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Estuarine Circulation in the Rewa River, Fiji Edward Anderson - PowerPoint PPT Presentation

Estuarine Circulation in the Rewa River, Fiji Edward Anderson University of the South Pacific Aquatic Science Pacific aquascipac@gmail.com Crew We had an army of student volunteers From 2004 through 2010, we sampled the Rewa


  1. Estuarine Circulation in the Rewa River, Fiji Edward Anderson University of the South Pacific Aquatic Science Pacific aquascipac@gmail.com

  2. Crew • We had an army of student ”volunteers” • From 2004 through 2010, we sampled the Rewa River in September or October. • There were about 20 to 60 each class

  3. Boats • Halimeda is a 7.3 m vessel powered by two 150 hp outboard motors . • Hali can take about 15 students. • We took about 2 to 4 cruises per year

  4. What are we trying to achieve? What kind of estuary is this? What is the effect of the recent dredging?

  5. Schedule • We embarked at 0800n and returned at 1300 so that students could go to their next class • Organization, travel time and unloading time left only about 2hr to2.5hr on station. • We completed between 10 and 15 stations • We used CTD and droughes for each station

  6. Estuarine types • Where river flow is strong, and tidal currents weak, salt- wedge type estuaries are favored • A partially mixed estuary where river flow and tidal mixing are about equal. Most estuaries are of this type. • Where tidal mixing is strong, and river flow weak, a well mixed estuary is favored.

  7. Instruments • CTD measures salinity, temperature and depth • From salinity and temperature we get density, measured as sigma-t

  8. The Rewa Sampling plan • The river is about 3m deep • It is deepest on the outside of the bends • There are deep holes upstream at Kalabo bend, near the Rewa bridge, and where the river makes a sharp turn to enter the sea • There are about 12 stations • All begin at the bridge • Some terminate in Laucala Bay, and some in the ocean

  9. General results • Density is in red. • From upstream at Station the there is freshwater all the way to the bottom • There is a saltwater and shallow depth in the middle • Outside in Laucala Bay, there are traces of freshwater at the top, but almost uniform density below that

  10. Results to date • We have continuous records river at the primary gauge at Navalou from 2009 forward, • From 2004 through 2008. project HYCOS (SOPEC/SPC) keeps these records • We prefer the transects which terminate in the sea. Only the 1 2009 and 2010 satisfy all criteria. • We present results which meet these criteria.

  11. River flow has a dominante effect • Low Assembled Results 2008 and 2010 flow. 77.0 5 • High 77.05 2010-10-01 R2 flow, 255. 13 255.13 2010-10-08 R2

  12. The others … 2008-10-26 R2 2008-10-03 R2 2008-09-26 R2

  13. Assembled Results 2008 and 2010 77.05 2010-10-01 R2 255.13 2010-10-08 R2

  14. What of the people of the Rewa Delta?

  15. End

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