Reversal of subtidal dune asymmetries caused by seasonally reversing wind-driven currents in Torres Strait, northeastern Australia

Continental Shelf Research

Volumn 11, Issue 7, 1991, Pages 655-662

  Harris, Peter T ^a  

^a UNIVERSITY OF SYDNEY   (Australia)

Author keywords

[No Author keywords available]

Indexed keywords

ASYMMETRY; BEDFORM; CURRENT; DUNE; MONSOON; SAND TRANSPORT; SANDWAVE;

AUSTRALIA, TORRES STRAIT, ADOLPHUS CHANNEL;

EID: 0026271262     PISSN: 02784343     EISSN: None     Source Type: Journal    
DOI: 10.1016/0278-4343(91)90018-2     Document Type: Article

References (14)

1. Classification of large-scale subaqueous bedforms: a new look at an old problem
2. Bedforms
3. An assessment and calibration of formulations for Bagnold's bedload equation
4. Sediments, bedforms and bedload transport pathways on the continental shelf adjacent to Torres Strait, Australia-Papua New Guinea
5. Sandwave movement under tidal and wind-driven currents in a shallow marine environment: Adolphus Channel, northeastern Australia
6. Side-scan sonar investigation into temporal variation in sand wave morphology: Helwick Sands, Bristol Channel
7. Reversal of sand waves in the Bristol Channel
8. A study in the dynamics of a marine sandwave
9. Sandwaves in the North Sea off the coast of Holland
10. A Global Atlas of GEOS-3 Significant Waveheight Data and Comparison of the Data with National Buoy Data
11. Threshold of sediment motion under unidirectional currents
12. The tidal physics of headland flows and offshore bank formation
13. Mechanisms for linear sandbank formation and maintenance in relation to dynamical oceanographic observations
14. Currents through Torres Strait