IMIS | Flanders Marine Institute

Flanders Marine Institute

Platform for marine research


Publications | Institutes | Persons | Datasets | Projects | Maps
[ report an error in this record ]basket (0): add | show Printer-friendly version

Oceanic inflow from the Coral Sea into the Great Barrier Reef
Brinkman, R.; Wolanski, E.; Deleersnijder, E.; McAllister, F.; Skirving, W. (2002). Oceanic inflow from the Coral Sea into the Great Barrier Reef. Est., Coast. and Shelf Sci. 54(4): 655-668.
In: Estuarine, Coastal and Shelf Science. Academic Press: London; New York. ISSN 0272-7714, more
Peer reviewed article  

Available in  Authors 
    VLIZ: Open Repository 29183 [ OMA ]

    Mass transport; Mathematical models; Shelf dynamics; Water circulation; Australia [Marine Regions]; ISEW, East Australian Current; ISEW, Great Barrier Reef [Marine Regions]; PSE, East Australian Current; Marine
Author keywords
    water circulation; shelf dynamics; mass transport; numerical model; East Australian Current; Great Barrier Reef; Australia

Authors  Top 
  • Brinkman, R.
  • Wolanski, E., more
  • Deleersnijder, E., more
  • McAllister, F.
  • Skirving, W.

    Long-term current meter data from the continental shelf region of the Great Barrier Reef show that there exists a zone of oceanic inflow onto the shelf. This oceanic inflow splits into two branches on meeting the continental shelf slope, resulting in two net longshore currents on the slope, one to the north and the other to the south of the separation point. In 1981 this separation point was located between 17°S and 18°S. This circulation was successfully predicted using a depth-averaged two-dimensional model in which the regional sea level gradient is explicitly added in the momentum equations. The resulting circulation on the continental shelf is controlled by an oceanic inflow of 0·58 Sv, spread over 500 km of the shelf edge both north and south of the separation point. The inflow appears measurably impeded by the presence of coral reefs, with >50% of the inflow occurring in a 150 km long area where reef density is small. Satellite images confirm this spatial variability. Longshore currents on the shelf generated by the inflow are modulated by the wind and tides, which can deflect the mean current away from areas of high reef density and generate localized outflows to the Coral Sea. Oceanic inflow is believed to be important because it flushes the shelf even in the absence of wind; it controls the dominant direction of across-shelf and along-shelf spread of spawn material from reefs; it makes it possible for upwelled water to spread quickly over the GBR shelf; it may also protect coral reefs by preventing river plumes from spreading onto the outer shelf

All data in IMIS is subject to the VLIZ privacy policy Top | Authors