Lord Howe Island study

by Terry Owen last modified Dec 03, 2007 10:54 AM
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Studying exchange processes in an island lagoon

Lord Howe Island, about 700km north east of Sydney, Australia, was recently the site of a measurement program using a number of Nortek instruments. The project involved a collaboration between the University of New South Wales at the Australian Defence Force Academy, University of Melbourne, and ASR Ltd in New Zealand. A lagoon about 1km wide on the western side of the island is bounded by a coral reef about 6km long. The above photo shows a view along the reef looking south toward Mt Gower (elev 875m) in the background. The measurement program covered the period November 26 to December 19, 2004 with the aim of measuring the relative contributions of wave, wind and tidally driven flows in the exchange of water between the lagoon and offshore.

 

Howe Island arial map

The instrument array is shown in the aerial photo. Five Nortek Aquadopps (denoted by adcp in the photo) were deployed; three in the major channels between the ocean and the lagoon, one in a blind channel and one offshore of the reef crest. Three Nortek Vectors (denoted by adv) were deployed on the reef crest and a Nortek AWAC was deployed offshore to provide directional wave information. The instrument array was completed with four Interocean S4 current meters and an Aanderaa tide gauge in the lagoon. The AWAC was deployed in 10m water depth on the forereef where the bottom was extremely rough (see photo). The maximum significant wave height recorded was about 2.2m. In the channels the Aquadopps were deployed on a much smoother bottom consisting of sand and coral rubble. The Vectors were deployed on the reef crest where the topography was moderately rough (see photo) and the instruments were subject to breaking waves and strong wave driven mean flows.

 

Howe Island deployed

The measurement program was very successful with 100% data return from all of the Nortek instruments. The data clearly show the importance of wave forcing in the mean flows with inflow over the reef crest and outflow through the channels at all stages of the tide. The data will be used in comparison with numerical simulations to model larval dispersal. These model results will then be used to compare with results from a continuing biological sampling program addressing the question of self recruitment versus long distance recruitment.

The article appears by courtesy of: Graham Symonds (University of New South Wales at the Australian Defence Force Academy), Stephen Swearer (University of Melbourne), and Kerry Black (ASR Ltd, New Zealand)

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