- Oceanographic and Atmospheric Processes
- Geology and Paleoclimatology Research
- Geological formations and processes
- Marine and coastal ecosystems
- Geological and Geophysical Studies
- Methane Hydrates and Related Phenomena
- Marine Bivalve and Aquaculture Studies
- Arctic and Antarctic ice dynamics
- Coastal and Marine Management
- Tropical and Extratropical Cyclones Research
- Coastal and Marine Dynamics
- Marine and fisheries research
The University of Western Australia
2019-2020
Ocean Institute
2016-2020
Institute of Mining
2016
Transport of water between the coast and deeper ocean, across continental shelf, is an important process for distribution biota, nutrients, suspended dissolved material on shelf. Presence denser inner shelf results in a cross-shelf density gradient that drives gravitational circulation with offshore transport along sea bed defined as Dense Shelf Water Cascade (DSWC). Analysis field data, collected from multiple ocean glider data missions around Australia, confirmed under range wind tidal...
Along the majority of Australian shallow coastal regions, summer evaporation increases salinity waters, and subsequently in autumn/winter, nearshore waters become cooler due to heat loss. This results formation horizontal density gradients with increasing toward coast that generates gravity currents known as dense shelf water cascades (DSWCs) flowing offshore along sea bed. DSWCs play important role ecological biogeochemical processes through transport dissolved suspended materials offshore....
Mahjabin, T.; Pattiaratchi, C., and Hetzel, Y., 2016. Factors influencing the occurrence of Dense Shelf Water Cascades in Australia. In: Vila-Concejo, A.; Bruce, E.; Kennedy, D.M., McCarroll, R.J. (eds.), Proceedings 14th International Coastal Symposium (Sydney, Australia). Journal Research, Special Issue, No. 75, pp. 527–531. Coconut Creek (Florida), ISSN 0749-0208.Transport inshore waters suspended material off continental shelf by (DSWC) has important ecological biogeochemical...