SEO Codes:||96 ENVIRONMENT > 9605 Ecosystem Assessment and Management > 960502 Ecosystem Assessment and Management of Antarctic and Sub-Antarctic Environments @ 100%|
|Deposited On:||10 Sep 2010 13:00|
|Last Modified:||18 May 2013 01:14|
Last 12 Months: 0
|Citation Counts with External Providers:||Web of Science: 4|
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